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FOCUS MINERALS LTD — Capital/Financing Update 2024
Mar 7, 2024
64932_rns_2024-03-07_bdbe0738-388c-4e36-b4b8-14bf04d800d1.pdf
Capital/Financing Update
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Market Announcement
8 March 2024
Laverton Gold Project Mineral Resource Updates
Highlights:
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Review of Central Laverton resources improves geological confidence and delivers additional 233.9Koz Au
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Total updated Mineral Resources for the Laverton Gold Project now comprise: 74.2Mt @ 1.7 g/t for 3.98Moz, a 6.2% gain
West Australia’s newest gold producer Focus Minerals ( ASX: FML ) ( Focus or the Company ) is pleased to announce a compilation of Mineral Resources updates at the Laverton Gold Project ( LGP ). The updated Mineral Resources include the following significantly mineralised structural trends: Craigiemore – Mary Mac, Gladiator, West Laverton – Bulldog, and the Chatterbox Shear.
The LGP covers 407.2km[2] of highly prospective tenements, including the historic Lancefield and Chatterbox trend mines, on the outskirts of the Laverton township in the Goldfields region. Focus’ strategy is to identify sufficient open pit Mineral Resources across the Laverton tenement package to update the Stage 1 Open Pit PFS announced in March 2021.
March quarter 2024 Mineral Resource updates have increased LGP contained gold ounces by 6.2%. The aggregate LGP Measured, Indicated and Inferred Mineral Resources now comprise:
| Classification | Tonnage (Mt) |
Au Grade (g/t) |
Au Contained Moz |
|---|---|---|---|
| Total Measured | 0.39 | 1.7 | 0.02 |
| Total Indicated | 49.29 | 1.5 | 2.33 |
| Total Inferred | 24.54 | 2.1 | 1.63 |
| Total Mineral Resource | 74.22 | 1.7 | 3.98 |
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Figure 1: Key Laverton project deposits with recent Mineral Resource Estimates.
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Table 1: Summary of Combined March Quarter 2024 LGP Mineral Resources updates and changes versus previously reported Mineral Resources
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Central Laverton Location and Past Production
The Central Laverton mining area is located between 2 and 10km E to SSE from Laverton townsite (Figure 2). This mining area includes the following highly mineralised trends:
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Craigiemore - Mary Mac Trend located 2km to 3.6km SSE of Laverton
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West Laverton – Bull Dog Trend located 2.1 to 3.4km E and SE of Laverton
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Gladiator Trend (includes Murrays, Cousin Murrays, Gladiator North, Gladiator UG and Gladiator West) located 4 – 4.5km E and ESE of Laverton
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Chatterbox Trend (includes Innuendo, Eclipse, Apollo, Rumour) located 7.8 – 10km E and SE of Laverton
These deposits are linked by numerous roads including modern haul roads (Figure 2) and have had extensive historic production totalling at least 4,916,751 t @ 2.46 g/t for 389,168 oz stretching back to the turn of the century (Table 2).
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Table 2: Summary historic production from deposits under review in the March Quarter 2024
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Figure 2: Detailed location map for Central Laverton deposits with Mineral Resource Updates in the March quarter 2024. The map details location of Focus tenure and roads relative to the deposits and Laverton townsite. Drill collars are marked for holes extending beyond 60m depth. The collars for holes are coloured as per inset legend representing the best significant intersection for each hole exceeding 0.5g/t and including up to 3m internal dilution converted to GxM (grade x down hole interval). This helps to highlight the parts of the mineralised trends that have been drilled. Representative section locations for following figures are also marked.
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Figure 3: View North of representative 40m wide sections A-A’, B-B’, C-C’, D-D’, E-E’ as marked on Figure 2. The updated February 2024 block models cut off at 0.6 g/t are shown with centroids coloured for gold g/t as per the inset legend. Simplified geology is
marked up to the base of complete oxidisation for each deposit. Drill traces for RC, RC/DD and DD holes extending to at least 60m depth are shown.
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Central Laverton Deposit Summary Geology
The Craigiemore - Mary Mac Trend (Golden Pinnacles, Mary Mac North, Mary Mac South, Craigiemore deposits) broadly comprise N-S to NNE striking mineralisation that dips steeply to the E and ESE (Figures 2 and 3 A -A’). Predominantly mineralisation is strata bound within a BIF unit but in some locations gold mineralisation has extended into the hanging wall and footwall mafic rocks (tholeiitic basalts to the W and quartz dolerite to the E). The BIF has undergone significant deformation and structural thickening and is displaced by late-stage E-W faults. The central zone of mineralisation is associated with vein quartz and pyrite located along a sheared contact between faulted silicified cherty BIF and dolerite mafics. Other zones of mineralisation occur on shears within basalts and on the contacts of dolerites. Within the plane of the main mineralised structures, shoots of thicker and highergrade mineralisation plunge moderately to the NNE.
The West Laverton – Bulldog Trend (Rega, West Laverton and Bulldog deposits) comprises N-S striking mineralisation that dips at about 30 – 35 degrees towards the east (Figures 2 and 3 A -A’, B-B’ and C- C’). The central zone of mineralisation is shear hosted overprinting an ultramafic gabbro. In places the shear is also intruded by felsic porphyry. The footwall of the shear is dominated by a dolerite. The hanging wall comprises basalt. The mineralisation is open at depth, along strike and between deposits. Within the plane of the main mineralised structures shoots of thicker and higher grade mineralisation plunge to the NE.
The Gladiator Trend (Murrays, Cousin Murrays, Gladiator Pit and Gladiator West) comprises NNE, SW and NNW striking mineralisation that dips in a number of directions.
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Murrays deposit dips moderately ESE. Along strike to the north the rich Gladiator underground is located on the northern extension of the Murrays structure (Figures 2 and 3 B-B’).
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The Cousin Murrays deposit is located on a SE striking SW dipping splay/back fault structure that links into Murrays structure north of the pit (Figure 2). The mineralisation is best developed in the vicinity of a dolerite/basalt contact (Figure 3 B-B’)
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The Gladiator Pit structure strikes ESE and dips steeply ESE (Figures 2 and 3 B-B’). A number of moderate NE dipping hanging wall splays nucleate at the north end of the pit with mineralisation extending into the east wall of the pit. The main structure extends at least 500m north of the pit along the hanging wall contact of a dolerite dyke.
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Gladiator West comprises numerous moderate to shallow ESE dipping shears hosted by basalts and sub parallel intermediate porphyries. The mineralisation is developed footwall to the historic gladiator underground (northern extension of the Murrays structure). Where the low angle Gladiator west structures intersect steeper Gladiator UG the width and grade of the mined underground mineralisation locally increases
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Multiple shoot orientations have developed on the Gladiator trend presumably due to the intersections of shears/splays and geology.
The Chatterbox Shear Trend (Innuendo, Apollo (Whisper), Eclipse (Garden Well), Rumour deposits – Figure 2) are located on two prominent aeromagnetic trends that generally strike NNE. These structures extend several km to the north and the Beasley Creek deposits. Chatterbox mineralisation generally dips moderately to the ESE (Figure 3 D-D’ and E-E’). The main zone of mineralisation at Innuendo, Apollo (Whisper) and Rumour is located in the same geological position as the Beasley Creek/Beasley South deposits. The main zone structure comprises intensely altered and sheared melange of hanging wall/footwall sediments and metasediment rocks. This structure is regularly exploited by felsic intrusives and is commonly very deeply weathered. Hanging wall and footwall mineralisation occurs adjacent to and with similar dips to main zone mineralisation. The Eclipse
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(Garden Well) deposit exploits a hanging wall shear that includes intervals of meta sedimentary/BIF. The Garden Well mineralisation is located hanging wall to a dolerite dyke with significant strike that remains untested on Focus tenure.
Central Laverton March Quarter 2024 Updated Mineral Resources
Craigiemore - Mary Mac Trend
The updated Mineral Resources on the Craigiemore - Mary Mac Trend are reported on a dry tonnage basis using 0.6g/t cut off (previously 1.0g/t). Deposits are reported at various depths ranging from 170 - 195m below surface depending on the depth of resource quality drilling. An Ordinary Kriging (OK) estimation technique was selected and variograms were modelled in Supervisor. Each domain was estimated separately using its own sample data and applicable top cut. The updated total Mineral Resource Estimate for the Craigiemore - Mary Mac Trend is summarised with comparison to the previously reported Mineral Resource estimate.
| Classification | Tonnes (Kt) |
Change (t) |
Au Grade (g/t) |
Change (g/t) |
Au Contained (Koz) |
Change Oz |
|---|---|---|---|---|---|---|
| Indicated | 2,533 | 104% | 1.39 | -29% | 113.3 | 45% |
| Inferred | 956.9 | 351% | 1.34 | -43% | 41.2 | 158% |
| Total Craigiemore - Mary Mac Trend |
3,489.9 |
140% |
1.38 | -32% | 154.5 | 64% |
West Laverton Trend
The updated Mineral Resources on the West Laverton Trend are reported on a dry tonnage basis using 0.6g/t cut off. Deposits are reported at various depths ranging from 150 -160m below surface depending on the depth of resource quality drilling. An OK estimation technique was selected and variograms were modelled in Supervisor. Each domain was estimated separately using its own sample data and applicable top cut. The updated total Mineral Resource Estimate for the West Laverton Trend is summarised with comparison to the previously reported Mineral Resource estimate.
| Classification | Tonnes (Kt) |
Change (t) |
Au Grade (g/t) |
Change (g/t) |
Au Contained (Koz) |
Change Oz |
|---|---|---|---|---|---|---|
| Indicated | 1,113.3 | -11% |
1.8 | -14% | 64.5 | -24% |
| Inferred | 2,502.1 | 2,057% |
1.5 | -14% | 120.7 | 1,757% |
| Total West Laverton Trend |
3,615.4 | 164% |
1.59 | -23% | 185.2 | 104% |
Gladiator Trend
The updated Mineral Resources on the Gladiator Trend are reported on a dry tonnage basis using 0.6g/t cut off. Deposits are reported at various depths ranging from 150 -160m below surface depending on the depth of resource quality drilling. An OK estimation technique was selected and variograms were modelled in Supervisor. Each domain was estimated separately using its own sample data and applicable top cut. The updated total Mineral Resource Estimate for the Gladiator Trend is summarised with comparison to the previously reported Mineral Resource estimate.
| Classification | Tonnes (Kt) |
Change (t) |
Au Grade (g/t) |
Change (g/t) |
Au Contained (Koz) |
Change Oz |
|---|---|---|---|---|---|---|
| Indicated | 1,909.6 | 3,879% |
1.03 | -47% | 63 | 2,000% |
| Inferred | 1,405.4 | 1,076% |
1.00 | -34% | 45.1 | 673% |
| Total Gladiator Trend |
3,314.9 | 1,863% |
1.01 | -38% | 108.1 | 1,115% |
Chatterbox Trend
The updated Mineral Resources on the Chatterbox Trend are reported on a dry tonnage basis using 0.6g/t cut off (previously 0.8 – 1.0g/t). Deposits are reported at various depths ranging from 120 -140m below surface depending on the depth of resource quality drilling. An OK estimation technique was selected and variograms were modelled in Supervisor. Each domain was estimated separately using its own sample data and applicable top cut. The updated total Mineral Resource estimate for the Chatterbox Trend is summarised with comparison to the previously reported Mineral Resource estimate.
| Classification | Tonnes (Kt) |
Change (t) |
Au Grade (g/t) |
Change (g/t) |
Au Contained (Koz) |
Change Oz |
|---|---|---|---|---|---|---|
| Measured | 0 | -100% | 0 | -100% | 0 | -100% |
| Indicated | 4,208.5 | 53% |
1.6 | -25% | 215.8 | 15% |
| Inferred | 3,541.1 | 65% |
1.32 | -44% | 150.0 | -7% |
| Total West Laverton Trend |
7,749.6 | 43% |
1.47 | -34% | 365.8 | -5% |
The release of this ASX announcement was authorised by Mr Wanghong Yang, Executive Chairman of Focus Minerals Ltd.
For further information please contact:
For media and investor enquiries please contact:
Alex Aaltonen Nicholas Ong General Manager Exploration Company Secretary Focus Minerals Ltd. Focus Minerals Ltd. Phone: +61 8 9215 7888 Phone: +61 8 9215 7888 Email: [email protected] Email: [email protected]
About Focus Minerals Limited (ASX: FML)
Focus is committed to delivering shareholder value from the Coolgardie Gold Operation, a 116.6km[2] tenement holding that includes a 1.2Mtpa processing plant at Three Mile Hill, with commencement of mining activities in mid2023. A new Life of Mine plan with 7-year production for 402,000oz of gold was announced to the ASX on 24 October 2022.
The Laverton Gold Project covers 407.2km[2] area of highly prospective ground that includes the historic Lancefield and Chatterbox Trend mines. Focus’ priority target is to confirm sufficient gold mineralisation to support production restart at Laverton.
Competent Person Statement
The information in this announcement that relates to Exploration Results is based on information compiled by Mr Alex Aaltonen, who is a Member of the Australasian Institute of Mining and Metallurgy (AusIMM). Mr Aaltonen is an employee of Focus Minerals Limited. Mr Aaltonen has sufficient experience that is relevant to the style of
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mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves.
The Mineral Resource estimates were undertaken by Ms Hannah Kosovich, an employee of Focus Minerals. Ms Hannah Kosovich is a member of Australian Institute of Geoscientists and has sufficient experience to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves.
Mr Aaltonen and Ms Hannah Kosovich consent to the inclusion in the report of the matters based on the information in the form and context in which it appears.
ASX Listing Rule 5.19.2
The Central Laverton deposits with updated Mineral Resource estimates are not included in the Laverton Stage 1 Open Pit PFS Progressive Results announced on 11 March 2021. Therefore, the material assumptions underpinning the production target, or the forecast financial information derived from the PFS continue to apply and have not materially changed.
JORC Code, 2012 Edition – Table 1 Laverton deposits – Chatterbox Deposits (Apollo-Whisper, Eclipse-Garden Well, Innuendo, Rumor), West Laverton Deposits (West Laverton, Rega, Bulldog), Gladiator Deposits (Gladiator West, Murrays, Cousin Murray, Gladiator Pit), Craigiemore, Mary Mac to Mary Mac North and Golden Pinnacles.
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria | Explanation | |
|---|---|---|
| Sampling techniques |
• This report relates to results from Reverse Circulation (RC) and diamond core (DDH) drilling. • Unless specifically mentioned Chatterbox deposits Apollo - Whisper, Eclipse – Garden Well, Innuendo and Rumor are referred to the Chatterbox in this table. West Laverton refers to the deposits West Laverton, Rega and Bulldog in this table. Gladiator deposits Gladiator Pit, Murrays, Cousin Murray and Gladiator West are referred to as Gladiator in this table. Deposits Craigiemore, Mary Mac, Mary Mac North and Golden Pinnacles trend are referred to as CM/MM in this report. • The deposits covered in this release have been drilled by various companies over the years. Most companies held multiple tenements during their tenure with similar drill practices were applied at each deposit. This includes Focus Minerals Ltd (FML), Crescent Gold NL (Crescent), Metex Resources (Metex) and its Laverton Exploration Joint Venture (LEJV) with Delta Gold NL(DGL) and Placer Dome Asia Pacific (PDAP), Sons of Gwalia Ltd (SOG), Western Mining Corporation (WMC), Hillmin Gold Mines Pty Ltd (Hillmin), which was renamed Ashton Gold Mines Pty Ltd (Ashton) in October 1989. This was dissolved in December 1990 with all rights and obligations assumed by Ashton Gold (WA) Ltd. • Chatterbox Trend was drilled by FML, Crescent, Metex/LEJV and WMC. • West Laverton trend was drilled by FML, Crescent, SOG and Hillmin/Ashton. • Gladiator trend was drilled by FML, SOG, WMC, Hillmin/Ashton, Metex/LEJV, Teck Explorations Ltd, Technomin Australia NL • CM/MM trend was drilled by FML, Crescent, SOG and Hillmin/Ashton. • Early Crescent RC holes were sampled at 1m intervals with the sample from the cyclone being collected in a plastic bag then put through a 75/25 riffle splitter, resulting in a 3-4kg sample. Later, larger programs collected 1m RC samples automatically using a cone splitter off the drill rig producing 3kg samples. • Crescent diamond core was sampled across geologically identified zones of mineralisation, the sample lengths varied between a minimum of 0.1m and a maximum of 1.3m. The diamond core was marked up for sampling by the supervising geologist during the core logging process, with sample intervals determined by the presence of lithology, alteration, and where applicable core loss. The core was cut in half using a core saw and the same half of the core (RHS looking downhole) was routinely sent to the laboratory for analysis. Infrequent whole core samples were submitted at CM/MM. • FML and more recent Crescent RC percussion drill chips were collected through a cone splitter from the drill rig. The bulk sample from drilling was placed in neat rows directly on theground(not bagged) with the nominal 2-3kg calico split sub- |
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| sample placed on top of the corresponding pile. RC chips were passed through a cone splitter to achieve a nominal sample weight of approximately 3kg. The splitter was levelled at the beginning of each hole. Geological logging defined whether a sample was to be submitted as a 1m cone split sample or a 4m spear composite sample. Split samples (1m) were transferred to sample numbered calico bags for submission to the laboratory. Composite samples were spear sampled using a scoop to obtain a small representative sample and deposited into numbered sample bags. Mineralised 4m composite sampled where resampled at 1m intervals using stored original 1m cyclone split samples. • FML diamond core was sampled across identified zones of mineralisation and vary from 0.2m to a maximum of 1.2m. The core was cut in half using a core saw and the ½ core samples submitted for assay. • WMC RC samples were collected on 1m intervals. • Hillmin/Ashton collected 1m RC samples via a riffle splitter, some programs also concurrently collected 4m composite samples. Where composite assays exceeded 0.1 ppm Au, the corresponding 1m samples for the entire composite interval were submitted for assay. Hillmin/Ashton recorded duplicate samples in the assay files. • Hillmin diamond core was sampled after diamond sawing to ½ core and mineralised intervals sampled to lithological contacts while non ore grade host rock was submitted as 4m filleted composites. • Ashton diamond drilling was either with an RC pre-collar followed by HQ diamond coring or PQ diamond core from surface, which was reduced to HQ in earlier holes. Diamond core was either quarter or half core sampled in 1m intervals within the mineralised zones or composited to 4m outside known mineralisation zones. • Teck Exploration collected samples in 1m intervals that were composited to 2m for analysis with anomalous values and/or chert intersections assayed at 1m intervals. • Technomin submitted 1m or 2m samples for analysis. • SOG RC holes were sampled as 1m samples from surface using a riffle splitter to generate ~ 3kg samples with later programs collecting samples at 3m- 4m composites and submitting 1m split samples where “significant gold” was intersected. • Metex / LEJV collected RC samples in 1m intervals in plastic bags. All dry sample were riffle split to return a representative 1m split sample for analysis. Any wet/Moist samples where 50mm PVC spear sampled. Samples were 4m composites with corresponding 1m intervals resampled via the same method from composites that returned assay values greater than 0.1ppm. • Metex Diamond holes had an RC pre-collar that was generally composite sampled in 4m intervals, the core was half core samples with sample lengths from only a handful of 4m composites to 0.5m length with the majority of core sampled to 1m intervals. |
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|---|---|
| Drilling techniques | • Only Reverse Circulation (RC) and Diamond drilling (DD) methods have been included in the resource estimate. • FML RC drilling was conducted using a 5 3/8inch face sampling hammer for RC drilling or NQ2 triple tube diamond drilling. At hole completion, downhole surveys for RC holes were completed at 30m intervals using a True North Seeking Gyro tool. • Crescent completed RC using a face sampling hammer or HQ diamond drilling. • Hillmin used rotary mud pre-collars or existing RC holes for its diamond drilling using a PQ or HQ diameter drill bit. • Ashton RC reports state drilling was by a face sampling hammer RC rig. • Ashton used a PQ or HQ diameter drill bit, with coring either from surface or with an RC pre-collar. • SOG used RC face sampling hammer drilling techniques. |
| • Metex/LEJV RC drilling was conducted using 5 3/8inch bits and face sampling hammers with 900cfm/350psi of air boosted to 1200cfm/700psi where necessary by an auxiliary compressor. • Metex Diamond drilling was by NQ sized core barrels at Gladiator and PQ or HQ triple tube core barrels at Chatterbox all with RC pre-collars. • Metex reported that WMC RC holes were drilled using a conventional cross-over sub. • Teck used a variety of RC drilling hammers depending on the rock type using a Schramm rig with 425cfm/250 psi. |
|
|---|---|
| Drill sample recovery |
• Historic RC drill sample recovery is not well documented. • FML/Crescent RC sample recovery was recorded by a visual estimate % during the logging process. • Crescent diamond core recovery was reported as a percentage of the core run. • FML diamond core recovery was measured and recorded as a percentage of the core “run”. That is, the length of core between the run blocks against the increase in hole depth. • Hillmin early RC drill logs do not document drill recovery, however later drill logs have a percentage estimate recorded. • Hillmin Diamond core recovery is recorded as a % of the core in the drill logs and varies from 73% to 100% with majority of recovery above 90%. • Ashton Diamond core recovery is recorded as a % of the core in the drill logs and overall was good. • Metex/LEJV sample recovery is not well documented in their WAMEX reports. In a Chatterbox report diamond core recoveries were generally good. Core loss was recorded in limited areas with significant jointing/fractures or weathered clays. • Along the Chatterbox trend the high water table issues prevalent at Beasley Creek also impacted samples. • Work by Crescent in 2011 to establish unreliable samples based on logging of Wet samples or poor recovery from sample weights were flagged and excluded from the Resource estimate. • Metex developed a sample quality matrix to log sample return and moisture when logging. Sample recovery/return was split into 0-25%, 25-65%, 65-100%; whilst moisture was Wet, Damp, Dry. A record of 1 had the lowest recovery and was wet, 9 was considered high recovery and dry. Samples logged with a Quality ranking of wet, regardless of % return was set to absent and ignored during the grade estimation process but used in the guidance of mineralisation. |
| Logging | • FML/Crescent RC samples were geologically logged to record weathering, regolith, rock type, colour, alteration, mineralisation, structure, texture and any other notable features that are present. All data is entered directly into validating digital software directly. • In addition to parameters logged over RC chips, all diamond core was also logged for structure. If an orientation line was available, structure orientation measurements were taken and recorded. • Core holes were oriented where possible and marked into metre intervals with relation to hole depth. Any loss of core was noted and recorded in the drilling database. Recovery and RQD measurements were recorded. • The logging information was transferred into the company’s drilling database once the log was complete. • Logging was qualitative, however the geologists often recorded quantitative mineral percentage ranges for the sulphide minerals present. • Diamond core was photographed one core tray at a time wet and dry using a standardised photography jig. • The entire length of all holes was logged. • Hillmin/Ashton logged the entire drill hole for colour, weathering, rock type, texture, structure, alteration, veining and mineralisation. |
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| • Ashton diamond holes were also geologically logged for colour, weathering, rock type, texture, structure, alteration, veining and mineralisation. • SOG logged holes from surface for weathering, lithology, texture, grain size, colour, alteration and veining. • WMC RC samples were logged to record colour, grain size, occasional weathering, structural fabric and rock type. • Metex/LEJV RC and DD holes were logged for colour, weathering, structural fabric, alteration, veining, mineralisation, sample quality and lithology. Diamond core was also logged for recovery and RQD. • Teck and Technomin RC holes were logged for colour, weathering, rock type, quartz veining. |
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|---|---|
| Sub-sampling techniques and sample preparation |
• FML All samples were collected in a pre-numbered calico bag bearing a unique sample ID. Jinning Testing & Inspection completed the assay testing, with sample preparation and assay completed in Kalgoorlie. All samples were oven dried, crushed to a nominal 10mm using a jaw crusher (core samples only) and weighed. Samples in excess of 3kg in weight were riffle split to achieve a maximum 3kg sample weight before being pulverized to 90% passing 75μm. Gold analysis was by 40g Fire Assay with an AAS Finish. • Crescent submitted 1m RC samples or ½ core diamond samples. Samples were collected in pre-numbered bags weighing approx. 3kg and submitted to various laboratories for fire assay or screen fire assay with an ICP-OES or AAS Finish. • Hillmin/Ashton submitted either 1m samples or 4m composite samples in numbered bags that corresponded to the 1m intervals they’d composited. Samples were sent to AAL Laboratories in Leonora, SGS in Kalgoorlie or Ultratrace in Perth for Fire Assay on a 50g charge with an AAS finish. Where the composite sample exceeded 0.1 ppm Au, the pre-numbered individual 1m samples were submitted for Fire Assay to a lower detection limit of 0.01ppm Au. • Ashton reports state samples submitted to SGS Kalgoorlie, samples were dried, jaw crushed, hammer milled, split and pulverised. Samples were analysed for gold by fire assay on a 50g charge to a lower limit of detection of 0.01 ppm Au. Where the composite assay exceeded 0.1 ppm, the relevant 1m interval was submitted to SGS for analysis. • Hillmin/Ashton diamond core was sampled as either 4m filleted composites or a sawn core sampled to lithological contacts. Samples were submitted to Genalysis or SGS Kalgoorlie for gold analysis by screen fire assay method. • WMC sub-sampling and assay preparation not documented. Samples were submitted to WMC labs at its Windarra or Kalgoorlie operations. • SOG submitted 1m or 2-4m composite samples for analysis to ALS Laboratories for analysis by aqua regia digest with an AAS finish or Ultra Trace Perth for fire assay. • Teck submitted 2m composite samples to Analabs Kalgoorlie by aqua regia digest with an AAS, subsequent 1m samples submitted were analysed by fire assay. • Technomin submitted 1m or 2m composite samples weighing approx. 2-3kg to Australian Assay Laboratories for a 50g fire assay. • Metex/ LEJV RC samples were submitted to Amdel or Genalysis Kalgoorlie for analysis with either an aqua regia digest or 50g fire assay. At Gladiator a multielement analysis was run on samples. • Metex diamond samples were submitted to Genalysis for multielement analysis with Aqua regia analysis and fire assay on the re-split. |
| Quality of assay data and laboratory tests |
• FML inserted 2 standards and collected 4 duplicates for every 100 samples. Diamond core field duplicates were not taken. Laboratory replicates were also taken in the sample preparation stage by the responsible laboratory. • All results from assay standards, duplicates and lab repeats were scrutinised to ensure they fell within acceptable tolerances. |
| • Crescent submitted Certified Standards, blanks, field duplicates and laboratory repeats at regular intervals over the drill programme. • Crescent logged the sample quality as wet, moist or dry and reviewed sample weights to flag holes as being unreliable and excluded from the estimation. • Crescent also twinned 5 RC holes at Innuendo with diamond to ascertain the effects of the high water content encountered whilst drilling. The report concluded there is reliability issues with down hole contamination in wet samples. This has been taken into account with the estimation by removing all samples logged as wet or unreliable. • All results from assay standards, duplicates and lab repeats were scrutinised to ensure they fell within acceptable tolerances. • Crescent resource geologists also reviewed the available QAQC data for pre- Crescent drilling and generated Q-Q plots to compare the data within flagged lodes and filtered by reliability. The data distribution between companies was comparable and considered acceptable to use. • Hillmin/Ashton took field duplicate samples in the RC. • Hillmin ran a laboratory comparison check during the 1987 drill program comparing RDL Assay results to SGS Assay results for selected drill hole intervals. Then comparing with Minlab. • At CM/MM Hillmin twinned a selection of RC holes with Diamond holes in 1988. • Ashton also ran a laboratory comparison check during the 1989 drill program comparing SGS Assay results for selected drill hole intervals another laboratory, Minlab using a 50g fire assay. Results were found to be comparable. • SOG used Field duplicates and laboratory replicates to check repeatability of results. • WMC sample checks and laboratory information is not well documented however the drilling techniques and assay method are appropriate for this style of mineralisation. Previous Crescent and Metex resource estimates have reviewed and plotted QQ plots to confirm the tenor of mineralisation is comparable. • Teck minerals also ran a re-assaying program with comparable results. • Technomin submitted duplicates as a check on repeatability. • Metex submitted field duplicates at a rate of 1:50 for RC drilling and also used laboratory repeats and standards in their quality checks. • In 1998 along the Chatterbox trend Metex drilled diamond holes to twin previously drilled Metex RC holes as a check. Results showed similar widths and grades of mineralisation were intersected by both drilling methods. • No geophysical tools, spectrometers or handheld XRF instruments were used. |
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|---|---|
| Verification of sampling and assaying |
• Historic sampling and assaying have been checked against hard copy WAMEX reports. • FML primary data is sent in digital format to the company’s Database Administrator (DBA) as often as was practicable. The DBA imports the data into an acQuire database, with assay results merged into the database upon receipt from the laboratory. Once loaded, data was extracted for verification by the geologist in charge of the project. • No adjustments were made to any current or historic data. If data could not be validated to a reasonable level of certainty it was not used in any resource estimations. |
| Location of data points |
• FML utilises Landgate sourced regional topographic maps and contours as well as internally produced survey pick-ups produced by the mining survey teams utilising DGPS base station instruments. • FML drill collars were surveyed upon completion, using a DGPS instrument. Drill core was oriented by the drilling contractor using an Ezy-mark system. For RC a north-seeking gyroscope tool was used to survey down hole. For DDH a magnetic single shot survey was completed at 30m intervals on advance. • The majority of Crescent Gold holes were surveyed by Electronic Multi-shot down hole orgyroscopic survey with collar’s surveyed by site survey personnel. |
Market Announcement | Page 15 of 50
| Drill core was oriented by the drilling contractor using an Ezy-mark system. • Hillmin WAMEX reports note the use of registered surveyors to record the drill hole collars in a local grid. • Ashton collar survey methods are unknown and reported in local grid. • SOG holes were surveyed using an Eastman Single Shot camera at the base of holes over 60m depth. • WMC holes were collar surveyed by WMC survey staff in a local grid. • Teck and Technomin do not state their survey methods. Down hole dips are the planned dip. • Metex/LEJV holes were surveyed by a consultant survey company. Diamond core samples were surveyed by Single Shot Eastman camera. Later RC holes drilled in the JV were gyroscopic down-hole surveyed. • All coordinates and bearings use the MGA94 Zone 51 grid system. • Historic holes have been converted to MGA94 Zone 51 grid system in Acquire. • Historic hole collars were sometimes still visible and re-surveyed to check the accuracy of the grid conversion. The comparison was considered within acceptable error limits of using a DGPS unit. |
|
|---|---|
| Data spacing and distribution |
• Drill spacing along the Chatterbox Trend within the deposit areas is nominally on a grid spacing of 25m x 25m, although at Rumor the grid spacing is closer to 50m x 25m. Apollo within and proximal to the existing open pits has been drilled down to 12.5m x 12.5m spacing in places. Between deposits spacing increases to 50m x 25m and 100m x 50m at the extremes. • West Laverton drill spacing within and immediately surrounding the existing open pits is tight grid spacing 10m x 10m to 25m x 15m. Further out from the pits it extends to a more irregular spacing 25m x 30m-60m. Between West Laverton and Bulldog the drill spacing is irregular, a 350m gap in RC or DD drilling exists between the West Laverton and Bulldog deposits. • Gladiator drill spacing within the existing open pits of Gladiator and Murrays is 15m x 25m, extending out along strike of the pits to 15m x 35m – 50m for a couple of drill lines before becoming a single drill line. Cousin Murray has a 25m x 25m spaced drill pattern. Gladiator West is more irregular spaced pattern of ~ 25m x 25m to 40m x 50m. • CM/MM trend drill spacing is tightly spaced within pit area’s along known mineralisation trends. Within the pit area’s drill spacing is 10m x 15m. Near pit drill spacing extends to an irregular 25m x 20m, which has been infilled down to 12.5m x 10m in certain target areas. • Between Craigiemore and Mary Mac deposits the drill spacing is irregular. There is an 80m gap at the end of the known Craigiemore trend before a small 140m strike of two RC “fence lines” of drilling 25m x 50m spaced. It is then another 90m from the end of the small cluster of RC to the start of the Mary Mac trend and more regular spaced drilling. A gap of 200m exists between the end of Mary Mac Hill and the Golden Pinnacles drilling which focuses on two out-crops and has an irregular drill spacing. |
| Orientation of data in relation to geological structure |
• Drilling was designed based on known geological models, field mapping, verified historical data and cross-sectional interpretation. • Drill holes were oriented at right angles to strike of deposit, with dip optimised for drill capabilities and the dip of the ore body. |
| Sample security | • All samples were reconciled against the sample submission with any omissions or variations reported to FML. • All samples were bagged in a tied numbered calico bag, grouped into green plastic bags. The bags were placed into bulka bags with a sample submission sheet and kept within the Laverton yard until ready for transport to Kalgoorlie by transport courier. • Historic sample security is not recorded. |
Audits or reviews
-
Early Crescent Resource Models were completed by external consultants who undertook data validation as part of the scope of works.
-
• No external audit or review of the Resource Models has been undertaken.
Market Announcement | Page 17 of 50
Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section)
| Criteria | Explanation |
|---|---|
| Mineral tenement and land tenure status |
• All exploration was conducted on tenements 100% owned by FML or its subsidiary companies Focus Operations Pty Ltd and Focus Minerals Laverton. All tenements are in good standing. • Various royalties may be in place as documented in the FML Annual Report. • Native title determination for Nyalpa Pirniku was announced on 31 October 2023. The Laverton Gold Project includes regions that are variously classified in this determination. The Central Laverton deposits and Mineralised Trends detailed in this report are within regions now classified as: Native title exists (non exclusive). • Chatterbox deposits occur across tenements M 38/535 and M 38/101. • West Laverton deposits are within tenement M 38/345. • Adjacent Gladiator deposits occur across tenements M 38/363, M 38/364, M 38/342, E 38/3424. • CM/MM deposits are within tenement M38/270 |
| Exploration done by other parties |
• Various stakeholders over the years have engaged in activities over the deposits including but not limited to geological mapping, ground magnetic surveys, soil sampling, aeromagnetic surveys, costean sampling and rock chip sampling. • Drilling campaigns have been completed over the area by various parties detailed in Section 1. • Along with RC and DD drilling, Air Core and RAB drilling methods have been used to delineate the deposits. • Focus Minerals Laverton successful acquired Crescent Gold in October 2012. • Along the Chatterbox, in 2004 the JV between Metex Resources and PDAP mined a trial pit at Apollo (formerly known as Whisper at time of mining) as part of a pre-feasibility study. A figure of 68Kt @ 2.44g/t Au for 5,351 ounces has been recorded. Crescent Gold commenced open cut mining along the Apollo trend as four discrete pits, separate from the original Whisper pit, from November 2011 to September 2012. The pits varied from 20m deep to 75m total depth. A total of 1.05Mt @ 1.76g/t Au for 59,500 ounces was mined from the four pits. Eclipse (Garden Well) was also mined by Crescent during this time to a depth of 60m for a total of 103Kt @ 2.86g/t Au for 9,443 ounces. • All three deposits along the West Laverton trend have been historically mined as discrete open pits by Ashton Gold in the early 1990’s, with West Laverton the largest. West Laverton was excavated from December 1990 through to May 1992. A reported 116Kt @ 3.15g/t Au for 11,791 ounces was mined from the pit. The final pit reached a depth of 61m. Whilst mining West Laverton, Rega Pit was mined by Ashton from November 1991 until May 1992. A total of 120Kt @ 3.53g/t Au for 13,709 ounces was extracted. The final pit depth was 62.5m. Bulldog was also mined during this period producing 158Kt @ 2.15g/t Au for 10,940 ounces. The final pit reached a depth of 50m. In November 2010 Crescent Gold commence pre-strip waste mining in the 230m long region between West Laverton and Rega open pits. A 247-drill hole campaign of 10m x 10m grid shallow RC grade control was conducted in the region prior to waste mining commencing. In December 2010, trial of mining mineralised waste for two benches was conducted to test the proposed mining methods to account for the shallow dip of the mineralisation. A reported 9Kt @ 0.57g/t Au of mineralised waste was excavated and stockpiled. No further mining was conducted at West Laverton. • Gladiator open pit was mined as a North and South pit by Ashton from Sept 1990 through until February 1992 to a depth of 72.5m. Milling data reports 409Kt @ 2.49g/t Au for 32,771 ounces was processed from both pits. Nearby Murrays open pit was also mined by Ashton from January 1991 to May 1992 for a final depth of 35m. Milling data for Murrays reported 144Kt @ 1.94g/t Au for 8,967 ounces processed. A historic underground mine also known as Gladiator (at the southern extent of Gladiator West) was actively mined between 1897 and 1942 when WW2 impacted mining. It was reportedly mined to about 200m vertically with a strike length of ~ 200m producing 139Kt @ 12g/t Au for 53,600 ounces. • The Craigiemore deposit has been historically mined as underground drives and shafts in the early 1900’s through to the late 1930’s, with a recorded production of 135Kt @ 9.60g/t Au for 41,774 ounces. Minor open cut mining occurred by a private entity in the late 1970’s to early 1980’s with a recorded production of 4Kt @ 1.84g/t Au for 240 ounces. In 1988 Hillmin commenced mining Craigiemore by open cut methods until 1993producing 592Kt@ 2.13g/t Au for 38,000 ounces. |
| Criteria | Explanation |
|---|---|
| Crescent Gold recommenced open cut mining at Craigiemore in June 2010 through until July 2011. An unreconciled mining production of 619Kt @ 1.67g/t Au for 33,178 ounces was recorded in the Crescent mining database. • The Mary Mac deposit was historically mined in the early 1900’s by underground drives and shafts mostly from 1909 until 1913, a figure of 42Kt @ 9.21g/t Au for 12,440 ounces has been reported. In August 2010, Crescent commenced open cut mining at Mary Mac South (MMS) until April 2011, reportedly mining 692Kt @ 1.26g/t Au for 28,034 ounces. Whilst still mining MMS, open pit excavation of Mary Mac Hill (MMH) to the North of MMS commenced in February 2011. Mining open pit continued until July 2012, reportedly 494Kt @ 1.84g/t Au for 29,230 ounces was open cut excavated from MMH. • Numerous historical shafts exist on the Golden Pinnacles deposit, production figures are unknown. |
|
| Geology | • Regionally the deposits are part of the Laverton Greenstone Belt in the Eastern Yilgarn Craton. Lying within the Kurnalpi Terrane which is dominated by andesitic volcanics with erosional remnants of siliclastic sequences, the deposits are located on N to NE striking shear zones between the Mt Margaret Dome in northwest and the Kirgella Dome in the southeast. • Locally the Chatterbox Trend of deposits is hosted by a large-scale structural feature of the region – the Chatterbox Shear Zone, from which its name is derived. This moderately ESE dipping ductile/brittle fault zone separates the Laverton Lithostructural domains from the Mount Margaret Lithostructural domains. Rock units within the deposit areas are strongly altered and sheared sediments and metasediment rocks, felsic intrusives and ultramafics to the east, in the footwall. Mineralisation is commonly associated with increased goethite/manganese/hematite alteration or the intrusions. • The West Laverton deposits consists of two north-south trending banded iron formation (BIF) ridges within a sequence of mafic and ultramafic volcanic and intrusive rocks with interflow sediments. The Laverton Shear Zone, a major north-south trending shear that delineates the western boundary of the Laverton Tectonic Zone, is interpreted as extending through the West Laverton trend from Rega in the North to Bulldog in the south. The footwall of the shear is dominated by a dolerite. The hanging wall comprises basalt. Gold mineralisation is associated with the shear zone overprinting an ultramafic gabbro. West Laverton mineralisation is generally associated within dilational jogs along the shear zone and shallowly dipping quartz veins. Rega mineralisation is interpreted as hosted within two shear zones within massive mafic and pillow basalt units. Bulldog mineralisation is hosted within ductile shear zones with quartz veining. • Gladiator Underground and Murrays deposits are closely related to a bending NNE, SW to NNW striking, east dipping banded iron formation (BIF). Mineralisation is associated with quartz reefs parallel to the BIF and dips in multiple directions. The stratigraphy is dominated by a basalt unit on the west and gabbroic units of varying compositional and granulometry on the east with felsic porphyry units intruding sporadically. Gladiator West sits on the basaltic footwall of Gladiator Underground. Cousin Murray is within the gabbroic hanging wall of Murrays Open Pit and is striking NW, mineralization is associated with silica-sericite alteration. Gladiator Open pit mineralization is associated with quartz feldspar porphyry intrusives. Geology is dominated by basalt with a corridor of dolerite and a felsic tuff on the SW side of the pit and a NE striking BIF on the NE side of the pit. The Central BIF between Cousin Murray and Gladiator South and the NE BIF on the NE of Gladiator South hold mineralization. • The CM/MM trend is hosted in a meta-sedimentary/ mafic volcanic package of rocks that has been highly deformed through late stage folding and faulting. A central steeply dipping Banded Iron Formation (BIF) unit has been associated with the gold mineralisation. Gold commonly occurring within the quartz veining and disseminated pyrite of the silicified chert horizons of the BIF. Evidence of a supergene enrichment zone near the vicinity of the water table was noted during mining by Crescent. The BIF horizon strikes north south and has been traced northwards to Laverton townsite, approximately 4km away. |
| Drill hole Information |
Chatterbox: Historic drilling information has been validated against publicly available WAMEX reports. Not all drill _holes can be found referenced in the WAMEX reports. However, cross-checking of original drill surveys _ |
Market Announcement | Page 19 of 50
| Criteria | Explanation | Explanation | ||
|---|---|---|---|---|
| was verified against the database. | WAMEX Report Date Jun-89 Feb-92 Mar-98 Mar-99 Feb-02 |
|||
| Company | Drill Hole Number | WAMEX Report A- Number |
WAMEX Report Date |
|
| WMC | GDWC009, GDWC010, GDWC012, GDWC013, GDWC014, GDWC030, GDWC031, GDWC034, GDWC035, GDWC037, GDWC038, GDWC048, GDWC049,GDWC052,GDWC053,GDWC056,GDWC057,GDWC058 |
31396 | Jun-89 | |
| GDWC086, GDWC091, GDWC093, GDWC094, GDWC100, GDWC101, GDWC102, GDWC103, GDWC105, GDWC106, GDWC107, GDWC109, GDWC110, GDWC111, GDWC113, GDWC114, GDWC115, GDWC125, GDWC121, GDWC122, GDWC123, GDWC126, GDWC127, GDWC128, GDWC130, GDWC131, GDWC132, GDWC133, GDWC134, GDWC135, GDWC136, GDWC137, GDWC138, GDWC139, GDWC140, GDWC145, GDWC146,GDWC147 |
35126 | Feb-92 | ||
| METEX RESOURCES |
GWD001_W, GWD002_W, GWRC004, GWRC005, GWRC007, GWRC008, GWRC009, GWRC010, GWRC015, GWRC018, GWRC019, GWRC020, GWRC021, GWRC025, GWRC026, GWRC027, GWRC028, GWRC029, GWRC031, GWRC032, GWRC033, GWRC034, GWRC035, GWRC036, GWRC037, GWRC038, GWRC039, GWRC040, GWRC041, GWRC042, GWRC043, GWRC045, GWRC046, GWRC047, GWRC048, GWRC049, GWRC050, GWRC051, GWRC052, GWRC055, GWRC056, GWRC057, GWRC058, GWRC059, GWRC060, GWRC061, GWRC062, GWRC063, GWRC064, GWRC065, GWRC066, GWRC067, GWRC068, GWRC069, GWRC070, GWRC072, GWRC074, GWRC075, GWRC076, GWRC077, GWRC078, GWRC079, GWRC080, GWRC081, GWRC082, GWRC084, GWRC085, GWRC087, GWRC088, GWRC089, GWRC090, GWRC092, GWRC093, GWRC094, GWRC095, GWRC097, GWRC099, GWRC100, GWRC101, GWRC102, GWRC103, GWRC104, GWRC105, GWRC106, GWRC107 |
54899 | Mar-98 | |
| GWD004_W, GWD005_W, GWD006_W, GWD007_W, GWD008_W, GWD009_W, GWD010_W, GWD011_W, GWD012_W, GWD013_W, GWD014_W, GWD015_W, GWD016_W, GWD017_W, GWD018_W, GWD019, GWRC108, GWRC109, GWRC110, GWRC111, GWRC113, GWRC114, GWRC117, GWRC120, GWRC121, GWRC122, GWRC124, GWRC125, GWRC126, GWRC127, GWRC128, GWRC129, GWRC132, GWRC133, GWRC137, GWRC138, GWRC140, GWRC141, GWRC142, GWRC143, GWRC145, GWRC146, GWRC147, GWRC148, GWRC149, GWRC150, GWRC151, GWRC152, GWRC153, GWRC154, GWRC155, GWRC157, GWRC158, GWRC159, GWRC160, GWRC161, GWRC163, GWRC164, GWRC165, GWRC166, GWRC167, GWRC168, GWRC170, GWRC171, GWRC173, GWRC174, GWRC175, GWRC176, GWRC177, GWRC178, GWRC179, GWRC180, GWRC185, GWRC186, GWRC187, GWRC189, GWRC190, GWRC191, GWRC192, GWRC193, GWRC194, GWRC195, GWRC196, GWRC197, GWRC198, GWRC199, GWRC200, GWRC201, GWRC202, GWRC204, GWRC205, GWRC207, GWRC210, GWRC211, GWRC212, GWRC213, GWRC217, GWRC218, GWRC219, GWRC220, GWRC221, GWRC223, GWRC225, GWRC226, GWRC227, GWRC229, GWRC230, GWRC231, GWRC232, GWRC233, GWRC234, GWRC236, GWRC237, GWRC239, GWRC240, GWRC241, GWRC242, GWRC243, GWRC244, GWRC245, GWRC246, GWRC247, GWRC248, GWRC249, GWRC250, GWRC251, GWRC252, GWRC253, GWRC254, GWRC255, GWRC256, GWRC257, GWRC258, GWRC259, GWRC260, GWRC261, GWRC263, GWRC264, GWRC266, GWRC267, GWRC268, GWRC269, GWRC270, GWRC271, GWRC272, GWRC273, GWRC277, GWRC281, GWRC282, GWRC283, GWRC285, GWRC286, GWRC289, GWRC290, GWRC291, GWRC292, GWRC293, GWRC294, GWRC295, GWRC296, GWRC297, GWRC298, GWRC299, GWRC300, GWRC301, GWRC302, GWRC303, GWRC304, GWRC305, GWRC306, GWRC307, GWRC308, GWRC309, GWRC310, GWRC311, GWRC313, GWRC314, GWRC315, GWRC316, GWRC317, GWRC318, GWRC320, GWRC321, GWRC322, GWRC323, GWRC324, GWRC325, GWRC326, GWRC329, GWRC330, GWRC331, GWRC332, GWRC333, GWRC334, GWRC335, GWRC336, GWRC338, GWRC340, GWRC341, RFRC002, RFRC005, RFRC006, RFRC008,RFRC009,RFRC010,RFRC011 |
57921 | Mar-99 | ||
| GWD023, GWD024 | 65027 | Feb-02 |
| Criteria | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | |||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| GWD025, GWD027, GWD028, GWD030, GWD031, GWD032, GWRC410, GWRC411 |
66477 | May-03 | ||||||||||
| GWD035 | 68953 | Mar-04 | ||||||||||
| METEX / AURION GOLD |
GWRC348, GWRC349, GWRC350, GWRC352, GWRC355, GWRC356, GWRC357, GWRC358, GWRC359, GWRC360, GWRC361, GWRC362, GWRC363, GWRC364, GWRC365, GWRC366, GWRC367, GWRC368, GWRC369, GWRC370, GWRC371, GWRC372, GWRC373, GWRC374, GWRC375, GWRC376, GWRC378, GWRC379, GWRC380, GWRC381, GWRC383, GWRC384, GWRC385, GWRC386, GWRC387, GWRC388, GWRC389, GWRC391, GWRC392, GWRC393, GWRC394, GWRC395, GWRC397, GWRC398, GWRC399, GWRC400, GWRC401, GWRC403, GWRC404,GWRC405,GWRC406 |
65027 | Feb-02 | |||||||||
| GWRC420, GWRC421, GWRC422, GWRC423, GWRC424, GWRC425, GWRC426, GWRC427, GWRC428, GWRC429, GWRC430, GWRC431, GWRC432, GWRC433, GWRC434, GWRC435, GWRC436, GWRC437, GWRC438,GWRC439 |
68953 | Jul-04 | ||||||||||
| CRESCENT GOLD |
WHDD001, WHDD002, WHDD003, WHDD004, GWRC468, GWRC469, GWRC470, GWRC471, GWRC472, GWRC475, GWRC476, INRC005, INRC006, INRC007, INRC008, INRC009, INRC010, INRC011, INRC013, INRC015, INRC016, INRC017, INRC018, INRC021, INRC022, INRC023, INRC024, INRC025, INRC026, INRC027, INRC028, INRC029, INRC030, INRC031, INRC032, INRC033, INRC034, INRC035, INRC036, INRC037, INRC040, INRC041, INRC042, INRC043, INRC044, INRC046, INRC048, INRC049, INRC053, INRC054, WHRC018, WHRC019, WHRC020, WHRC022, WHRC023, WHRC024, WHRC025, WHRC026, WHRC027, WHRC028, WHRC029, WHRC030, WHRC031, WHRC032, WHRC033, WHRC034, WHRC035, WHRC036, WHRC037, WHRC038, WHRC039, WHRC040, WHRC041, WHRC042, WHRC043, WHRC044, WHRC045, WHRC046, WHRC047, WHRC048, WHRC049, WHRC050, WHRC051, WHRC052, WHRC053, WHRC054, WHRC055, WHRC056, WHRC059, WHRC060, WHRC061, WHRC062, WHRC063, WHRC064, WHRC065, WHRC066, WHRC067, WHRC068, WHRC069, WHRC070, WHRC071, WHRC072, WHRC073, WHRC074, WHRC075, WHRC076, WHRC077, WHRC078, WHRC079, WHRC080, WHRC081, WHRC082, WHRC083, WHRC085, WHRC086, WHRC087, WHRC088, WHRC090, WHRC091, WHRC092, WHRC093, WHRC094, WHRC095, WHRC096, WHRC098, WHRC100, WHRC101, WHRC102, WHRC103, WHRC104, WHRC105, WHRC106, WHRC107, WHRC109, WHRC110, WHRC111, WHRC113, WHRC114, WHRC117, WHRC118, WHRC119, WHRC120, WHRC121, WHRC122, WHRC123, WHRC124,WHRC125,WHRC126 |
90143 | Apr-11 | |||||||||
| APDD004, APDD005, AUDD001, AUDD002, AUDD003, AUDD004, AUDD005, ECDD001, ECDD002, ECDD003, INDD001, INDD002, APRC001, APRC002, APRC003, APRC004, APRC005, APRC006, APRC007, APRC008, APRC009, APRC010, APRC011, APRC012, APRC013, APRC014, APRC015, APRC016, APRC017, APRC019, APRC020, APRC021, APRC023, APRC024, APRC025, APRC026, APRC027, APRC028, APRC029, APRC030, APRC031, APRC032, APRC033, APRC034, APRC035, APRC036, APRC037, APRC038, APRC039, APRC040, APRC041, APRC042, APRC043, APRC044, APRC045, APRC046, APRC047, APRC048, APRC049, APRC050, APRC051, APRC052, APRC053, APRC054, APRC055, APRC056, APRC057, APRC058, APRC059, APRC060, APRC061, APRC062, APRC063, APRC064, APRC065, APRC066, APRC067, APRC068, APRC069, APRC070, APRC071, APRC072, APRC072A, APRC080, APRC081, APRC085, APRC086, APRC096, APRC097, APRC098, APRC100, APRC101, APRC102, APRC103, APRC104, APRC105, APRC106, APRC107, APRC108, APRC109, APRC110, APRC111, APRC113, APRC114, APRC115, APRC116, APRC118, APRC120, APRC121, APRC122, APRC123, APRC125, APRC126, APRC127, APRC128, APRC129, APRC130, APRC131, APRC132, APRC133, APRC134, APRC135, APRC136, APRC137, APRC138, APRC139, APRC140, APRC142, APRC144, APRC145, APRC146, APRC147, APRC148, APRC149, APRC150, APRC151, APRC152, APRC153, APRC154, ECRC001, ECRC002, ECRC003, ECRC004, ECRC005, ECRC006, ECRC007, ECRC009, ECRC013, ECRC014, ECRC015, ECRC016, ECRC017, ECRC018, ECRC019, ECRC020,ECRC021,ECRC022 |
93988 | Jun-12 | ||||||||||
| ECRC024, EMRC001 | 98404 | Jun-13 | ||||||||||
| Chatterbox collar details of holes not previously externally reported: COMPANY BHID EAST NORTH RL AZIMUTH |
||||||||||||
| COMPANY | BHID | EAST | NORTH | RL | AZIMUTH | DIP | DEPTH |
Market Announcement | Page 21 of 50
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| FOCUS GWRC478 433639.44 6830109.6 441.61 262.6 -60 152 METEX GWRC001 434067.78 6831338.3 440.77 270 -60 20 GWRC002 434137.79 6831338.3 442.8 270 -60 90 GWRC003 434157.79 6831338.3 442.8 270 -60 96 GWRC006 434087.79 6831378.3 441.82 270 -60 30 METEX / PDAP GWRC450 433637.55 6830432.5 438.18 270 -60 60 GWRC451 433668.63 6830482.5 437.8 270 -60 60 GWRC452 433638.63 6830483.3 437.59 90 -60 60 GWRC453 433697.76 6830833.2 434.8 270 -60 65 GWRC454 433709.15 6830833.3 434.88 270 -60 69 GWRC455 433721.06 6830832.8 434.94 270 -60 80 GWRC456 433697.49 6830858.3 434.12 270 -60 65 GWRC457 433709.94 6830858 434.39 270 -60 70 GWRC458 433721.67 6830858.1 434.4 270 -60 80 GWRC459 433662.87 6830858 434.05 90 -60 65 GWRC460 433697.56 6830883.5 434.19 270 -60 65 GWRC461 433709.58 6830882.9 434 270 -60 75 GWRC462 433693.32 6830908.2 434.33 270 -60 60 GWRC463 433702.43 6830908.3 434.35 270 -60 70 GWRC464 433647.76 6830908.2 434.13 270 -60 50 Chatterbox RC Grade control holes drilled by Crescent / FML remaining beneath the current pit floors are tabulated below: BHID EAST NORTH RL AZIMUTH DIP DEPTH AP410101 433722.71 6831508.7 435.34 270 -60 18 AP410102 433712.81 6831507.5 435.27 270 -60 12 AP410105 433743.4 6831522.6 435.68 270 -60 36 AP410106 433735.37 6831522.6 435.58 270 -60 24 AP410107 433727.38 6831522.7 435.51 270 -60 24 AP410108 433718.52 6831522.4 435.43 270 -60 21 AP410109 433709.16 6831522.6 435.28 270 -60 15 AP410110 433758.02 6831532.8 435.35 270 -60 30 AP410111 433749.71 6831533 435.71 270 -60 30 AP410113 433733.59 6831532.9 435.55 270 -60 30 AP410114 433717.84 6831532.9 435.34 270 -60 24 AP410115 433761.75 6831545.4 435.85 270 -60 27 AP410116 433754.12 6831545.4 435.78 270 -60 27 AP410118 433737.73 6831545.5 435.54 270 -60 30 AP410119 433729.6 6831545.6 435.46 270 -60 30 AP410120 433721.26 6831545.7 435.44 270 -60 24 AP410121 433745.44 6831559.1 435.65 270 -60 36 AP410122 433727.25 6831556.8 435.47 270 -60 30 AP410123 433701.15 6831557.4 435.14 270 -60 18 AP410124 433693.1 6831557.4 435.11 270 -60 18 AP410128 433735.04 6831569.5 435.65 270 -60 30 AP410129 433726.72 6831569.5 435.48 270 -60 30 AP410132 433748.39 6831583.5 435.78 270 -60 24 AP410134 433720.18 6831583.4 435.33 270 -60 24 AP410136 433691.92 6831509.6 435.04 270 -90 10 AP410138 433696.29 6831522.4 435.15 0 -90 10 AP410140 433680.43 6831522.5 434.98 0 -90 10 AP410149 433688.77 6831545.8 435.05 0 -90 10 AP410163 433746.96 6831596.2 435.82 0 -90 12 AP410164 433739.47 6831595.5 435.7 0 -90 12 AP410165 433731.62 6831595.3 435.56 0 -90 15 AP410166 433723.63 6831595.5 435.56 0 -90 15 AP410169 433699.82 6831595.5 435.14 0 -90 12 AP410172 433744.17 6831608.4 435.68 0 -90 10 AP410173 433729.85 6831608.1 435.56 0 -90 10 AP410174 433720.32 6831608.1 435.43 0 -90 10 AP410175 433704.95 6831608.3 435.21 0 -90 10 |
FOCUS | GWRC478 | 433639.44 | 6830109.6 | 441.61 | 262.6 | -60 | 152 | |
| METEX |
GWRC001 | 434067.78 | 6831338.3 | 440.77 | 270 | -60 | 20 | ||
| GWRC002 | 434137.79 | 6831338.3 | 442.8 | 270 | -60 | 90 | |||
| GWRC003 | 434157.79 | 6831338.3 | 442.8 | 270 | -60 | 96 | |||
| GWRC006 | 434087.79 | 6831378.3 | 441.82 | 270 | -60 | 30 | |||
| METEX / PDAP |
GWRC450 | 433637.55 | 6830432.5 | 438.18 | 270 | -60 | 60 | ||
| GWRC451 | 433668.63 | 6830482.5 | 437.8 | 270 | -60 | 60 | |||
| GWRC452 | 433638.63 | 6830483.3 | 437.59 | 90 | -60 | 60 | |||
| GWRC453 | 433697.76 | 6830833.2 | 434.8 | 270 | -60 | 65 | |||
| GWRC454 | 433709.15 | 6830833.3 | 434.88 | 270 | -60 | 69 | |||
| GWRC455 | 433721.06 | 6830832.8 | 434.94 | 270 | -60 | 80 | |||
| GWRC456 | 433697.49 | 6830858.3 | 434.12 | 270 | -60 | 65 | |||
| GWRC457 | 433709.94 | 6830858 | 434.39 | 270 | -60 | 70 | |||
| GWRC458 | 433721.67 | 6830858.1 | 434.4 | 270 | -60 | 80 | |||
| GWRC459 | 433662.87 | 6830858 | 434.05 | 90 | -60 | 65 | |||
| GWRC460 | 433697.56 | 6830883.5 | 434.19 | 270 | -60 | 65 | |||
| GWRC461 | 433709.58 | 6830882.9 | 434 | 270 | -60 | 75 | |||
| GWRC462 | 433693.32 | 6830908.2 | 434.33 | 270 | -60 | 60 | |||
| GWRC463 | 433702.43 | 6830908.3 | 434.35 | 270 | -60 | 70 | |||
| GWRC464 | 433647.76 | 6830908.2 | 434.13 | 270 | -60 | 50 |
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| AP410177 | 433731.21 | 6831620.8 | 435.61 | 0 | -90 | 10 | |||
| AP410180 | 433706.91 | 6831620.3 | 435.27 | 0 | -90 | 10 | |||
| AP410188 | 433699.02 | 6831645.6 | 435.14 | 0 | -90 | 10 | |||
| AP410191 | 433731.51 | 6831527.7 | 435.48 | 270 | -60 | 18 | |||
| AP410192 | 433739.35 | 6831527.7 | 435.56 | 270 | -60 | 21 | |||
| AP410193 | 433746.95 | 6831527.7 | 435.34 | 270 | -60 | 25 | |||
| AP410195 | 433762.97 | 6831527.4 | 435.62 | 270 | -60 | 25 | |||
| AP410196 | 433770.89 | 6831527.6 | 435.93 | 270 | -60 | 25 | |||
| AP410202 | 433754.61 | 6831539 | 435.7 | 270 | -60 | 25 | |||
| AP410203 | 433762.33 | 6831538.8 | 435.52 | 270 | -60 | 25 | |||
| AP410204 | 433770.56 | 6831538.8 | 435.96 | 270 | -60 | 25 | |||
| AP410208 | 433739.35 | 6831551.3 | 435.47 | 270 | -60 | 25 | |||
| AP410209 | 433747.52 | 6831551.1 | 435.71 | 270 | -60 | 25 | |||
| AP410210 | 433755.26 | 6831551.1 | 435.6 | 270 | -60 | 25 | |||
| AP410214 | 433749.82 | 6831557.1 | 435.73 | 270 | -60 | 25 | |||
| AP410216 | 433723.68 | 6831562.9 | 435.36 | 270 | -60 | 21 | |||
| AP410217 | 433731.58 | 6831562.8 | 435.36 | 270 | -60 | 25 | |||
| AP410218 | 433739.69 | 6831563 | 435.54 | 270 | -60 | 25 | |||
| AP410226 | 433702.89 | 6831627 | 435.14 | 0 | -90 | 6 | |||
| AP410229 | 433727.77 | 6831626.9 | 435.52 | 0 | -90 | 6 | |||
| AP410232 | 433717.14 | 6831614.2 | 435.36 | 0 | -90 | 6 | |||
| AP410234 | 433732.44 | 6831614.3 | 435.59 | 0 | -90 | 6 | |||
| AP410236 | 433701.39 | 6831602 | 435.18 | 0 | -90 | 6 | |||
| AP410237 | 433717.02 | 6831602.1 | 435.4 | 0 | -90 | 6 | |||
| AP410238 | 433725.34 | 6831602.5 | 435.44 | 0 | -90 | 10 | |||
| AP410240 | 433740.75 | 6831602.1 | 435.67 | 0 | -90 | 10 | |||
| AP410244 | 433679.38 | 6831589.5 | 434.72 | 0 | -90 | 7 | |||
| AP410250 | 433727.8 | 6831589.5 | 435.15 | 0 | -90 | 10 | |||
| AP410251 | 433735.54 | 6831589.4 | 435.21 | 0 | -90 | 10 | |||
| AP410252 | 433743.01 | 6831589.4 | 435.38 | 0 | -90 | 10 | |||
| AP410261 | 433676.81 | 6831516 | 434.75 | 0 | -90 | 6 | |||
| AP410263 | 433691.52 | 6831515.8 | 434.82 | 0 | -90 | 6 | |||
| AP410437 | 433635.65 | 6830443.1 | 437.86 | 289 | -50 | 41 | |||
| AP410443 | 433652.62 | 6830463.4 | 437.77 | 290 | -50 | 45 | |||
| AP410457 | 433652.94 | 6830504.7 | 437.1 | 279.6 | -60 | 35 | |||
| AP410462 | 433675.25 | 6830512.9 | 437.19 | 280 | -50 | 48 | |||
| AP410464 | 433670.05 | 6830527.5 | 437.03 | 280 | -50 | 36 | |||
| AP410465 | 433680.36 | 6830524.5 | 437.19 | 279.6 | -50 | 45 | |||
| AP410467 | 433670.33 | 6830540.2 | 436.91 | 280 | -50 | 29 | |||
| AP410468 | 433677.38 | 6830540 | 437.09 | 279.6 | -50 | 36 | |||
| AP410469 | 433683.14 | 6830539.6 | 437.03 | 279.6 | -50 | 44 | |||
| AP410471 | 433685.75 | 6830550.6 | 436.93 | 280 | -50 | 48 | |||
| AP410476 | 433692.86 | 6830561.8 | 436.81 | 279.6 | -50 | 46 | |||
| AP410481 | 433697.57 | 6830572.9 | 436.76 | 280 | -50 | 48 | |||
| AP410485 | 433695.69 | 6830585.8 | 436.67 | 280 | -50 | 45 | |||
| AP410503 | 433225.77 | 6829388.3 | 439.65 | 290 | -50 | 48 | |||
| AP410504 | 433233.79 | 6829385.4 | 439.78 | 290 | -50 | 54 | |||
| AP410505 | 433226.18 | 6829401.3 | 439.64 | 290 | -50 | 36 | |||
| AP410506 | 433233.92 | 6829398.3 | 439.67 | 290 | -50 | 46 | |||
| AP410507 | 433248.01 | 6829393.3 | 439.74 | 289.6 | -50 | 60 | |||
| AP410510 | 433241.1 | 6829409.3 | 439.54 | 290 | -50 | 48 | |||
| AP410511 | 433248.92 | 6829406.5 | 439.59 | 290 | -50 | 54 | |||
| AP410515 | 433256.38 | 6829416.6 | 439.38 | 290 | -50 | 54 | |||
| AP410516 | 433264.53 | 6829413.6 | 439.54 | 290 | -50 | 60 | |||
| AP410520 | 433256.77 | 6829430.6 | 439.38 | 289.6 | -50 | 46 | |||
| AP410523 | 433258.43 | 6829442.8 | 439.15 | 289.6 | -50 | 40.19 | |||
| AP410524 | 433265.68 | 6829440.4 | 439.33 | 289.6 | -50 | 43 | |||
| AP410526 | 433258.78 | 6829456.2 | 439.01 | 289.6 | -50 | 36 | |||
| AP410527 | 433265.88 | 6829453.8 | 439.11 | 289.6 | -50 | 39 | |||
| AP410528 | 433269.61 | 6829452.1 | 439.19 | 289.6 | -60.1 | 42 | |||
| AP410531 | 433274.19 | 6829464.1 | 439.01 | 289.6 | -50 | 42 | |||
| AP410533 | 433271.96 | 6829478 | 438.9 | 289.6 | -60 | 35 | |||
| AP410536 | 433282.85 | 6829487.3 | 438.84 | 289.6 | -50 | 36 | |||
| AP410537 | 433289.28 | 6829484.9 | 438.93 | 289.6 | -50 | 44 | |||
| AP410538 | 433281.03 | 6829500 | 438.99 | 289.34 | -60.29 | 36.33 | |||
| AP420105 | 433655.87 | 6830520.8 | 419.77 | 270 | -60 | 24 |
Market Announcement | Page 23 of 50
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| AP420106 | 433664.68 | 6830520.6 | 419.51 | 270 | -60 | 36 | |||
| AP420107 | 433672.83 | 6830520.6 | 419.81 | 270 | -60 | 36 | |||
| AP420108 | 433680.46 | 6830520.2 | 419.93 | 270 | -60 | 36 | |||
| AP420110 | 433657.7 | 6830508.1 | 419.57 | 270 | -60 | 36 | |||
| AP420111 | 433669.66 | 6830508.1 | 419.81 | 270 | -60 | 48 | |||
| AP420113 | 433696.79 | 6830505.9 | 422.24 | 270 | -60 | 54 | |||
| AP420115 | 433680.9 | 6830495.7 | 422.38 | 270 | -60 | 42 | |||
| AP420116 | 433685.85 | 6830495.3 | 422.3 | 270 | -60 | 42 | |||
| AP420117 | 433692.98 | 6830495.3 | 422.28 | 270 | -60 | 48 | |||
| AP420118 | 433701.53 | 6830495.2 | 422.42 | 270 | -60 | 48 | |||
| AP420119 | 433646.22 | 6830482.9 | 422.37 | 270 | -60 | 36 | |||
| AP420120 | 433679.61 | 6830482.7 | 422.38 | 270 | -60 | 42 | |||
| AP420121 | 433688.03 | 6830482.5 | 422.35 | 270 | -60 | 48 | |||
| AP420122 | 433646.91 | 6830470.9 | 422.49 | 270 | -60 | 36 | |||
| AP420124 | 433680.03 | 6830470.6 | 422.47 | 270 | -60 | 48 | |||
| AP420125 | 433687.7 | 6830470.4 | 422.45 | 270 | -60 | 48 | |||
| AP420126 | 433651.67 | 6830458.1 | 422.39 | 270 | -60 | 48 | |||
| AP420130 | 433665.79 | 6830445.8 | 422.7 | 270 | -60 | 48 | |||
| AP420131 | 433672.9 | 6830445.6 | 422.68 | 270 | -60 | 48 | |||
| APC420002 | 433713.91 | 6830989.1 | 419.5 | 280 | -55 | 21 | |||
| APC420003 | 433723.22 | 6830987.5 | 419.72 | 280 | -55 | 28 | |||
| APC420004 | 433758.45 | 6830979.8 | 419.57 | 280 | -60 | 19 | |||
| APC420007 | 433722.82 | 6830974.2 | 419.9 | 280 | -50 | 29 | |||
| APC420008 | 433730.42 | 6830973.2 | 420.05 | 280 | -50 | 38 | |||
| APC420015 | 433684.96 | 6830968.6 | 419.71 | 280 | -70 | 25 | |||
| APC420017 | 433699.91 | 6830966.4 | 419.77 | 280 | -70 | 27 | |||
| APC420018 | 433707.84 | 6830965 | 419.79 | 280 | -65 | 29 | |||
| APC420019 | 433719.69 | 6830963 | 420.01 | 280 | -60 | 30 | |||
| APC420020 | 433738.04 | 6830959.4 | 420 | 277.2 | -59.7 | 46 | |||
| APC420022 | 433766.5 | 6830953.9 | 420.42 | 280 | -65 | 30 | |||
| APC420023 | 433652.99 | 6830962.5 | 419.52 | 0 | -90 | 25 | |||
| APC420026 | 433718.69 | 6830950.1 | 419.96 | 280 | -50 | 39 | |||
| APC420027 | 433726.45 | 6830948.7 | 420 | 272.9 | -49 | 41 | |||
| APC420028 | 433735.17 | 6830947.3 | 419.91 | 272 | -49 | 44 | |||
| APC420029 | 433743.12 | 6830945.8 | 419.9 | 268.8 | -49.4 | 47 | |||
| APC420030 | 433750.13 | 6830944.5 | 419.9 | 270.5 | -50 | 52 | |||
| APC420034 | 433644.2 | 6830951.7 | 419.77 | 0 | -90 | 31 | |||
| APC420035 | 433651.72 | 6830949.7 | 419.55 | 0 | -90 | 34 | |||
| APC420036 | 433659.98 | 6830947.8 | 419.71 | 0 | -90 | 34 | |||
| APC420037 | 433667.23 | 6830946.5 | 419.77 | 0 | -90 | 34 | |||
| APC420038 | 433676.9 | 6830944.4 | 419.75 | 280 | -80 | 34 | |||
| APC420039 | 433686.93 | 6830942.9 | 419.84 | 280 | -70 | 35 | |||
| APC420040 | 433698.12 | 6830940.6 | 419.7 | 280 | -60 | 38 | |||
| APC420041 | 433706.89 | 6830939.1 | 419.96 | 280 | -60 | 39 | |||
| APC420042 | 433720.43 | 6830936.5 | 420.02 | 270 | -60 | 44 | |||
| APC420043 | 433733.22 | 6830934.7 | 419.96 | 270 | -60 | 48 | |||
| APC420046 | 433659.4 | 6830935.5 | 419.61 | 270 | -60 | 38 | |||
| APC420047 | 433670.49 | 6830932.9 | 420.04 | 270 | -60 | 41 | |||
| APC420048 | 433682.73 | 6830930.3 | 420.21 | 270 | -60 | 43 | |||
| APC420051 | 433714.38 | 6830925.5 | 420.09 | 270 | -50 | 49 | |||
| APC420052 | 433721.11 | 6830924.1 | 420.09 | 270 | -50 | 53 | |||
| APC420053 | 433730.41 | 6830922.4 | 420.26 | 270 | -50 | 56 | |||
| APC420054 | 433736.89 | 6830921.4 | 420.27 | 270 | -50 | 53 | |||
| APC420056 | 433754.7 | 6830918.5 | 421.08 | 270 | -50 | 58 | |||
| APC420057 | 433762.68 | 6830916.9 | 420.93 | 270 | -50 | 65 | |||
| APC420059 | 433657.92 | 6830922.9 | 419.85 | 270 | -60 | 37 | |||
| APC420060 | 433665.2 | 6830921.9 | 419.97 | 270 | -60 | 39 | |||
| APC420061 | 433672.53 | 6830920.7 | 419.66 | 270 | -60 | 40 | |||
| APC420062 | 433680.32 | 6830919.1 | 419.8 | 270 | -60 | 42 | |||
| APC420063 | 433695.61 | 6830915.5 | 420.57 | 270 | -60 | 43 | |||
| APC420065 | 433711.92 | 6830913.2 | 419.96 | 270 | -60 | 43 | |||
| APC420066 | 433737.42 | 6830908.1 | 419.89 | 270 | -60 | 51 | |||
| APC420071 | 433718.29 | 6830904.1 | 419.84 | 250 | -55 | 48 | |||
| APC420072 | 433732.66 | 6830902.9 | 419.64 | 250 | -50 | 57 | |||
| APC420073 | 433745.12 | 6830894.7 | 420.11 | 270 | -50 | 60 | |||
| APC420074 | 433756.69 | 6830892.4 | 420.03 | 270 | -50 | 61 |
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| APC420076 | 433645.54 | 6830900.3 | 419.87 | 270 | -65 | 31 | |||
| APC420077 | 433655.88 | 6830899.2 | 419.78 | 270 | -65 | 34 | |||
| APC420078 | 433664.92 | 6830897 | 419.77 | 270 | -65 | 38 | |||
| APC420079 | 433675.87 | 6830895.1 | 419.77 | 270 | -64 | 41 | |||
| APC420080 | 433695.74 | 6830890.7 | 419.78 | 270 | -60 | 50 | |||
| APC420081 | 433705.15 | 6830889.5 | 419.88 | 270 | -60 | 54 | |||
| APC420082 | 433723.98 | 6830885.5 | 419.98 | 270 | -60 | 56 | |||
| APC420083 | 433737.48 | 6830883.5 | 420.08 | 270 | -60 | 52 | |||
| APC420084 | 433745.61 | 6830881.9 | 420 | 270 | -60 | 55 | |||
| APC420087 | 433673.03 | 6830882.3 | 419.28 | 270 | -60 | 38 | |||
| APC420088 | 433682.02 | 6830880.9 | 419.33 | 270 | -60 | 42 | |||
| APC420090 | 433730.83 | 6830871.9 | 420.18 | 270 | -60 | 57 | |||
| APC420091 | 433740.88 | 6830870.1 | 419.98 | 270 | -60 | 59 | |||
| APC420094 | 433767.85 | 6830865.1 | 419.84 | 270 | -60 | 41 | |||
| APC420098 | 433703.73 | 6830863.7 | 419.79 | 280 | -60 | 51 | |||
| APC420100 | 433721.91 | 6830860.6 | 420.13 | 270 | -60 | 58 | |||
| APC420101 | 433735.59 | 6830857.8 | 420.36 | 270 | -60 | 65 | |||
| APC420104 | 433735.23 | 6830845.7 | 420.25 | 270 | -60 | 68 | |||
| APC420107 | 433761.81 | 6830840.9 | 420.2 | 280 | -60 | 40 | |||
| APC420111 | 433695.02 | 6830838.8 | 420 | 280 | -50 | 52 | |||
| APC420112 | 433702.88 | 6830837.5 | 420.02 | 280 | -50 | 59 | |||
| APC420113 | 433710.41 | 6830836.3 | 420.08 | 280 | -50 | 66 | |||
| APC420114 | 433718.57 | 6830834.6 | 420.18 | 279 | -50 | 72 | |||
| APC420115 | 433724.04 | 6830834.1 | 420.19 | 280 | -60 | 67 | |||
| APC420120 | 433761.28 | 6830762.1 | 420.13 | 280 | -55 | 56 | |||
| APC420122 | 433702 | 6830695.9 | 419.94 | 280 | -50 | 17 | |||
| APC420123 | 433698.83 | 6830687.9 | 419.74 | 280 | -50 | 23 | |||
| APC425001 | 433714.29 | 6830684.5 | 424.64 | 280 | -50 | 38 | |||
| APC425003 | 433723.73 | 6830695.4 | 424.92 | 280 | -50 | 40 | |||
| APC425004 | 433733.63 | 6830693.1 | 425.11 | 280 | -50 | 36 | |||
| APC425007 | 433736.03 | 6830705.2 | 424.91 | 280 | -60 | 44 | |||
| APC425012 | 433738.62 | 6830717.6 | 424.84 | 280 | -50 | 44 | |||
| APC425013 | 433746.09 | 6830716.5 | 424.8 | 280 | -50 | 51 | |||
| APC425014 | 433754.51 | 6830714.8 | 424.92 | 280 | -50 | 58 | |||
| APC425018 | 433736.12 | 6830731.2 | 424.95 | 280 | -60 | 43 | |||
| APC425019 | 433747.12 | 6830729.2 | 424.97 | 280 | -60 | 50 | |||
| APC425027 | 433759.23 | 6830739.5 | 425.18 | 280 | -50 | 57 | |||
| APC425042 | 433691.41 | 6830790.5 | 424.88 | 280 | -50 | 38 | |||
| APC425043A | 433699.26 | 6830788.4 | 424.97 | 280 | -60 | 42 | |||
| APC425051 | 433708.62 | 6830799.6 | 424.85 | 280 | -50 | 53 | |||
| APC425062 | 433701.86 | 6830813.2 | 424.86 | 280 | -50 | 62 | |||
| APC425063 | 433709.96 | 6830811.8 | 424.85 | 280 | -50 | 63 | |||
| APC425064 | 433726.01 | 6830809.3 | 425.05 | 280 | -50 | 74 | |||
| APC425071 | 433708.14 | 6830824.8 | 425.07 | 280 | -60 | 62 | |||
| APC425072 | 433711.17 | 6830823.9 | 424.77 | 280 | -70 | 65 | |||
| APC425079 | 433771.99 | 6830813.9 | 424.77 | 280 | -50 | 46 | |||
| APD410103 | 433521.59 | 6830120.5 | 409.88 | 270 | -60 | 42 | |||
| APD410104 | 433529.04 | 6830120.5 | 409.99 | 270 | -60 | 42 | |||
| APD410106 | 433519.9 | 6830107.9 | 409.87 | 270 | -60 | 42 | |||
| APD410107 | 433527.04 | 6830107.9 | 409.89 | 270 | -60 | 42 | |||
| APD410111 | 433521.6 | 6830095.6 | 409.63 | 270 | -60 | 48 | |||
| APD410112 | 433528.93 | 6830095.4 | 409.7 | 270 | -60 | 54 | |||
| APD410114 | 433524.69 | 6830082.9 | 409.78 | 270 | -60 | 60 | |||
| APD410115 | 433532.41 | 6830082.8 | 409.87 | 270 | -60 | 66 | |||
| APD410118 | 433526.02 | 6830070.3 | 409.9 | 270 | -60 | 66 | |||
| APD410119 | 433533.17 | 6830070.4 | 410.1 | 270 | -60 | 73 | |||
| APD410122 | 433525.55 | 6830058 | 410.19 | 270 | -60 | 66 | |||
| APD410123 | 433540.58 | 6830058.1 | 410.23 | 270 | -60 | 66 | |||
| APD410127 | 433513 | 6830045.5 | 410 | 270 | -60 | 60 | |||
| APD410128 | 433529.91 | 6830045.4 | 409.96 | 270 | -60 | 72 | |||
| APD410133 | 433522.62 | 6830032.9 | 410.09 | 270 | -60 | 66 | |||
| APD410139 | 433512.63 | 6830020.5 | 410.05 | 270 | -60 | 60 | |||
| APD410140 | 433519.79 | 6830020.4 | 410 | 270 | -60 | 60 | |||
| APD410141 | 433526.81 | 6830020.5 | 410.12 | 270 | -60 | 60 | |||
| APD410144 | 433501.74 | 6830008.1 | 409.56 | 270 | -60 | 60 | |||
| APD410147 | 433486.61 | 6829995.5 | 409.81 | 270 | -60 | 48 |
Market Announcement | Page 25 of 50
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| APD410148 | 433501.15 | 6829995.5 | 409.9 | 270 | -60 | 60 | |||
| APD410149 | 433509.59 | 6829995.4 | 409.98 | 270 | -60 | 60 | |||
| APD410151 | 433499.14 | 6829983.2 | 409.9 | 270 | -60 | 60 | |||
| APD410152 | 433507.69 | 6829983.3 | 410.02 | 270 | -60 | 60 | |||
| APD410154 | 433475.86 | 6829970.5 | 409.98 | 270 | -60 | 30 | |||
| APD410155 | 433483.81 | 6829970.5 | 410.05 | 270 | -60 | 36 | |||
| APD410156 | 433491.67 | 6829970.5 | 410.14 | 270 | -60 | 36 | |||
| APD410157 | 433499.62 | 6829970.5 | 410.01 | 270 | -60 | 45 | |||
| APD415101 | 433669.13 | 6830530.4 | 415.17 | 270 | -60 | 30 | |||
| APD415102 | 433678.86 | 6830508.2 | 414.76 | 270 | -59.1 | 50 | |||
| APD415103 | 433654.18 | 6830495.3 | 414.83 | 270 | -60 | 30 | |||
| APD415106 | 433631.7 | 6830483 | 414.9 | 270 | -60 | 18 | |||
| APD415107 | 433697.18 | 6830482.9 | 414.82 | 270 | -60.9 | 48 | |||
| APD415108 | 433691.38 | 6830470.2 | 414.92 | 270 | -59 | 42 | |||
| APD415109 | 433678.14 | 6830458 | 414.73 | 270 | -58.7 | 42 | |||
| APD415111 | 433675.76 | 6830445.7 | 414.72 | 270 | -58.7 | 42 | |||
| APD415113 | 433654.94 | 6830433.2 | 414.94 | 270 | -60 | 36 | |||
| APD415116 | 433647.99 | 6830420.5 | 414.82 | 270 | -60 | 36 | |||
| APD415117 | 433656.14 | 6830420.5 | 414.9 | 270 | -57.3 | 42 | |||
| APD415118 | 433664.07 | 6830420.4 | 414.91 | 270 | -59.1 | 54 | |||
| APD415120 | 433607.05 | 6830408 | 414.82 | 270 | -60 | 24 | |||
| APD415121 | 433622.95 | 6830408 | 414.54 | 270 | -60 | 36 | |||
| APD415123 | 433651.61 | 6830407.9 | 414.66 | 270 | -60 | 60 | |||
| APD415124 | 433666.93 | 6830407.8 | 415.07 | 270 | -60 | 60 | |||
| APD415125 | 433681.44 | 6830407.9 | 414.92 | 270 | -60 | 60 | |||
| APD415127 | 433604.5 | 6830395.3 | 414.69 | 270 | -60 | 30 | |||
| APD415128 | 433612.81 | 6830395.4 | 414.63 | 270 | -60 | 30 | |||
| APD415135 | 433663.79 | 6830395.6 | 414.76 | 270 | -60 | 60 | |||
| APD415137 | 433605.93 | 6830383 | 414.79 | 270 | -60 | 36 | |||
| APD415138 | 433612.56 | 6830382.9 | 414.75 | 270 | -60 | 36 | |||
| APD415141 | 433652.84 | 6830383 | 414.86 | 270 | -60 | 60 | |||
| APD415142 | 433667.12 | 6830382.8 | 414.92 | 270 | -60 | 60 | |||
| APD415143 | 433678.7 | 6830382.9 | 414.96 | 270 | -59.1 | 42 | |||
| APD415146 | 433594.01 | 6830370.4 | 414.81 | 270 | -60 | 30 | |||
| APD415147 | 433601.74 | 6830370.4 | 414.68 | 270 | -60 | 30 | |||
| APD415153 | 433649.72 | 6830370.4 | 415.07 | 270 | -59.1 | 54 | |||
| APD415156 | 433673.86 | 6830370.5 | 414.97 | 270 | -60 | 30 | |||
| APD415157 | 433681.61 | 6830370.4 | 414.98 | 270 | -60 | 30 | |||
| APD415163 | 433641.71 | 6830358 | 414.56 | 270 | -60 | 60 | |||
| APD415168 | 433587.26 | 6830345.5 | 414.7 | 270 | -60 | 30 | |||
| APD415173 | 433628.62 | 6830345.7 | 414.71 | 270 | -60 | 54 | |||
| APD415174 | 433636.39 | 6830345.8 | 414.8 | 270 | -60 | 54 | |||
| APD415180 | 433583.66 | 6830333.1 | 414.71 | 270 | -60 | 36 | |||
| APD415181 | 433591.42 | 6830333.5 | 414.81 | 270 | -60 | 42 | |||
| APD415182 | 433598.24 | 6830333.3 | 414.86 | 270 | -60 | 42 | |||
| APD415183 | 433615.49 | 6830333.2 | 414.99 | 270 | -60 | 54 | |||
| APD415184 | 433632.23 | 6830333.2 | 414.9 | 270 | -60 | 60 | |||
| APD415189 | 433575.42 | 6830320.5 | 414.88 | 270 | -60 | 36 | |||
| APD415190 | 433584.09 | 6830320.5 | 414.83 | 270 | -60 | 42 | |||
| APD415191 | 433592.09 | 6830320.5 | 414.81 | 270 | -60 | 54 | |||
| APD415192 | 433599.8 | 6830320.5 | 414.86 | 270 | -60 | 54 | |||
| APD415194 | 433615.95 | 6830320.6 | 414.68 | 270 | -60 | 54 | |||
| APD415195 | 433624.03 | 6830320.4 | 414.81 | 270 | -60 | 54 | |||
| APD415199 | 433581.4 | 6830308.1 | 414.81 | 270 | -60 | 48 | |||
| APD415200 | 433600.15 | 6830308 | 414.88 | 270 | -60 | 48 | |||
| APD415208 | 433572.04 | 6830295.6 | 414.54 | 270 | -60 | 42 | |||
| APD415209 | 433579.82 | 6830295.4 | 414.67 | 270 | -60 | 54 | |||
| APD415210 | 433588.23 | 6830295.5 | 414.72 | 270 | -60 | 60 | |||
| APD415211 | 433595.66 | 6830295.4 | 414.69 | 270 | -60 | 60 | |||
| APD415212 | 433603.8 | 6830295.3 | 414.83 | 270 | -60 | 48 | |||
| APD415217 | 433575 | 6830283 | 415 | 270 | -60 | 42 | |||
| APD415218 | 433585.48 | 6830283.1 | 414.49 | 270 | -60 | 54 | |||
| APD415219 | 433597.44 | 6830283.1 | 414.62 | 270 | -60 | 48 | |||
| APD415220 | 433606 | 6830283 | 415 | 270 | -60 | 48 | |||
| APD415224 | 433568.99 | 6830270.5 | 414.42 | 270 | -60 | 42 | |||
| APD415225 | 433576.97 | 6830270.4 | 414.43 | 270 | -60 | 54 |
| Criteria | Explanation | Explanation | |||||||
|---|---|---|---|---|---|---|---|---|---|
| APD415226 | 433585.1 | 6830270.5 | 414.55 | 270 | -60 | 48 | |||
| APD415227 | 433592.75 | 6830270.4 | 414.65 | 270 | -60 | 48 | |||
| APD415232 | 433554.74 | 6830257.8 | 414.5 | 270 | -60 | 36 | |||
| APD415233 | 433566.99 | 6830257.8 | 414.61 | 270 | -60 | 48 | |||
| APD415234 | 433579.7 | 6830257.9 | 414.34 | 270 | -60 | 48 | |||
| APD415235 | 433587.04 | 6830258 | 414.61 | 270 | -60 | 54 | |||
| APD415237 | 433611.35 | 6830258.1 | 414.71 | 270 | -60 | 12 | |||
| APD415241 | 433548.06 | 6830245.4 | 414.8 | 270 | -60 | 36 | |||
| APD415242 | 433554.89 | 6830245.5 | 414.92 | 270 | -60 | 42 | |||
| APD415243 | 433562.02 | 6830245.4 | 414.77 | 270 | -60 | 42 | |||
| APD415244 | 433568.94 | 6830245.3 | 414.6 | 270 | -60 | 42 | |||
| APD415245 | 433575.76 | 6830245.4 | 414.52 | 270 | -60 | 42 | |||
| APD415246 | 433582.81 | 6830245.4 | 414.47 | 270 | -60 | 36 | |||
| APD415247 | 433590.84 | 6830245.3 | 414.54 | 270 | -60 | 36 | |||
| APD415250 | 433539.38 | 6830233.3 | 414.65 | 270 | -60 | 30 | |||
| APD415251 | 433558.18 | 6830233.1 | 414.86 | 270 | -60 | 42 | |||
| APD415255 | 433532.7 | 6830220.4 | 414.54 | 270 | -60 | 30 | |||
| APD415256 | 433540.24 | 6830220.8 | 414.79 | 270 | -60 | 36 | |||
| APD415257 | 433547 | 6830220.5 | 414.99 | 270 | -59.1 | 42 | |||
| APD415258 | 433554.32 | 6830220.4 | 414.92 | 270 | -60 | 42 | |||
| APD415259 | 433561.07 | 6830220.4 | 414.85 | 270 | -58.7 | 42 | |||
| APD415260 | 433568.16 | 6830220.4 | 414.8 | 270 | -58.4 | 42 | |||
| APD415263 | 433542.03 | 6830207.8 | 414.5 | 270 | -60 | 36 | |||
| APD415264 | 433556.1 | 6830207.9 | 414.49 | 270 | -59.4 | 42 | |||
| APD415267 | 433537.85 | 6830195.4 | 414.55 | 270 | -60 | 36 | |||
| APD415268 | 433546.05 | 6830195.4 | 414.52 | 270 | -58.8 | 42 | |||
| APD415269 | 433553.73 | 6830195.3 | 414.48 | 270 | -57.9 | 42 | |||
| APD415272 | 433536.86 | 6830183 | 415.04 | 270 | -60 | 36 | |||
| APD415273 | 433547.74 | 6830182.9 | 414.84 | 270 | -58.1 | 42 | |||
| APD415276 | 433535.8 | 6830170.4 | 414.94 | 270 | -59.1 | 42 | |||
| APD415277 | 433543.68 | 6830170.3 | 414.83 | 270 | -59.3 | 42 | |||
| APD415278 | 433551.92 | 6830170.5 | 414.88 | 270 | -58.5 | 42 | |||
| APD415281 | 433533.37 | 6830157.9 | 415.11 | 270 | -60 | 36 | |||
| APD415282 | 433546.07 | 6830157.9 | 414.8 | 270 | -58.5 | 42 | |||
| APD415285 | 433530.87 | 6830145.4 | 415.09 | 270 | -59.7 | 42 | |||
| APD415286 | 433538.66 | 6830145.5 | 415 | 270 | -60 | 42 | |||
| APD415289 | 433525.84 | 6830133.1 | 414.82 | 270 | -60.5 | 42 | |||
| APD415290 | 433537.04 | 6830133 | 414.91 | 270 | -59.4 | 42 | |||
| APD415291 | 433544.94 | 6830132.9 | 414.83 | 270 | -59.2 | 48 | |||
| APD415305 | 433575.93 | 6830083 | 414.72 | 270 | -60 | 24 | |||
| APD415309 | 433577.96 | 6830070.5 | 414.97 | 270 | -60 | 24 | |||
| APD415310 | 433559.81 | 6830057.8 | 414.94 | 282 | -89.2 | 54 | |||
| APD415311 | 433579.7 | 6830057.9 | 415.14 | 270 | -60 | 30 | |||
| APD415320 | 433568.06 | 6830020.5 | 414.8 | 270 | -60 | 36 | |||
| APD415323 | 433528.92 | 6829995.5 | 410.89 | 270 | -60 | 36 | |||
| APD415324 | 433544.19 | 6829995.7 | 414.82 | 270 | -59.5 | 42 | |||
| APD415325 | 433556.9 | 6829995.7 | 414.92 | 270 | -59.6 | 42 | |||
| APD415326 | 433529.47 | 6829982.9 | 412.03 | 270 | -60 | 36 | |||
| APD415327 | 433551.52 | 6829983.7 | 411.28 | 270 | -60 | 36 | |||
| APD415329 | 433529.7 | 6829970 | 412.75 | 270 | -60 | 40 | |||
| APD415330 | 433540.83 | 6829970.4 | 412.34 | 270 | -60 | 40 | |||
| ECGC0007 | 434102.07 | 6831327.6 | 441.48 | 270 | -60 | 48 | |||
| ECGC0029 | 434112.15 | 6831387.4 | 442.67 | 270 | -60 | 48 | |||
| ECGC0030 | 434101.8 | 6831387.8 | 442.4 | 270 | -60 | 48 | |||
| ECGC0044 | 434084.84 | 6831417.6 | 442.25 | 270 | -60 | 30 | |||
| ECGC41505 | 434105.98 | 6831310.9 | 414.28 | 270 | -60 | 24 | |||
| ECGC41506 | 434098.84 | 6831311.8 | 414.47 | 270 | -60 | 24 | |||
| ECGC41508 | 434114 | 6831319.4 | 414.6 | 270 | -70 | 36 | |||
| ECGC41509 | 434105.98 | 6831320 | 414.5 | 270 | -60 | 33 | |||
| ECGC41510 | 434098.18 | 6831320.5 | 414.66 | 270 | -60 | 30 | |||
| ECGC41513 | 434111.51 | 6831329.4 | 414.86 | 270 | -65 | 38 | |||
| ECGC41515 | 434102.44 | 6831329.5 | 415.02 | 270 | -60 | 30 | |||
| ECGC41516 | 434098.02 | 6831329.4 | 414.98 | 270 | -60 | 30 | |||
| ECGC41517 | 434091.43 | 6831329.8 | 414.99 | 270 | -60 | 24 | |||
| ECGC41520 | 434114.89 | 6831340.1 | 415.22 | 270 | -65 | 36 | |||
| ECGC41521 | 434098.54 | 6831339.8 | 415.18 | 0 | -90 | 36 |
Market Announcement | Page 27 of 50
| Criteria | Explanation | Explanation | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| ECGC41526 434115.64 6831350 415 270 -60 40 ECGC41527 434109.64 6831350 415 270 -60 36 ECGC41532 434116.79 6831359.8 415.09 270 -60 36 ECGC41534 434094.33 6831360.2 414.89 270 -60 24 ECGC41536 434109.56 6831369.6 414.82 270 -60 30 ECGC41537 434104.2 6831369.9 414.82 270 -60 30 ECGC41538 434098.63 6831370.2 414.93 270 -60 24 ECGC41541 434102.26 6831380.1 415.04 270 -60 24 ECGC41542 434095.6 6831379.8 414.78 270 -60 24 ECGC41544 434102.3 6831390 414.96 270 -60 24 ECGC41545 434090.75 6831390 414.93 270 -60 18 ECGC41548 434086.08 6831399.5 414.85 270 -60 12 West Laverton Historic drilling information has been validated against publicly available WAMEX reports. Not all drill holes can be found referenced in the WAMEX reports. However, cross-checking of original drill surveys was verified against the database. Company Drill Hole Number WAMEX Report A- Number WAMEX Report Date HILLMIN WL10, WL11, WL12, WL13, WL15, WL18, WL7, WL8, WL9 17871 Dec-85 WL26, WL30, WL31, WL32, WL33 20650 Feb-87 BD1, BD3, BD4, BD5 23452 Feb-88 WL34, WL35, WL36, WL37, WL38, WL39, WL40, WL41, WL42, WL43, WL44 23455 Feb-88 BD8, BD9, BD10, BD11, BD12, BD13, BD14, BD15, BD16, BD17, BD18, BD19, BD20, BD21, BD22, BD23, BD24, BD25, BD26, BD27, BD28, BD31, BD32, BD33, BD34, BD35, BD37, BD38, BD39, BD40, BD41, BD42, BD7, WL101, WL102, WL103, WL105, WL106, WL107, WL110, WL111, WL112, WL113, WL114, WL115, WL116, WL117, WL118, WL119, WL120, WL121, WL51, WL52, WL53, WL54, WL55, WL56, WL58, WL59, WL60, WL61, WL62, WL63, WL64, WL65, WL66, WL67, WL68, WL70, WL71, WL72, WL73, WL75, WL76, WL77, WL78, WL80, WL81, WL82, WL83, WL84, WL86, WL88, WL89, WL90, WL91, WL92, WL95, WL96, WL97, WL98, WL99, WLD1, WLD10, WLD11, WLD12, WLD2, WLD3, WLD4, WLD5, WLD6, WLD7, WLD8, WLD9 27622 Jun-88 ASHTON BD100_WESTLA, BD101_WESTLA, BD103_WESTLA, BD105_WESTLA, BD107_WESTLA, BD108_WESTLA, BD109_WESTLA, BD110_WESTLA, BD111_WESTLA, BD112_WESTLA, BD113_WESTLA, BD114_WESTLA, BD115_WESTLA, BD116_WESTLA, BD117_WESTLA, BD118_WESTLA, BD121_WESTLA, BD122_WESTLA, BD123_WESTLA, BD126, BD127, BD45, BD46, BD47, BD50, BD51, BD52, BD56, BD57, BD58, BD59, BD62, BD67, BD69, BD70, BD73, BD74, BD75, BD76, BD78, BD79, BD80, BD81, BD82, BD83, BD85, BD86, BD91, BD94, BD95, BD97, BD98, BDD1, BDD2, BDD3, BDD4, WL122, WL123, WL124, WL125, WL126, WL127, WL128, WL129, WL130, WL131, WL132, WL133, WL134, WL135, WL136, WL137, WL138, WL139, WL140, WL141, WL142, WL143, WL144, WL145, WL146, WL147, WL148, WL149, WL150, WL151, WL152, WL163, WL164, WL165, WL166, WL167, WL168, WL169, WL170, WL171, WL172 30496 Jan-90 WL173, WL174, WL175, WL176, WL177, WL178, WL180, WL181, WL183, WL186, WL187, WL188, WL190, WL191, WL192, WL193, WL194, WL196, WL197, WL198, WL200, WL201, WL202, WL203, WL204, WL210, WL211, WL212, WL213, WL214, WL215, WL216, WL217, WL218, WL219, WL220, WL221, WL222, WL223, WL225, WL226, WL227, WL228, WL229, WL230, WL232, WL233, WL234, WL235, WL236, WL237, WL238, WL239, WL240 35703 Dec-91 SOG ENC002, ENC003, ENC004, ENC005, ENC006, ENC007, ENC008, ENC009, ENC011, ENC012, ENC013 51454 May-97 |
ECGC41526 | 434115.64 | 6831350 | 415 | 270 | -60 | 40 | ||||
| ECGC41527 | 434109.64 | 6831350 | 415 | 270 | -60 | 36 | |||||
| ECGC41532 | 434116.79 | 6831359.8 | 415.09 | 270 | -60 | 36 | |||||
| ECGC41534 | 434094.33 | 6831360.2 | 414.89 | 270 | -60 | 24 | |||||
| ECGC41536 | 434109.56 | 6831369.6 | 414.82 | 270 | -60 | 30 | |||||
| ECGC41537 | 434104.2 | 6831369.9 | 414.82 | 270 | -60 | 30 | |||||
| ECGC41538 | 434098.63 | 6831370.2 | 414.93 | 270 | -60 | 24 | |||||
| ECGC41541 | 434102.26 | 6831380.1 | 415.04 | 270 | -60 | 24 | |||||
| ECGC41542 | 434095.6 | 6831379.8 | 414.78 | 270 | -60 | 24 | |||||
| ECGC41544 | 434102.3 | 6831390 | 414.96 | 270 | -60 | 24 | |||||
| ECGC41545 | 434090.75 | 6831390 | 414.93 | 270 | -60 | 18 | |||||
| ECGC41548 | 434086.08 | 6831399.5 | 414.85 | 270 | -60 | 12 | |||||
| Company | Drill Hole Number | WAMEX Report A- Number |
WAMEX Report Date |
||||||||
| HILLMIN | WL10, WL11, WL12, WL13, WL15, WL18, WL7, WL8, WL9 | 17871 | Dec-85 | ||||||||
| WL26, WL30, WL31, WL32, WL33 | 20650 | Feb-87 | |||||||||
| BD1, BD3, BD4, BD5 | 23452 | Feb-88 | |||||||||
| WL34, WL35, WL36, WL37, WL38, WL39, WL40, WL41, WL42, WL43, WL44 | 23455 | Feb-88 | |||||||||
| BD8, BD9, BD10, BD11, BD12, BD13, BD14, BD15, BD16, BD17, BD18, BD19, BD20, BD21, BD22, BD23, BD24, BD25, BD26, BD27, BD28, BD31, BD32, BD33, BD34, BD35, BD37, BD38, BD39, BD40, BD41, BD42, BD7, WL101, WL102, WL103, WL105, WL106, WL107, WL110, WL111, WL112, WL113, WL114, WL115, WL116, WL117, WL118, WL119, WL120, WL121, WL51, WL52, WL53, WL54, WL55, WL56, WL58, WL59, WL60, WL61, WL62, WL63, WL64, WL65, WL66, WL67, WL68, WL70, WL71, WL72, WL73, WL75, WL76, WL77, WL78, WL80, WL81, WL82, WL83, WL84, WL86, WL88, WL89, WL90, WL91, WL92, WL95, WL96, WL97, WL98, WL99, WLD1, WLD10, WLD11, WLD12, WLD2, WLD3, WLD4, WLD5, WLD6, WLD7, WLD8, WLD9 |
27622 | Jun-88 | |||||||||
| ASHTON | BD100_WESTLA, BD101_WESTLA, BD103_WESTLA, BD105_WESTLA, BD107_WESTLA, BD108_WESTLA, BD109_WESTLA, BD110_WESTLA, BD111_WESTLA, BD112_WESTLA, BD113_WESTLA, BD114_WESTLA, BD115_WESTLA, BD116_WESTLA, BD117_WESTLA, BD118_WESTLA, BD121_WESTLA, BD122_WESTLA, BD123_WESTLA, BD126, BD127, BD45, BD46, BD47, BD50, BD51, BD52, BD56, BD57, BD58, BD59, BD62, BD67, BD69, BD70, BD73, BD74, BD75, BD76, BD78, BD79, BD80, BD81, BD82, BD83, BD85, BD86, BD91, BD94, BD95, BD97, BD98, BDD1, BDD2, BDD3, BDD4, WL122, WL123, WL124, WL125, WL126, WL127, WL128, WL129, WL130, WL131, WL132, WL133, WL134, WL135, WL136, WL137, WL138, WL139, WL140, WL141, WL142, WL143, WL144, WL145, WL146, WL147, WL148, WL149, WL150, WL151, WL152, WL163, WL164, WL165, WL166, WL167, WL168, WL169, WL170, WL171, WL172 |
30496 | Jan-90 | ||||||||
| WL173, WL174, WL175, WL176, WL177, WL178, WL180, WL181, WL183, WL186, WL187, WL188, WL190, WL191, WL192, WL193, WL194, WL196, WL197, WL198, WL200, WL201, WL202, WL203, WL204, WL210, WL211, WL212, WL213, WL214, WL215, WL216, WL217, WL218, WL219, WL220, WL221, WL222, WL223, WL225, WL226, WL227, WL228, WL229, WL230, WL232, WL233, WL234, WL235, WL236, WL237, WL238, WL239, WL240 |
35703 | Dec-91 | |||||||||
| SOG | ENC002, ENC003, ENC004, ENC005, ENC006, ENC007, ENC008, ENC009, ENC011, ENC012, ENC013 |
51454 | May-97 |
| Criteria | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | |||
|---|---|---|---|---|---|---|---|---|---|
| ENC286, ENC289 ENC457, ENC458, ENC459, ENC460, ENC461, ENC462 |
55360 | Nov-97 | |||||||
| 62396 | Feb-01 | ||||||||
| APOLLO | WV018, WV019, WV020, WV021, WV023, WV024, WV025, WV026, WV027 | 68420 | Apr-04 | ||||||
| CRESCENT | WV029, WV030, WV031, WV032, WV033, WV034, WV035, WV036, WV037, WV038, WV039, WV040, WV041, WV044, WV045, WV046, WV047 WLDD001, WLDD002, WLDD003, WLRC200, WLRC201, WLRC202, WLRC203, WLRC204, WLRC205, WLRC207 WLRC209, WLRC210, WLRC211, WLRC212, WLRC213, WLRC215, WLRC217, WLRC218, WLRC219, WLRC220, WLRC222, WLRC223, WLRC224, WLRC225, WLRC226, WLRC227, WLRC228, WLRC229, WLRC230, WLRC231, WLRC232, WLRC233, WLRC234, WLRC235, WLRC240, WLRC241, WLRC242, WLRC243, WLRC244, WLRC245, WLRC246 WLRC247, WLRC248, WLRC249, WLRC250, WLRC251, WLRC252, WLRC253, WLRC254, WLRC255, WLRC256, WLRC257, WLRC258, WLRC259, WLRC260, WLRC261, WLRC262, WLRC263, WLRC264, WLRC265, WLRC266, WLRC267, WLRC268 WLRC269, WLRC270, WLRC271, WLRC272, WLRC273, WLRC274, WLRC275, WLRC276, WLRC277 |
74767 | Mar-07 | ||||||
| 81229 | Feb-09 | ||||||||
| 86387 | Feb-10 | ||||||||
| 90143 | Apr-11 | ||||||||
| 98404 | Jun-13 | ||||||||
| FOCUS | WLDD004, WLDD005, WLDD006 | 102282 | Jun-14 | ||||||
| West Laverton collar details of holes not previously externally reported: | |||||||||
| COMPANY | DRILL | HOLE ID | MGA 94 Zone 51 | DEPTH (m) | |||||
| TYPE | EAST | NORTH | RL | AZIMUTH | DIP | ||||
| WMC | RC | RGAC1 | 438822.98 | 6833124.1 | 453.06 | 255 | -60 | 20 | |
| WMC | RC | RGAC12 | 438845.71 | 6833090.8 | 453.81 | 255 | -60 | 30 | |
| WMC | RC | RGAC13 | 438864.36 | 6833096.6 | 453.94 | 255 | -60 | 40 | |
| WMC | RC | RGAC18 | 438892.72 | 6833194.8 | 452.85 | 255 | -60 | 40 | |
| WMC | RC | RGAC22 | 439007.55 | 6833208.9 | 453.99 | 255 | -60 | 20 | |
| WMC | RC | RGAC23 | 439026.74 | 6833215.8 | 454.28 | 255 | -60 | 30 | |
| WMC | RC | RGAC24 | 439010.96 | 6833168.3 | 454.61 | 255 | -60 | 20 | |
| WMC | RC | RGAC25 | 439029.13 | 6833176.5 | 454.81 | 255 | -60 | 30 | |
| WMC | RC | RGAC26 | 439044.89 | 6833222.4 | 454.58 | 255 | -60 | 40 | |
| WMC | RC | RGAC27 | 438994.8 | 6833184.4 | 454.19 | 255 | -60 | 20 | |
| WMC | RC | RGAC28 | 439013.41 | 6833190.5 | 454.32 | 255 | -60 | 30 | |
| WMC | RC | RGAC29 | 439032.79 | 6833196.9 | 454.64 | 255 | -60 | 40 | |
| WMC | RC | RGAC31 | 439007.94 | 6833146.2 | 454.9 | 255 | -60 | 30 | |
| WMC | RC | RGAC32 | 439027.06 | 6833152.3 | 455.06 | 255 | -60 | 40 | |
| WMC | RC | RGAC33 | 439045.81 | 6833158.9 | 455.38 | 255 | -60 | 40 | |
| SOG | RC | WLRC023 | 439043.34 | 6832760.2 | 454.1 | 0 | -90 | 65 | |
| SOG | RC | WLRC025 | 438882.88 | 6832784.5 | 453.18 | 0 | -90 | 25 | |
| SOG | RC | WLRC026 | 438903.53 | 6832784.7 | 453.31 | 0 | -90 | 35 | |
| SOG | RC | WLRC027 | 438923.04 | 6832784.4 | 453.48 | 0 | -90 | 45 | |
| SOG | RC | WLRC028 | 438942.93 | 6832785.9 | 453.45 | 0 | -90 | 50 | |
| SOG | RC | WLRC030 | 438887.98 | 6832809.2 | 453.05 | 0 | -90 | 25 | |
| SOG | RC | WLRC032 | 438879.23 | 6832834.3 | 453.02 | 0 | -90 | 30 | |
| SOG | RC | WLRC033 | 438899.81 | 6832834.8 | 453.17 | 0 | -90 | 40 | |
| SOG | RC | WLRC034 | 438917.8 | 6832835 | 453.47 | 0 | -90 | 50 | |
| SOG | RC | WLRC035 | 438938.08 | 6832834.8 | 453.74 | 0 | -90 | 60 | |
| SOG | RC | WLRC036 | 438958.76 | 6832834.7 | 453.98 | 0 | -90 | 70 | |
| SOG | RC | WLRC037 | 438977.87 | 6832834.6 | 453.97 | 0 | -90 | 85 | |
| SOG | RC | WLRC038 | 438998.21 | 6832834.9 | 454 | 0 | -90 | 40 | |
| SOG | RC | WLRC039 | 438858.82 | 6832859.8 | 453.51 | 0 | -90 | 15 | |
| SOG | RC | WLRC040 | 438902.92 | 6832859.5 | 453.55 | 0 | -90 | 40 | |
| SOG | RC | WLRC041 | 438925.04 | 6832859.5 | 453.63 | 0 | -90 | 50 |
Market Announcement | Page 29 of 50
| Criteria | Explanation | Explanation | Explanation | Explanation | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| SOG | RC | WLRC042 | 438943.5 | 6832859.1 | 453.65 | 0 | -90 | 60 | ||||||
| SOG | RC | WLRC043 | 438963.12 | 6832859.9 | 453.58 | 0 | -90 | 70 | ||||||
| SOG | RC | WLRC044 | 438988.07 | 6832859.6 | 453.38 | 0 | -90 | 85 | ||||||
| SOG | RC | WLRC045 | 439033.54 | 6832860.1 | 453.52 | 0 | -90 | 100 | ||||||
| SOG | RC | WLRC046 | 438858.12 | 6832884.9 | 453.11 | 0 | -90 | 25 | ||||||
| SOG | RC | WLRC047 | 438877.91 | 6832884.7 | 453.42 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC048 | 438898.49 | 6832885 | 453.44 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC049 | 438918.35 | 6832885 | 453.17 | 0 | -90 | 45 | ||||||
| SOG | RC | WLRC050 | 438938.73 | 6832884.7 | 452.91 | 0 | -90 | 55 | ||||||
| SOG | RC | WLRC051 | 438958.4 | 6832885.1 | 452.99 | 0 | -90 | 65 | ||||||
| SOG | RC | WLRC052 | 438979.52 | 6832887.2 | 453.05 | 0 | -90 | 75 | ||||||
| SOG | RC | WLRC053 | 438997.35 | 6832883.2 | 453.16 | 0 | -90 | 85 | ||||||
| SOG | RC | WLRC054 | 439019.66 | 6832884.9 | 453.27 | 0 | -90 | 100 | ||||||
| SOG | RC | WLRC055 | 439037.9 | 6832884.8 | 453.36 | 0 | -90 | 40 | ||||||
| SOG | RC | WLRC056 | 438867.66 | 6832908.7 | 452.77 | 0 | -90 | 30 | ||||||
| SOG | RC | WLRC058 | 438912.23 | 6832909.4 | 452.82 | 0 | -90 | 40 | ||||||
| SOG | RC | WLRC060 | 438988.39 | 6832909.9 | 452.89 | 0 | -90 | 40 | ||||||
| SOG | RC | WLRC061 | 438867.93 | 6832934.8 | 452.24 | 0 | -90 | 30 | ||||||
| SOG | RC | WLRC062 | 438888.32 | 6832934.7 | 452.38 | 0 | -90 | 40 | ||||||
| SOG | RC | WLRC063 | 438908.54 | 6832934.9 | 452.47 | 0 | -90 | 40 | ||||||
| SOG | RC | WLRC064 | 438928.1 | 6832934.5 | 452.58 | 0 | -90 | 55 | ||||||
| SOG | RC | WLRC065 | 438947.95 | 6832934.4 | 452.73 | 0 | -90 | 65 | ||||||
| SOG | RC | WLRC066 | 438968 | 6832935.2 | 452.83 | 0 | -90 | 80 | ||||||
| SOG | RC | WLRC067 | 438988.23 | 6832934.5 | 452.86 | 0 | -90 | 60 | ||||||
| SOG | RC | WLRC068 | 439007.92 | 6832935.5 | 453 | 0 | -90 | 70 | ||||||
| SOG | RC | WLRC069 | 438873.1 | 6832960.3 | 451.91 | 0 | -90 | 30 | ||||||
| SOG | RC | WLRC070 | 438893.63 | 6832959.6 | 452.17 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC071 | 438912.73 | 6832959.9 | 452.44 | 0 | -90 | 45 | ||||||
| SOG | RC | WLRC072 | 438948.24 | 6832959.5 | 452.65 | 0 | -90 | 65 | ||||||
| SOG | RC | WLRC073 | 438967.95 | 6832959.5 | 452.93 | 0 | -90 | 75 | ||||||
| SOG | RC | WLRC076 | 438957.9 | 6832984.4 | 452.51 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC077 | 438978.24 | 6832984.7 | 452.74 | 0 | -90 | 50 | ||||||
| SOG | RC | WLRC078 | 438998.02 | 6832985 | 452.85 | 0 | -90 | 60 | ||||||
| SOG | RC | WLRC079 | 439017.8 | 6832988.4 | 452.88 | 0 | -90 | 70 | ||||||
| SOG | RC | WLRC084 | 438962.64 | 6833036.5 | 452.32 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC086 | 438871.56 | 6832990.6 | 451.97 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC087 | 438877.12 | 6833040.5 | 451.78 | 0 | -90 | 35 | ||||||
| SOG | RC | WLRC100 | 439062.68 | 6832985.9 | 453.01 | 0 | -60 | 102 | ||||||
| SOG | RC | WLRC101 | 439041.76 | 6832992.7 | 452.93 | 0 | -60 | 90 | ||||||
| SOG | RC | WLRC102 | 439019.58 | 6833006.8 | 452.74 | 0 | -60 | 74 | ||||||
| SOG | RC | WLRC103 | 439001.03 | 6833007.5 | 452.77 | 0 | -60 | 66 | ||||||
| SOG | RC | WLRC104 | 438967.14 | 6833011.1 | 452.34 | 0 | -60 | 54 | ||||||
| SOG | RC | WLRC106 | 438877.48 | 6832861.5 | 453.22 | 0 | -90 | 25 | ||||||
| SOG | RC | WLRC107 | 439012.66 | 6832834.9 | 454.26 | 0 | -90 | 100 | ||||||
| SOG | RC | WLRC108 | 439050.07 | 6832985.9 | 452.94 | 0 | -90 | 90 | ||||||
| West Laverton shallow Crescent RC grade control holes not externally reported: | ||||||||||||||
| COANY | DRILL | HOLE ID | MGA 94 Zone 51 | DEPTH | ||||||||||
| MP | TYPE | EAST | NORTH | RL | AZIMUTH | DIP | ||||||||
| WMC | RC | RGAC1 | 438822.98 | 6833124.1 | 453.06 | 255 | -60 | 20 | ||||||
| WMC | RC | RGAC12 | 438845.71 | 6833090.8 | 453.81 | 255 | -60 | 30 | ||||||
| WMC | RC | RGAC13 | 438864.36 | 6833096.6 | 453.94 | 255 | -60 | 40 |
| Criteria | Explanation | Explanation | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| WMC | RC | RGAC18 | 438892.72 | 6833194.8 | 452.85 | 255 | -60 | 40 | ||
| WMC | RC | RGAC22 | 439007.55 | 6833208.9 | 453.99 | 255 | -60 | 20 | ||
| WMC | RC | RGAC23 | 439026.74 | 6833215.8 | 454.28 | 255 | -60 | 30 | ||
| WMC | RC | RGAC24 | 439010.96 | 6833168.3 | 454.61 | 255 | -60 | 20 | ||
| WMC | RC | RGAC25 | 439029.13 | 6833176.5 | 454.81 | 255 | -60 | 30 | ||
| WMC | RC | RGAC26 | 439044.89 | 6833222.4 | 454.58 | 255 | -60 | 40 | ||
| WMC | RC | RGAC27 | 438994.8 | 6833184.4 | 454.19 | 255 | -60 | 20 | ||
| WMC | RC | RGAC28 | 439013.41 | 6833190.5 | 454.32 | 255 | -60 | 30 | ||
| WMC | RC | RGAC29 | 439032.79 | 6833196.9 | 454.64 | 255 | -60 | 40 | ||
| WMC | RC | RGAC31 | 439007.94 | 6833146.2 | 454.9 | 255 | -60 | 30 | ||
| WMC | RC | RGAC32 | 439027.06 | 6833152.3 | 455.06 | 255 | -60 | 40 | ||
| WMC | RC | RGAC33 | 439045.81 | 6833158.9 | 455.38 | 255 | -60 | 40 | ||
| SOG | RC | WLRC023 | 439043.34 | 6832760.2 | 454.1 | 0 | -90 | 65 | ||
| SOG | RC | WLRC025 | 438882.88 | 6832784.5 | 453.18 | 0 | -90 | 25 | ||
| SOG | RC | WLRC026 | 438903.53 | 6832784.7 | 453.31 | 0 | -90 | 35 | ||
| SOG | RC | WLRC027 | 438923.04 | 6832784.4 | 453.48 | 0 | -90 | 45 | ||
| SOG | RC | WLRC028 | 438942.93 | 6832785.9 | 453.45 | 0 | -90 | 50 | ||
| SOG | RC | WLRC030 | 438887.98 | 6832809.2 | 453.05 | 0 | -90 | 25 | ||
| SOG | RC | WLRC032 | 438879.23 | 6832834.3 | 453.02 | 0 | -90 | 30 | ||
| SOG | RC | WLRC033 | 438899.81 | 6832834.8 | 453.17 | 0 | -90 | 40 | ||
| SOG | RC | WLRC034 | 438917.8 | 6832835 | 453.47 | 0 | -90 | 50 | ||
| SOG | RC | WLRC035 | 438938.08 | 6832834.8 | 453.74 | 0 | -90 | 60 | ||
| SOG | RC | WLRC036 | 438958.76 | 6832834.7 | 453.98 | 0 | -90 | 70 | ||
| SOG | RC | WLRC037 | 438977.87 | 6832834.6 | 453.97 | 0 | -90 | 85 | ||
| SOG | RC | WLRC038 | 438998.21 | 6832834.9 | 454 | 0 | -90 | 40 | ||
| SOG | RC | WLRC039 | 438858.82 | 6832859.8 | 453.51 | 0 | -90 | 15 | ||
| SOG | RC | WLRC040 | 438902.92 | 6832859.5 | 453.55 | 0 | -90 | 40 | ||
| SOG | RC | WLRC041 | 438925.04 | 6832859.5 | 453.63 | 0 | -90 | 50 | ||
| SOG | RC | WLRC042 | 438943.5 | 6832859.1 | 453.65 | 0 | -90 | 60 | ||
| SOG | RC | WLRC043 | 438963.12 | 6832859.9 | 453.58 | 0 | -90 | 70 | ||
| SOG | RC | WLRC044 | 438988.07 | 6832859.6 | 453.38 | 0 | -90 | 85 | ||
| SOG | RC | WLRC045 | 439033.54 | 6832860.1 | 453.52 | 0 | -90 | 100 | ||
| SOG | RC | WLRC046 | 438858.12 | 6832884.9 | 453.11 | 0 | -90 | 25 | ||
| SOG | RC | WLRC047 | 438877.91 | 6832884.7 | 453.42 | 0 | -90 | 35 | ||
| SOG | RC | WLRC048 | 438898.49 | 6832885 | 453.44 | 0 | -90 | 35 | ||
| SOG | RC | WLRC049 | 438918.35 | 6832885 | 453.17 | 0 | -90 | 45 | ||
| SOG | RC | WLRC050 | 438938.73 | 6832884.7 | 452.91 | 0 | -90 | 55 | ||
| SOG | RC | WLRC051 | 438958.4 | 6832885.1 | 452.99 | 0 | -90 | 65 | ||
| SOG | RC | WLRC052 | 438979.52 | 6832887.2 | 453.05 | 0 | -90 | 75 | ||
| SOG | RC | WLRC053 | 438997.35 | 6832883.2 | 453.16 | 0 | -90 | 85 | ||
| SOG | RC | WLRC054 | 439019.66 | 6832884.9 | 453.27 | 0 | -90 | 100 | ||
| SOG | RC | WLRC055 | 439037.9 | 6832884.8 | 453.36 | 0 | -90 | 40 | ||
| SOG | RC | WLRC056 | 438867.66 | 6832908.7 | 452.77 | 0 | -90 | 30 | ||
| SOG | RC | WLRC058 | 438912.23 | 6832909.4 | 452.82 | 0 | -90 | 40 | ||
| SOG | RC | WLRC060 | 438988.39 | 6832909.9 | 452.89 | 0 | -90 | 40 | ||
| SOG | RC | WLRC061 | 438867.93 | 6832934.8 | 452.24 | 0 | -90 | 30 | ||
| SOG | RC | WLRC062 | 438888.32 | 6832934.7 | 452.38 | 0 | -90 | 40 | ||
| SOG | RC | WLRC063 | 438908.54 | 6832934.9 | 452.47 | 0 | -90 | 40 | ||
| SOG | RC | WLRC064 | 438928.1 | 6832934.5 | 452.58 | 0 | -90 | 55 | ||
| SOG | RC | WLRC065 | 438947.95 | 6832934.4 | 452.73 | 0 | -90 | 65 | ||
| SOG | RC | WLRC066 | 438968 | 6832935.2 | 452.83 | 0 | -90 | 80 | ||
| SOG | RC | WLRC067 | 438988.23 | 6832934.5 | 452.86 | 0 | -90 | 60 | ||
| SOG | RC | WLRC068 | 439007.92 | 6832935.5 | 453 | 0 | -90 | 70 | ||
| SOG | RC | WLRC069 | 438873.1 | 6832960.3 | 451.91 | 0 | -90 | 30 | ||
| SOG | RC | WLRC070 | 438893.63 | 6832959.6 | 452.17 | 0 | -90 | 35 | ||
| SOG | RC | WLRC071 | 438912.73 | 6832959.9 | 452.44 | 0 | -90 | 45 | ||
| SOG | RC | WLRC072 | 438948.24 | 6832959.5 | 452.65 | 0 | -90 | 65 | ||
| SOG | RC | WLRC073 | 438967.95 | 6832959.5 | 452.93 | 0 | -90 | 75 | ||
| SOG | RC | WLRC076 | 438957.9 | 6832984.4 | 452.51 | 0 | -90 | 35 | ||
| SOG | RC | WLRC077 | 438978.24 | 6832984.7 | 452.74 | 0 | -90 | 50 | ||
| SOG | RC | WLRC078 | 438998.02 | 6832985 | 452.85 | 0 | -90 | 60 | ||
| SOG | RC | WLRC079 | 439017.8 | 6832988.4 | 452.88 | 0 | -90 | 70 | ||
| SOG | RC | WLRC084 | 438962.64 | 6833036.5 | 452.32 | 0 | -90 | 35 | ||
| SOG | RC | WLRC086 | 438871.56 | 6832990.6 | 451.97 | 0 | -90 | 35 | ||
| SOG | RC | WLRC087 | 438877.12 | 6833040.5 | 451.78 | 0 | -90 | 35 | ||
| SOG | RC | WLRC100 | 439062.68 | 6832985.9 | 453.01 | 0 | -60 | 102 |
Market Announcement | Page 31 of 50
| Criteria | Explanation | Explanation | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| SOG | RC | WLRC101 | 439041.76 | 6832992.7 | 452.93 | 0 | -60 | 90 | ||||
| SOG | RC | WLRC102 | 439019.58 | 6833006.8 | 452.74 | 0 | -60 | 74 | ||||
| SOG | RC | WLRC103 | 439001.03 | 6833007.5 | 452.77 | 0 | -60 | 66 | ||||
| SOG | RC | WLRC104 | 438967.14 | 6833011.1 | 452.34 | 0 | -60 | 54 | ||||
| SOG | RC | WLRC106 | 438877.48 | 6832861.5 | 453.22 | 0 | -90 | 25 | ||||
| SOG | RC | WLRC107 | 439012.66 | 6832834.9 | 454.26 | 0 | -90 | 100 | ||||
| SOG | RC | WLRC108 | 439050.07 | 6832985.9 | 452.94 | 0 | -90 | 90 | ||||
| Gladiator Historic drilling information has been validated holes can be found referenced in the WAMEX was verified against the database. |
||||||||||||
| Company | Drill Hole Number | WAMEX Report A- Number |
WAMEX Report Date |
|||||||||
| Teck Exploration Ltd |
GP1,GP2 | 11969 | 01-Jan-83 | |||||||||
| Technominerals | GRC1,GRC3 | 20213 | 01-Mar-87 | |||||||||
| Hill Minerals | GP7,GP8 | 15071 | 01-Mar-85 | |||||||||
| GP11,GP12,GP14,GP16,GP17,GP18 | 17467 | 01-Feb-86 | ||||||||||
| GP25,GP26,GP27,GP28,GP29,GP30 | 27702 | 01-Dec-88 | ||||||||||
| GP31,GP32,GP33,GP34,GP35,GP36,GP37,GP38,GP39,GP40 | 27703 | 01-Feb-89 | ||||||||||
| WMC | TWP107, TWP108, TWP109, TWP110, TWP111, TWP112, TWP113, TWP114 |
22647 | 31-Jan-88 | |||||||||
| TWP175,TWP176,TWP177,TWP178,TWP179,TWP180 | 35126 | 01-Feb-92 | ||||||||||
| Ashton | GP100, GP101, GP116, GP119, GP120, GP123, GP126, GP127, GP130, GP131, GP132, GP135, GP142, GP143, GP144, GP145, GP146, GP147, GP148, GP149, GP151, GP152, GP161, GP162, GP163, GP164, GP168, GP41, GP42, GP43, GP44, GP45, GP46, GP47, GP48, GP49, GP50, GP51, GP52, GP53, GP54, GP55, GP56, GP57, GP58, GP59, GP60, GP61, GP62, GP63, GP64, GP65, GP66, GP67, GP68, GP69, GP70, GP71, GP72, GP73, GP74, GP82, GP83, GP84, GP85, GP86, GP87, GP88, GP89, GP90, GP93, GP94,GP95,GP96,GP97,GP98,GP99,GSD1,GSD2,GSD4,GSD5 |
17957 | 01-Jan-90 | |||||||||
| GP102, GP103, GP105, GP106, GP107, GP109, GP110, GP111, GP112, GP113, GP114, GP115, GP118, GP121, GP122, GP124, GP125, GP128, GP129, GP133, GP134, GP136, GP137, GP138, GP139, GP141, GP150, GP153, GP155, GP156, GP157, GP158, GP159, GP160, GP165, GP169, GP76,GP77,GP78,GP79,GP80,GP81,GSD3,GSD6,GSD7 |
30488 | 01-Jan-90 | ||||||||||
| GP174,GP175,GP176 | 34630 | 01-Sep-91 | ||||||||||
| GP171, GP177, GP178, GP179, GP180, GP181, GP182, GP183, GP184, GP185, GP186, GP187, GP188, GP189, GP190, GP191, GP192, GP193, GP194, GP195, GP196, GP197, GP199, GP200, GP201, GP202, GP203, GP204, GP205, GP206, GP207, GP208, GP209, GP210, GP211, GP212, GP213, GP214, GP215, GP216, GP217, GP218, GP219, GP220, GP221, GP222, GP224, GP225, GP226, GP227, GP228, GP229, GP230, GP231, GP232, GP233, GP234, GP235, GP236, GP237, GP238, GP239, GP240, GP241,GP242 |
34657 | 01-Sep-91 | ||||||||||
| GP244, GP245, GP249, GP251, GP252, GP255, GP256, GP257, GP258, GP259,GP265,GP266,GP270,GP271,GP277 |
35680 | 01-Jan-92 | ||||||||||
| SOG | ENC298, ENC299, ENC301, ENC302, ENC303, ENC306, ENC307, ENC308, ENC310,ENC311,ENC312 |
55360 | 30-Nov-97 | |||||||||
| ENC465 | 62396 | 28-Feb-01 | ||||||||||
| Metex Resources |
GMDH001, GMDH002, GMDH003, GMRC001, GMRC004, GMRC005, GMRC006, GMRC007, GMRC008, GMRC009, GMRC010, GMRC012, GMRC013, GMRC014, GMRC015, GMRC016, GMRC018, GMRC019, GMRC020, GMRC021, GMRC023, GMRC024, GMRC026, GMRC029, GMRC030 |
69813 | 01-Feb-05 | |||||||||
| GMDH004,GMRC049,GMRC031,GMRC032 | 72705 | 01-Mar-06 | ||||||||||
| Metex/Barrick (Granny Smith) PtyLtd |
LJC0014,LJC0015,LJC0016,LJC0017,LJC0018,LJC0032 | 72705 | 01-Mar-06 | |||||||||
| LJC0033, LJC0034, LJC0035, LJC0036 | 75073 | 01-Mar-07 |
| Criteria | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | ||
|---|---|---|---|---|---|---|---|---|---|---|
| Drill Hole ID | ASX Release Title | Date | ||||||||
| 19GLRC001, 19GLRC002, 19GLRC003, 19GLRC004, 19GLRC005,19GLRC006,19GLRC007 |
Strong gold hits from Laverton regional drillingcampaign |
29-Jan-20 | ||||||||
| 21GLRC001, 21GLRC002, 21GLRC003, 21GLRC004, 21GLRC005, 21GLRC006, 21GLRC007, 21GLRC008, 21GLRC009,21GLRC010,21GLRC011 |
Exploration Update - Laverton Gold Project |
28-Apr-21 | ||||||||
| Gladiator Ashton drilled RC holes not externally reported: | ||||||||||
| HOLE ID | MGA 94 | Zone 51 | DEPTH (m) | |||||||
| EAST | NORTH | RL | AZIMUTH | DI P |
||||||
| GP304 | 437617.25 | 6832650.1 | 457.72 | 0 | -90 | 100 | ||||
| GP306 | 437679.17 | 6832638.7 | 456.53 | 0 | -90 | 100 | ||||
| GP307 | 437676.68 | 6832816.9 | 457.76 | 270 | -60 | 65 | ||||
| GP308 | 437701.83 | 6832867.9 | 463.12 | 270 | -60 | 65 | ||||
| GP309 | 437743.55 | 6832840.4 | 464.29 | 270 | -60 | 60 | ||||
| GP310 | 437727.69 | 6832791.5 | 461.85 | 270 | -60 | 60 | ||||
| GP311 | 437724.41 | 6832816.9 | 462.2 | 270 | -60 | 60 | ||||
| GP312 | 437698.71 | 6832742.9 | 460.19 | 270 | -60 | 60 | ||||
| GP313 | 437668.3 | 6832793.9 | 457.33 | 270 | -60 | 68 | ||||
| GP314 | 437699.83 | 6832892.8 | 466.25 | 270 | -60 | 60 | ||||
| GP315 | 437675.8 | 6832868.7 | 460.29 | 270 | -60 | 80 | ||||
| GP316 | 437670.48 | 6832844 | 459.37 | 270 | -60 | 70 | ||||
| GP317 | 437584.32 | 6832999.1 | 459.19 | 0 | -90 | 94 | ||||
| GP318 | 437613.39 | 6833000.1 | 458.24 | 0 | -90 | 118 | ||||
| GP320 | 437722.97 | 6832817.6 | 462.11 | 270 | -60 | 105 | ||||
| GP321 | 437707.93 | 6832793.5 | 460.55 | 270 | -60 | 93 | ||||
| GP322 | 437686.76 | 6832835.1 | 458.37 | 225 | -60 | 81 | ||||
| GP323 | 437699.04 | 6832769.6 | 460.72 | 270 | -60 | 60 | ||||
| GP324 | 437749.16 | 6832766.8 | 460.07 | 270 | -60 | 80 | ||||
| GP325 | 437749.66 | 6832791.6 | 461.16 | 270 | -60 | 100 | ||||
| GP326 | 437750.8 | 6832816.6 | 462.37 | 270 | -60 | 150 | ||||
| GP329 | 437730.26 | 6832792.3 | 461.75 | 270 | -60 | 90 | ||||
| GP5 | 437184.81 | 6832777.8 | 461.74 | 272 | -60 | 42 | ||||
| Company | Drill Hole Number | WAMEX Report A- Number |
WAMEX Report Date |
|||||||
| Hillmin | SL16, SL17, SL18, SL19, SL20, SL21, SL22, SL23, SL26, SL27, SL28, SL29_WESTLAV, SL31, SL32_WESTLAV, SL33, SL34, SL35, SL36, SL37, SL38, SL39,SL40,SL41,SL42,SL43,SL44,SL46 |
14966 | Apr-85 | |||||||
| SL80,SLD1,SLD2,SLD4,SLD6,SLD7,SLD8 | 17424 | Feb-86 | ||||||||
| SL106,SL107,SL108,SL109 | 20572 | Dec-86 | ||||||||
| SL117, SL118, SL119, SL120, SL121, SL122, SL123, SL126, SL127, SL128, SL129, SL130, SL131, SL132, SL133, SL134, SL135, SL136, SL137, SL138, SL140, SL141, SL142, SL143, SL144, SL146, SL147, SL148, SL149, SL150, SL151, SL152, SL153, SL154, SL155, SL156, SL157, SL158, SL159, SL160, SL161, SL162, SL164, SL166, SL167, SL168, SL169, SL171, SL173, SL174, SL175, SL176, SL180, SL181, SL182, SL183, SL184, SL185, SL186, SL187, SL188, SL190, SL191, SL192, SL193, SL194, SL195,SL196,SL197,SL198,SL199 |
23452 | Jan-88 | ||||||||
| SL206, SL207, SL208, SL209, SL210, SL212, SL213, SL214, SL215, SL216, SL217, SL218, SL219, SL220, SL221, SL222, SL223, SL224, SL227, SL228, SL229, SL230, SL231, SL232, SL233, SL234, SL235, SL236, SL237, SL238, SL239, SL240, SL241, SL242, SL247, SL248, SL249, SL250, SL251, SL252, SL253, SL254, SL256, SL257, SL258,SL259,SL261,SL262,SL263,SL265,SL266,SL267,SL268,SL270,SL271, |
27853 | Feb-89 |
Market Announcement | Page 33 of 50
| Criteria | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | Explanation | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| SL272, SL273, SL274, SL275, SL276, SL278, SL279, SL281, SL282, SL283, SL284, SL285, SL286, SL287, SL288, SL289, SL291, SL292, SL297, SL298, SL299, SL301, SL302, SL314, SL315, SL316, SL317, SL319, SL320, SL324, SL325, SL326, SL327, SL328, SL329, SL332, SL334, SL358, SL359, SL360, SL368, SL369, SL371, SL372, SL374, SL375, SL383, SL386, SL388, SL389, SL390, SL391, SL393, SL394, SL395, SL396, SL397, SL398, SL399, SL400, SL401, SL402, SL403, SL405, SL406, SL407, SL408, SL409, SL410, SL411, SL419, SL420, SL421, SL422, SL423, SL424, SLD11, SLD12, SLD13, SLD14, SLD16, SLD17, SLD19, SLD21, SLD22, SLD23, SLD24, SLD25,SLD27 |
|||||||||||
| Ashton | SL547,SL548,SL549,SL550 | 35678 | Jan-92 | ||||||||
| Sons of Gwalia |
ENC316,ENC317,ENC318,ENC319,ENC320,ENC321,ENC323 | 59191 | Nov-99 | ||||||||
| Apollo | WV001, WV002, WV004, WV008, WV009, WV012, WV013, WV014, WV015, WV016,WV028 |
68420 | Apr-04 | ||||||||
| Crescent | CMRC001,CMRC002A,CMRC004,CMRC005,CMRC006,CMRC007 | 74767 | Mar-07 | ||||||||
| CMD001, CMRC008, CMRC009, CMRC010, CMRC011, CMRC012, CMRC013, CMRC014, CMRC015, CMRC016, CMRC017, CMRC018, CMRC019, CMRC020, CMRC021, CMRC022, CMRC023, CMRC024, CMRC025, CMRC026, CMRC027, CMRC028, CMRC029, CMRC030, CMRC031, CMRC032, CMRC033, CMRC034, CMRC035, CMRC036, CMRC037, CMRC038, CMRC039, CMRC040, CMRC041, CMRC046, CMRC047, CMRC049, CMRC050, CMRC051, CMRC052, CMRC053, CMRC054, CMRC055, CMRC056, CMRC057, CMRC058, CMRC059, CMRC060, CMRC061, CMRC062, CMRC063, CMRC064, CMRC065, CMRC067, CMRC068, CMRC069, CMRC070, CMRC071, CMRC072, CMRC073, CMRC076, CMRC077, CMRC078,CMRC079 |
77949 | Apr-08 | |||||||||
| CMRC082,CMRC083,CMRC084,CMRC085,CRNRC001 | 81229 | Feb-09 | |||||||||
| CMRC201, CMRC202, CMRC203, CMRC204, CMRC205, CMRC206, CMRC207, CMRC208, CMRC209, CMRC210, CMRC211, CMRC212, CMRC213, CMRC214, CMRC215, CMRC216, CMRC217, CMRC219, CMRC221, CMRC222, CMRC223, CMRC224,CMRC225,CMRC226,CMRC227,CMRC228 |
86387 | Feb-10 | |||||||||
| CMRC229, CMRC230, CMRC231, CMRC232, CMRC233, CMRC234, CMRC235, CMRC236, CMRC237, CMRC238, CMRC239, CMRC240, CMRC241, CMRC242, CMRC243, CMRC245, CMRC246, CMRC247, CMRC248, CMRC249, CMRC251, CMRC252, CMRC253, CMRC255, CMRC256, CMRC257, CMRC258, CMRC259, CMRC260, CMRC261, CMRC262, CMRC263, CMRC264, CMRC265, CMRC266, CMRC267, CMRC268, CMRC269, CMRC270, CMRC271, CMRC272, CMRC273, CMRC274, CMRC276, CMRC277, CMRC278, CMRC279, CMRC280, CMRC281, CMRC282, CMRC284, CMRC285, CMRC286, CMRC287, CMRC295, CMRC296, CMRC297, CMRC298, CMRC299, CMRC300, CMRC303, CMRC304, CMRC310, CMRC311, CMRC312, CMRC313, CMRC314, CMRC315, CMRC316, CMRC317, CMRC318, CMRC319, CMRC320, CMRC321, CMRC322, CMRC323, CMRC325, CMRC326,CMRC328,CRADD001 |
90143 | Apr-11 | |||||||||
| CMRC329, CMRC330, CMRC332, CMRC333, CMRC334, CMRC335, CMRC336, CMRC337,CMRC338 |
93988 | Jun-12 | |||||||||
| CM/MM FML holes ASX announcements: | |||||||||||
| Drill Hole Number | ASX Release Title | ASX Release Date | |||||||||
| Focus Confirms Strong Results from Coolgardie and Laverton Exploration Campaigns |
30-July-14 | ||||||||||
| CMDD348, CMRC341, CMRC342 | |||||||||||
| CM/MM historic Collar details of holes not previously externally reported: | |||||||||||
| Hole ID | MGA 94 Zone 51 | Depth (m) |
Company | ||||||||
| Easting | Northing | RL | Azimuth | Dip | |||||||
| SL10 | 440357.68 | 6829668.2 | 478.33 | 277 | -60 | 93 | Hillmin | ||||
| SL14 | 440317.25 | 6829956.1 | 474.58 | 106 | -56 | 50 | Hillmin |
| Criteria | Explanation | Explanation | Explanation | ||||||
|---|---|---|---|---|---|---|---|---|---|
| SL5 | 440404.13 | 6829942.9 | 478.08 | 287 | -60 | 63 | Hillmin | ||
| SL6 | 440371.95 | 6829937.7 | 477.86 | 280 | -60 | 69 | Hillmin | ||
| SL7 | 440365.44 | 6829870.9 | 477.98 | 288 | -60 | 33 | Hillmin | ||
| SL8 | 440351.28 | 6829874.9 | 477.6 | 288 | -60 | 63 | Hillmin | ||
| CM002 | 440311.56 | 6829547.3 | 471.33 | 256.7 | -60 | 42 | SOG | ||
| CM003 | 440307.18 | 6829566.8 | 472.4 | 256.7 | -60 | 30 | SOG | ||
| CM004 | 440311.3 | 6829582.9 | 469.62 | 256.7 | -60 | 40 | SOG | ||
| CM005 | 440308.45 | 6829590.4 | 469.52 | 256.7 | -60 | 50 | SOG | ||
| CM007 | 440318.17 | 6829613.8 | 467.79 | 256.7 | -60 | 42 | SOG | ||
| CM008 | 440322.5 | 6829625.4 | 467 | 256.7 | -60 | 54 | SOG | ||
| CM010 | 440407.48 | 6829541.8 | 469.99 | 285.7 | -60 | 50 | SOG | ||
| CM012 | 440329.14 | 6829616.2 | 467 | 256.7 | -60 | 60 | SOG | ||
| CM013 | 440334.25 | 6829627.5 | 467 | 256.7 | -60 | 60 | SOG | ||
| CM015 | 440404.77 | 6829532.4 | 469.66 | 285.7 | -60 | 46 | SOG | ||
| CM016 | 440401.59 | 6829515.9 | 468.58 | 285.7 | -60 | 46 | SOG | ||
| CM017 | 440309.71 | 6829612.3 | 468.24 | 256.7 | -60 | 54 | SOG | ||
| CM018 | 440310.7 | 6829623 | 467 | 256.7 | -60 | 54 | SOG | ||
| CM019 | 440390.54 | 6829504.2 | 468.79 | 285.7 | -60 | 50 | SOG | ||
| CM020 | 440321.34 | 6829583.7 | 469 | 256.7 | -60 | 60 | SOG | ||
| CM021 | 440306.41 | 6829583.4 | 470.21 | 256.7 | -60 | 36 | SOG | ||
| CM022 | 440318.56 | 6829593.3 | 469.19 | 261.7 | -60 | 54 | SOG | ||
| CM023 | 440301.3 | 6829589.1 | 470.27 | 256.7 | -60 | 30 | SOG | ||
| CM024 | 440308.1 | 6829566.4 | 472.27 | 286.7 | -60 | 60 | SOG | ||
| CM025 | 440307.14 | 6829548.1 | 471.59 | 256.7 | -60 | 34 | SOG | ||
| CM026 | 440319.25 | 6829546.6 | 471 | 256.7 | -60 | 72 | SOG | ||
| CM027 | 440312.91 | 6829597.5 | 469.64 | 286.7 | -60 | 39 | SOG | ||
| CM028 | 440324 | 6829593.8 | 468.52 | 291.7 | -60 | 72 | SOG | ||
| CM029 | 440322.1 | 6829627.9 | 467 | 286.7 | -60 | 40 | SOG | ||
| CM030 | 440311.34 | 6829626.7 | 467 | 286.7 | -60 | 75 | SOG | ||
| CM032 | 440309.49 | 6829547.7 | 471.48 | 256.7 | -60 | 39 | SOG | ||
| Hole ID | MGA 94 Zone 51 | Depth (m) | |||||||
| Easting | Northing | RL | Azimuth | Dip | |||||
| CR410002 | 440344.34 | 6829679.5 | 409.42 | 285 | 60 | 36 | |||
| CR410003 | 440348.93 | 6829678.6 | 409.51 | 285 | 60 | 36 | |||
| CR410004 | 440342.37 | 6829690.1 | 409.44 | 285 | 60 | 36 | |||
| CR410006 | 440356.26 | 6829696.9 | 409.29 | 285 | 60 | 42 | |||
| CR410008 | 440339.92 | 6829711.6 | 408.84 | 285 | 50 | 36 | |||
| CR410009 | 440356.08 | 6829706.2 | 409.39 | 285 | 60 | 42 | |||
| CR410011 | 440345.71 | 6829720.1 | 409.16 | 285 | 50 | 40 | |||
| CR410012 | 440354.46 | 6829717.3 | 409.16 | 285 | 60 | 42 | |||
| CR410014 | 440347.43 | 6829730.1 | 409.62 | 285 | 60 | 42 | |||
| CR410021 | 440344.45 | 6829749.3 | 409.46 | 285 | 65 | 40 | |||
| CR410023 | 440312.52 | 6829771.5 | 409.59 | 285 | 60 | 28 | |||
| CR410026 | 440314.5 | 6829767.8 | 409.34 | 105 | 60 | 36 | |||
| CR410029 | 440313.16 | 6829781.9 | 409.64 | 105 | 65 | 36 | |||
| CR410032 | 440317.92 | 6829791 | 409.65 | 105 | 80 | 33 | |||
| CR410035 | 440355.27 | 6829780 | 409.54 | 285 | 60 | 24 | |||
| CR410040 | 440354.46 | 6829790.6 | 409.66 | 285 | 60 | 36 | |||
| CR410042 | 440317.57 | 6829810.8 | 410.01 | 285 | 85 | 33 | |||
| CR410045 | 440350.97 | 6829802.1 | 409.69 | 105 | 55 | 36 | |||
| CR410048 | 440318.87 | 6829822.1 | 410.21 | 105 | 85 | 33 |
Market Announcement | Page 35 of 50
| Criteria | Explanation | Explanation | Explanation | Explanation | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| CR410055 | 440321.73 | 6829841.9 | 410 | 0 | 90 | 33 | ||||||
| CR410056 | 440324.37 | 6829841.4 | 409.98 | 0 | 50 | 24 | ||||||
| CR410057 | 440350.41 | 6829834 | 409.95 | 285 | 60 | 24 | ||||||
| CR420005 | 440302.55 | 6829660.2 | 420 | 105 | 60 | 24 | ||||||
| CR420016 | 440293.05 | 6829600.5 | 420 | 105 | 60 | 12 | ||||||
| CR420017 | 440300.76 | 6829598.4 | 420 | 105 | 60 | 12 | ||||||
| CR425005 | 440361.47 | 6829685.1 | 424.7 | 285 | 55 | 54 | ||||||
| CR425006 | 440360.21 | 6829695.7 | 424.96 | 285 | 60 | 54 | ||||||
| CR425008 | 440306.18 | 6829711.2 | 425.06 | 105 | 60 | 54 | ||||||
| CR425010 | 440361.07 | 6829706 | 424.95 | 285 | 60 | 54 | ||||||
| CR425012 | 440307.06 | 6829721.4 | 425.01 | 105 | 60 | 54 | ||||||
| CR425013 | 440304.97 | 6829732.4 | 424.87 | 105 | 60 | 54 | ||||||
| CR425017 | 440307.57 | 6829741.8 | 424.95 | 105 | 60 | 54 | ||||||
| CR425018 | 440305.71 | 6829752.7 | 424.95 | 105 | 55 | 54 | ||||||
| CR425027 | 440375.36 | 6829764.2 | 424.94 | 285 | 60 | 54 | ||||||
| CR425028 | 440378.94 | 6829773.6 | 424.97 | 285 | 60 | 24 | ||||||
| CR425031 | 440380.01 | 6829783.9 | 424.82 | 285 | 60 | 54 | ||||||
| CR425033 | 440377.76 | 6829794.8 | 424.95 | 285 | 60 | 24 | ||||||
| CR425035 | 440381.39 | 6829804.3 | 424.76 | 285 | 60 | 24 | ||||||
| CR425036 | 440376.16 | 6829815.9 | 425 | 285 | 50 | 55 | ||||||
| CR425037 | 440374.52 | 6829827.1 | 425.19 | 285 | 60 | 24 | ||||||
| CR425038 | 440374.42 | 6829837.5 | 425.07 | 285 | 60 | 24 | ||||||
| CR425045 | 440366.74 | 6829870.6 | 425.1 | 285 | 60 | 24 | ||||||
| CR425048 | 440333.05 | 6829900.9 | 425.17 | 285 | 60 | 24 | ||||||
| CR425051 | 440328.76 | 6829901.9 | 425.15 | 285 | 60 | 24 | ||||||
| CR470001 | 440378.67 | 6829463.4 | 469.7 | 285 | 60 | 15 | ||||||
| CR470002 | 440383.34 | 6829461.2 | 469 | 285 | 60 | 25 | ||||||
| CR470004 | 440380.57 | 6829472.1 | 469.29 | 285 | 60 | 20 | ||||||
| CR470005 | 440384.8 | 6829470.8 | 468.61 | 285 | 60 | 30 | ||||||
| CR470006 | 440385.61 | 6829481 | 468.6 | 285 | 60 | 22 | ||||||
| CR470009 | 440402.57 | 6829486.6 | 467.87 | 285 | 60 | 40 | ||||||
| CR470012 | 440401.85 | 6829497.4 | 468.25 | 285 | 60 | 40 | ||||||
| CR470026 | 440318.92 | 6829551.9 | 471.04 | 285 | 60 | 54 | ||||||
| CR470090 | 440390.43 | 6829947.5 | 473.05 | 285 | 60 | 38 | ||||||
| CR470093 | 440375.86 | 6829940.1 | 465.83 | 285 | 60 | 15 | ||||||
| CR470094 | 440382.08 | 6829928.6 | 465.65 | 285 | 60 | 34 | ||||||
| CR470104 | 440427.7 | 6829812.1 | 466.79 | 285 | 60 | 46 | ||||||
| CR470106 | 440419.59 | 6829803.8 | 467.17 | 285 | 60 | 39 | ||||||
| CR470110 | 440420.32 | 6829782.8 | 467.19 | 285 | 60 | 48 | ||||||
| CR470113 | 440423.46 | 6829771.7 | 467.43 | 285 | 60 | 48 | ||||||
| CR470116 | 440423.83 | 6829761.2 | 467.63 | 285 | 60 | 47 | ||||||
| CR470121 | 440426.9 | 6829749.8 | 467.86 | 285 | 60 | 47 | ||||||
| Mary Mac: | ||||||||||||
| Hole ID | MGA 94 Zone 51 | Depth (m) | ||||||||||
| Easting | Northing | RL | Azimuth | Dip | ||||||||
| MMHFPR14 | 440753.26 | 6831356.5 | 494.86 | 285 | 87 | 65 | ||||||
| MMHFPR19 | 440767.15 | 6831353.6 | 494.27 | 285 | 50 | 54 | ||||||
| MMHGC0028 | 440648.2 | 6831204.3 | 487.32 | 286 | 60 | 54 | ||||||
| MMHGC0122 | 440769.7 | 6831377.9 | 497.31 | 286 | 60 | 50 | ||||||
| MMHGC0123 | 440774.52 | 6831376.5 | 495.56 | 286 | 60 | 40 | ||||||
| MMHGC0124 | 440779.33 | 6831375.1 | 495 | 286 | 60 | 40 | ||||||
| MMHGC0129 | 440766.4 | 6831347.6 | 492.98 | 286 | 60 | 40 | ||||||
| MMHGC0130 | 440771.21 | 6831346.3 | 492 | 286 | 60 | 40 | ||||||
| MMHGC0131 | 440776.03 | 6831344.9 | 491.5 | 286 | 60 | 40 | ||||||
| MMHGC0134 | 440764.29 | 6831358.6 | 495.05 | 286 | 60 | 40 | ||||||
| MMHGC0135 | 440759.48 | 6831359.9 | 496.12 | 286 | 60 | 41 | ||||||
| MMHGC0140 | 440758.88 | 6831339.3 | 493.1 | 286 | 60 | 50 | ||||||
| MMHGC0157 | 440744.9 | 6831405.3 | 507.44 | 234 | 60 | 35 | ||||||
| MMHGC0159 | 440742.71 | 6831400.7 | 507.28 | 236 | 60 | 35 | ||||||
| MMHGC0218 | 440745.08 | 6831384.8 | 497.78 | 287 | 60 | 18 | ||||||
| MMHGC0219 | 440745.08 | 6831384.8 | 497.78 | 0 | 90 | 18 | ||||||
| MMHGC0221 | 440773.52 | 6831384.2 | 495 | 0 | 90 | 30 | ||||||
| MMHGC0222 | 440773.52 | 6831384.2 | 495 | 105 | 63 | 30 | ||||||
| MMHGC0224 | 440730.13 | 6831368.3 | 500 | 0 | 90 | 48 |
| Criteria | Explanation | Explanation | Explanation | |||||
|---|---|---|---|---|---|---|---|---|
| MMHGC0225 | 440728.13 | 6831358.5 | 500.16 | 285 | 60 | 54 | ||
| MMHGC0228 | 440715.86 | 6831351.6 | 500 | 285 | 70 | 48 | ||
| MMHGC0259 | 440713.19 | 6831248.7 | 487.72 | 285 | 60 | 42 | ||
| MMHGC0260 | 440721.12 | 6831246.3 | 486.49 | 285 | 60 | 36 | ||
| MMHGC0283 | 440647.18 | 6831187.8 | 470.02 | 285 | 60 | 30 | ||
| MMHGC0284 | 440639.6 | 6831179.6 | 475 | 285 | 80 | 36 | ||
| MMHGC45001 | 440726.03 | 6831318.3 | 449.79 | 285 | 60 | 30 | ||
| MMHGC45002 | 440696.84 | 6831326.3 | 450.09 | 285 | 60 | 12 | ||
| MMHGC45005 | 440699.18 | 6831303.1 | 450.13 | 285 | 60 | 24 | ||
| MMHGC45008 | 440676.35 | 6831310.9 | 450.54 | 285 | 60 | 12 | ||
| MMHGC45010 | 440698.27 | 6831284.4 | 450.29 | 285 | 60 | 30 | ||
| MMHGC45011 | 440690.63 | 6831285.8 | 450.31 | 285 | 60 | 24 | ||
| MMHGC45012 | 440676.09 | 6831287.2 | 450.03 | 285 | 60 | 18 | ||
| MMHGC45015 | 440689.93 | 6831276.3 | 450 | 285 | 60 | 30 | ||
| MMHGC45016 | 440683.17 | 6831278.1 | 450 | 285 | 60 | 24 | ||
| MMHGC45017 | 440675.36 | 6831281.1 | 450.03 | 285 | 60 | 18 | ||
| MMHGC45019 | 440658.17 | 6831284.9 | 450 | 285 | 60 | 18 | ||
| MMHGC45020 | 440678.73 | 6831269.3 | 450.12 | 285 | 60 | 30 | ||
| MMHGC45021 | 440673.73 | 6831270.2 | 450.13 | 285 | 60 | 24 | ||
| MMHGC45022 | 440666.88 | 6831272.1 | 450.02 | 285 | 60 | 24 | ||
| MMHGC45023 | 440660.55 | 6831273.9 | 449.96 | 285 | 60 | 24 | ||
| MMHGC45024 | 440653.36 | 6831275.8 | 450.05 | 285 | 60 | 24 | ||
| MMHGC45025 | 440646.68 | 6831277.5 | 449.92 | 285 | 60 | 24 | ||
| MMHGC45032 | 440650.41 | 6831255.5 | 450.06 | 285 | 60 | 26 | ||
| MMHGC45035 | 440628.05 | 6831261.4 | 449.96 | 285 | 60 | 15 | ||
| MMHGC45037 | 440639.23 | 6831248.6 | 449.84 | 285 | 60 | 24 | ||
| MMHGC45038 | 440632.02 | 6831249.1 | 449.86 | 285 | 60 | 24 | ||
| MMHGC45040 | 440650.69 | 6831235.2 | 450.01 | 285 | 60 | 30 | ||
| MMHGC45041 | 440640.01 | 6831238 | 449.86 | 285 | 60 | 24 | ||
| MMHGC45042 | 440629.41 | 6831240.7 | 449.81 | 285 | 60 | 24 | ||
| MMHGC45044 | 440636.33 | 6831228.7 | 449.95 | 285 | 60 | 24 | ||
| MMHGC45046 | 440649.33 | 6831214.2 | 450.28 | 0 | 90 | 15 | ||
| MMHGC45047 | 440641.74 | 6831216.4 | 450.12 | 285 | 60 | 18 | ||
| MMHGC45048 | 440635 | 6831218.5 | 450.02 | 285 | 60 | 18 | ||
| MMHGC45051 | 440633.85 | 6831213.6 | 449.89 | 285 | 80 | 30 | ||
| MMHGC45054 | 440618.44 | 6831208.5 | 450.13 | 285 | 80 | 30 | ||
| MMHGC45056 | 440622 | 6831191 | 452.52 | 285 | 60 | 30 | ||
| MMHGC45058 | 440618.22 | 6831182.7 | 452.66 | 285 | 60 | 30 | ||
| MMHGC45059 | 440602.46 | 6831186.5 | 452.52 | 285 | 60 | 30 | ||
| MMHGC45060 | 440612.99 | 6831174 | 452.52 | 285 | 80 | 30 | ||
| MMHGC465009 | 440650.69 | 6831222 | 464.64 | 285 | 60 | 45 | ||
| MMHGC465013 | 440632.36 | 6831228.8 | 465 | 285 | 60 | 36 | ||
| MMHGC465014 | 440657.86 | 6831221.4 | 464.59 | 285 | 60 | 53 | ||
| MMHGC465016 | 440647.93 | 6831235.3 | 464.8 | 285 | 60 | 46 | ||
| MMHGC465026 | 440621.33 | 6831263.5 | 464.68 | 0 | 90 | 30 | ||
| MMHGC465057 | 440681.11 | 6831329.8 | 464.95 | 105 | 85 | 24 | ||
| MMHGC470005 | 440741.69 | 6831333.5 | 469.63 | 285 | 70 | 30 | ||
| MMHGC470008 | 440738.19 | 6831324.4 | 469.46 | 285 | 60 | 36 | ||
| MMHGC470009 | 440730.55 | 6831326.4 | 469.65 | 285 | 60 | 36 | ||
| MMHGC470010 | 440722.93 | 6831328.6 | 470.1 | 285 | 60 | 36 | ||
| MMHGC470015 | 440736.19 | 6831304 | 469.61 | 285 | 60 | 36 | ||
| MMHGC470017 | 440728.89 | 6831295.8 | 469.64 | 285 | 60 | 45 | ||
| MMHGC470018a | 440712.1 | 6831300 | 469.78 | 285 | 60 | 48 | ||
| MMHGC470022 | 440720.1 | 6831277.9 | 469.88 | 285 | 60 | 36 | ||
| MMHGC470034 | 440706.95 | 6831260.5 | 469.93 | 285 | 60 | 36 | ||
| MMHGC470039 | 440687.67 | 6831245.1 | 469.95 | 285 | 60 | 24 | ||
| MMHSPR02 | 440632.01 | 6831195.8 | 469.92 | 285 | 50 | 36 | ||
| MMHSPR08 | 440624 | 6831176 | 470 | 285 | 50 | 30 | ||
| MMHSPR09 | 440594 | 6831175 | 470 | 105 | 70 | 36 | ||
| MMSGC001 | 440474.35 | 6830411.8 | 466.39 | 286 | 60 | 45 | ||
| MMSGC002 | 440467.53 | 6830413.6 | 466.42 | 286 | 60 | 45 | ||
| MMSGC003 | 440460.82 | 6830415.5 | 466.62 | 286 | 60 | 20 | ||
| MMSGC004 | 440454.04 | 6830417.4 | 466.81 | 286 | 60 | 10 | ||
| MMSGC005 | 440477.08 | 6830421.4 | 466.13 | 286 | 60 | 45 | ||
| MMSGC006 | 440470.29 | 6830423.3 | 466.08 | 286 | 60 | 45 | ||
| MMSGC007 | 440456.83 | 6830427 | 466.27 | 286 | 60 | 20 |
Market Announcement | Page 37 of 50
| Criteria | Explanation | Explanation | Explanation | |||||
|---|---|---|---|---|---|---|---|---|
| MMSGC009 | 440479.66 | 6830430.9 | 465.65 | 286 | 60 | 45 | ||
| MMSGC010 | 440473.04 | 6830432.9 | 465.85 | 286 | 60 | 45 | ||
| MMSGC011 | 440466.24 | 6830434.8 | 465.79 | 286 | 60 | 30 | ||
| MMSGC012 | 440459.49 | 6830436.6 | 465.74 | 286 | 60 | 20 | ||
| MMSGC014 | 440489.15 | 6830438.6 | 466.23 | 286 | 60 | 45 | ||
| MMSGC015 | 440482.42 | 6830440.5 | 466.42 | 286 | 60 | 45 | ||
| MMSGC016 | 440475.35 | 6830442.5 | 466.08 | 286 | 60 | 45 | ||
| MMSGC017 | 440468.51 | 6830444.9 | 466.03 | 286 | 60 | 20 | ||
| MMSGC019 | 440455.46 | 6830448.2 | 465.69 | 286 | 60 | 10 | ||
| MMSGC020 | 440485.13 | 6830450.3 | 466.27 | 286 | 60 | 45 | ||
| MMSGC021 | 440478.44 | 6830451.3 | 469.08 | 286 | 60 | 49 | ||
| MMSGC022 | 440471.38 | 6830454.1 | 469.37 | 286 | 60 | 24 | ||
| MMSGC023 | 440465.07 | 6830455.9 | 469.19 | 286 | 60 | 14 | ||
| MMSGC024 | 440457.41 | 6830457.8 | 465.9 | 286 | 60 | 10 | ||
| MMSGC025 | 440487.95 | 6830459.9 | 466.2 | 286 | 60 | 45 | ||
| MMSGC026 | 440481.26 | 6830461.6 | 466.06 | 286 | 60 | 45 | ||
| MMSGC027 | 440474.16 | 6830463.7 | 466.12 | 286 | 60 | 45 | ||
| MMSGC028 | 440467.58 | 6830465.5 | 466.04 | 286 | 60 | 20 | ||
| MMSGC029 | 440460.78 | 6830467.1 | 465.9 | 286 | 60 | 10 | ||
| MMSGC030 | 440490.51 | 6830469.5 | 466.41 | 286 | 60 | 45 | ||
| MMSGC031 | 440470.35 | 6830475.2 | 466.3 | 286 | 60 | 45 | ||
| MMSGC032 | 440463.54 | 6830477.1 | 466.2 | 286 | 60 | 45 | ||
| MMSGC033 | 440450.15 | 6830480.8 | 466.12 | 286 | 60 | 20 | ||
| MMSGC034 | 440443.39 | 6830482.8 | 466.02 | 286 | 60 | 10 | ||
| MMSGC035 | 440486.52 | 6830481 | 466.56 | 286 | 60 | 45 | ||
| MMSGC036 | 440479.7 | 6830482.9 | 466.54 | 286 | 60 | 45 | ||
| MMSGC037 | 440473.01 | 6830484.8 | 466.5 | 286 | 60 | 45 | ||
| MMSGC038 | 440466.26 | 6830486.8 | 466.38 | 286 | 60 | 45 | ||
| MMSGC039 | 440459.51 | 6830488.6 | 466.36 | 286 | 60 | 45 | ||
| MMSGC040 | 440452.86 | 6830490.5 | 466.39 | 286 | 60 | 20 | ||
| MMSGC041 | 440446.13 | 6830492.4 | 466.35 | 286 | 60 | 10 | ||
| MMSGC042 | 440489.16 | 6830490.6 | 466.85 | 286 | 60 | 45 | ||
| MMSGC043 | 440475.71 | 6830494.4 | 466.61 | 286 | 60 | 45 | ||
| MMSGC044 | 440469 | 6830496.3 | 466.63 | 286 | 60 | 45 | ||
| MMSGC045 | 440455.55 | 6830500 | 466.64 | 286 | 60 | 20 | ||
| MMSGC046 | 440448.79 | 6830502 | 466.57 | 286 | 60 | 10 | ||
| MMSGC047 | 440491.93 | 6830500.3 | 467.13 | 286 | 60 | 45 | ||
| MMSGC048 | 440485.16 | 6830502.2 | 466.93 | 286 | 60 | 45 | ||
| MMSGC049 | 440478.46 | 6830504.1 | 466.88 | 286 | 60 | 45 | ||
| MMSGC050 | 440471.67 | 6830506 | 466.89 | 286 | 60 | 45 | ||
| MMSGC0500 | 440540.91 | 6830855.5 | 475.7 | 285 | 60 | 24 | ||
| MMSGC0501 | 440548.13 | 6830854.3 | 475.06 | 285 | 60 | 24 | ||
| MMSGC0502 | 440554.24 | 6830851.6 | 474.79 | 285 | 60 | 24 | ||
| MMSGC051 | 440464.92 | 6830507.9 | 466.81 | 286 | 60 | 45 | ||
| MMSGC0512 | 440585.12 | 6830962.3 | 474.85 | 285 | 60 | 24 | ||
| MMSGC0514 | 440570.11 | 6830997.7 | 475.45 | 285 | 60 | 24 | ||
| MMSGC0515 | 440577.31 | 6830995.8 | 475.51 | 285 | 60 | 24 | ||
| MMSGC0516 | 440585.47 | 6830993.5 | 475.5 | 285 | 60 | 24 | ||
| MMSGC0517 | 440593.14 | 6830991.3 | 475.37 | 285 | 60 | 24 | ||
| MMSGC0518 | 440600.94 | 6830989.2 | 475.34 | 285 | 60 | 24 | ||
| MMSGC0519 | 440572.82 | 6831007.6 | 475.78 | 285 | 60 | 24 | ||
| MMSGC052 | 440458.31 | 6830509.8 | 466.75 | 286 | 60 | 20 | ||
| MMSGC0520 | 440580.42 | 6831005.1 | 475.7 | 285 | 60 | 24 | ||
| MMSGC0521 | 440588.24 | 6831003 | 475.7 | 285 | 60 | 24 | ||
| MMSGC0522 | 440595.97 | 6831000.9 | 475.52 | 285 | 60 | 24 | ||
| MMSGC0523 | 440603.6 | 6830998.8 | 475.49 | 285 | 60 | 24 | ||
| MMSGC0524 | 440583.12 | 6831014.8 | 475.91 | 285 | 60 | 24 | ||
| MMSGC0525 | 440585.78 | 6831024.5 | 476.16 | 285 | 60 | 24 | ||
| MMSGC0526 | 440593.66 | 6831022.2 | 476.17 | 285 | 60 | 24 | ||
| MMSGC0527 | 440601.27 | 6831020.1 | 476.15 | 285 | 60 | 24 | ||
| MMSGC0528 | 440608.78 | 6831017.8 | 476.01 | 285 | 60 | 24 | ||
| MMSGC0529 | 440616.64 | 6831015.7 | 475.83 | 285 | 60 | 24 | ||
| MMSGC053 | 440451.49 | 6830511.6 | 466.68 | 286 | 60 | 10 | ||
| MMSGC0530 | 440588.69 | 6831034.1 | 476.41 | 285 | 60 | 24 | ||
| MMSGC0531 | 440602.02 | 6831030.5 | 476.33 | 285 | 60 | 24 | ||
| MMSGC0532 | 440595.9 | 6831052.8 | 477.1 | 286 | 60 | 24 |
| Criteria | Explanation | Explanation | Explanation | |||||
|---|---|---|---|---|---|---|---|---|
| MMSGC0533 | 440603.41 | 6831050.7 | 477.06 | 286 | 60 | 24 | ||
| MMSGC0534 | 440611.22 | 6831048.5 | 476.97 | 286 | 60 | 24 | ||
| MMSGC0535 | 440619.06 | 6831046.3 | 476.94 | 286 | 60 | 24 | ||
| MMSGC054 | 440494.64 | 6830510 | 467.33 | 286 | 60 | 45 | ||
| MMSGC055 | 440481.11 | 6830513.7 | 467.28 | 286 | 60 | 45 | ||
| MMSGC056 | 440474.47 | 6830515.5 | 467.18 | 286 | 60 | 45 | ||
| MMSGC057 | 440461.01 | 6830519.4 | 467.14 | 286 | 60 | 30 | ||
| MMSGC058 | 440454.16 | 6830521.2 | 467.01 | 286 | 60 | 10 | ||
| MMSGC059 | 440497.4 | 6830519.5 | 467.9 | 286 | 60 | 30 | ||
| MMSGC060 | 440490.65 | 6830521.4 | 467.72 | 286 | 60 | 45 | ||
| MMSGC061 | 440483.84 | 6830523.4 | 467.69 | 286 | 60 | 45 | ||
| MMSGC062 | 440477.08 | 6830525.2 | 467.6 | 286 | 60 | 45 | ||
| MMSGC063 | 440470.37 | 6830527.1 | 467.76 | 286 | 60 | 45 | ||
| MMSGC064 | 440463.63 | 6830529 | 467.64 | 286 | 60 | 45 | ||
| MMSGC065 | 440456.89 | 6830530.9 | 467.57 | 286 | 60 | 20 | ||
| MMSGC066 | 440450.15 | 6830532.8 | 467.41 | 286 | 60 | 10 | ||
| MMSGC067 | 440493.25 | 6830531.1 | 468.23 | 286 | 60 | 45 | ||
| MMSGC068 | 440486.49 | 6830533 | 468.2 | 286 | 60 | 45 | ||
| MMSGC069 | 440479.79 | 6830534.9 | 468.15 | 286 | 60 | 45 | ||
| MMSGC070 | 440473.05 | 6830536.8 | 468.05 | 286 | 60 | 45 | ||
| MMSGC071 | 440466.31 | 6830538.6 | 468.08 | 286 | 60 | 45 | ||
| MMSGC072 | 440459.68 | 6830540.5 | 468.05 | 286 | 60 | 45 | ||
| MMSGC073 | 440452.77 | 6830542.5 | 467.96 | 286 | 60 | 20 | ||
| MMSGC074 | 440446.1 | 6830544.3 | 467.79 | 286 | 60 | 10 | ||
| MMSGC075 | 440482.44 | 6830544.6 | 468.64 | 286 | 60 | 45 | ||
| MMSGC076 | 440475.73 | 6830546.3 | 468.71 | 286 | 60 | 35 | ||
| MMSGC077 | 440462.24 | 6830550.1 | 468.65 | 286 | 60 | 45 | ||
| MMSGC078 | 440455.6 | 6830552.1 | 468.68 | 286 | 60 | 20 | ||
| MMSGC079 | 440498.68 | 6830550.3 | 469.07 | 286 | 60 | 45 | ||
| MMSGC080 | 440492.04 | 6830552.2 | 469.17 | 286 | 60 | 45 | ||
| MMSGC081 | 440485.26 | 6830554.1 | 469.18 | 286 | 60 | 25 | ||
| MMSGC084 | 440465.06 | 6830559.8 | 469.24 | 286 | 60 | 25 | ||
| MMSGC085 | 440458.27 | 6830561.7 | 469.17 | 286 | 60 | 25 | ||
| MMSGC091 | 440474.42 | 6830567.5 | 469.76 | 286 | 60 | 45 | ||
| MMSGC092 | 440460.98 | 6830571.3 | 469.71 | 286 | 60 | 45 | ||
| MMSGC094 | 440544.55 | 6830558.2 | 468.63 | 286 | 60 | 45 | ||
| MMSGC098 | 440490.63 | 6830573.3 | 470.17 | 286 | 60 | 45 | ||
| MMSGC099 | 440483.92 | 6830575.2 | 470.21 | 286 | 60 | 45 | ||
| MMSGC100 | 440477.16 | 6830577.2 | 470.27 | 286 | 60 | 45 | ||
| MMSGC101 | 440470.38 | 6830579 | 470.14 | 286 | 60 | 45 | ||
| MMSGC105 | 440547.25 | 6830567.8 | 468.37 | 286 | 60 | 45 | ||
| MMSGC106 | 440540.51 | 6830569.7 | 468.81 | 286 | 60 | 45 | ||
| MMSGC129 | 440552.66 | 6830587.1 | 468.8 | 286 | 60 | 45 | ||
| MMSGC331 | 440558.29 | 6830865.9 | 474.58 | 286 | 60 | 25 | ||
| MMSGC332 | 440551.53 | 6830867.8 | 474.97 | 286 | 60 | 25 | ||
| MMSGC333 | 440544.76 | 6830869.6 | 475.26 | 286 | 60 | 20 | ||
| MMSGC334 | 440538.09 | 6830871.7 | 475.76 | 286 | 60 | 10 | ||
| MMSGC335 | 440561.02 | 6830875.5 | 474.78 | 286 | 60 | 25 | ||
| MMSGC336 | 440554.32 | 6830877.5 | 474.96 | 286 | 60 | 25 | ||
| MMSGC337 | 440547.46 | 6830879.4 | 475.32 | 286 | 60 | 20 | ||
| MMSGC338 | 440540.81 | 6830881.2 | 477.08 | 286 | 60 | 25 | ||
| MMSGC340 | 440557 | 6830887.1 | 474.94 | 286 | 60 | 25 | ||
| MMSGC341 | 440543.52 | 6830890.9 | 475.67 | 286 | 60 | 25 | ||
| MMSGC342 | 440536.81 | 6830892.9 | 476.19 | 286 | 60 | 20 | ||
| MMSGC343 | 440530.09 | 6830894.7 | 477.52 | 286 | 60 | 10 | ||
| MMSGC344 | 440566.41 | 6830894.9 | 474.58 | 286 | 60 | 25 | ||
| MMSGC345 | 440559.53 | 6830896.6 | 474.72 | 286 | 60 | 45 | ||
| MMSGC346 | 440552.85 | 6830898.6 | 475.04 | 286 | 60 | 45 | ||
| MMSGC347 | 440546.13 | 6830900.5 | 475.52 | 286 | 60 | 45 | ||
| MMSGC348 | 440539.45 | 6830902.4 | 475.83 | 286 | 60 | 45 | ||
| MMSGC427 | 440478.88 | 6830410.4 | 466.34 | 286 | 60 | 50 | ||
| MMSGC428 | 440483.55 | 6830419.6 | 466.13 | 286 | 60 | 55 | ||
| MMSGC429 | 440495.74 | 6830436.8 | 466.31 | 286 | 60 | 70 | ||
| MMSGC430 | 440492.58 | 6830448.2 | 466.21 | 286 | 60 | 65 | ||
| MMSGC431 | 440495.37 | 6830457.9 | 466.04 | 286 | 60 | 65 | ||
| MMSGC432 | 440497.95 | 6830477.8 | 466.49 | 286 | 60 | 65 |
Market Announcement | Page 39 of 50
| Criteria | Explanation | Explanation | Explanation | ||||
|---|---|---|---|---|---|---|---|
| MMSGC433 | 440507.33 | 6830485.6 | 467.05 | 286 | 60 | 75 | |
| MMSGC434 | 440506.16 | 6830496.4 | 467.09 | 286 | 60 | 70 | |
| MMSGC435 | 440499.72 | 6830498.3 | 467.06 | 286 | 60 | 55 | |
| MMSGC436 | 440501.45 | 6830508 | 467.76 | 286 | 60 | 65 | |
| MMSGC437 | 440506.95 | 6830516.8 | 467.54 | 286 | 60 | 70 | |
| MMSGC438 | 440505 | 6830548.3 | 468.86 | 286 | 60 | 65 | |
| MMSGC439 | 440468.84 | 6830558.7 | 469.1 | 286 | 60 | 40 | |
| MMSGC440 | 440504.99 | 6830558.9 | 469.33 | 286 | 60 | 70 | |
| MMSGC441 | 440498.39 | 6830560.8 | 469.43 | 286 | 60 | 50 | |
| MMSGC442 | 440490.43 | 6830562.8 | 469.55 | 286 | 60 | 60 | |
| MMSGC443 | 440490.98 | 6830386.2 | 467.14 | 286 | 60 | 60 | |
| MMSGC444 | 440497.75 | 6830384.4 | 467.15 | 286 | 60 | 70 | |
| MMSGC446 | 440556.6 | 6830575.6 | 468.61 | 286 | 60 | 70 | |
| MMSGC447 | 440482.19 | 6830399.1 | 466.73 | 286 | 60 | 55 | |
| MMSGC448 | 440488.86 | 6830397.3 | 466.76 | 286 | 60 | 65 | |
| MMSGC449 | 440495.64 | 6830395.4 | 466.77 | 286 | 60 | 70 | |
| MMSGC450 | 440484.98 | 6830408.8 | 466.53 | 286 | 60 | 65 | |
| MMSGC451 | 440490.52 | 6830417.6 | 466.12 | 286 | 60 | 70 | |
| MMSGC452 | 440497.09 | 6830426.1 | 466.07 | 286 | 60 | 70 | |
| MMSGC453 | 440504.26 | 6830434.9 | 466.3 | 286 | 60 | 70 | |
| MMSGC454 | 440502.35 | 6830455.8 | 466.83 | 286 | 60 | 65 | |
| MMSGC458 | 440553.99 | 6830565.9 | 468.44 | 286 | 60 | 60 | |
| MMSGC459 | 440560.73 | 6830564 | 468 | 286 | 60 | 70 | |
| MMSGC461 | 440585.19 | 6830858.4 | 473.6 | 286 | 60 | 35 | |
| MMSGC462 | 440571.75 | 6830862.1 | 473.96 | 286 | 60 | 50 | |
| MMSGC463 | 440578.44 | 6830860.3 | 473.69 | 286 | 60 | 60 | |
| MMSGC464 | 440565.11 | 6830864.1 | 474.33 | 286 | 60 | 70 | |
| MMSGC465 | 440583.18 | 6830869.3 | 473.59 | 286 | 60 | 70 | |
| MMSGC466 | 440570.37 | 6830883.3 | 474.31 | 286 | 60 | 65 | |
| MMSGC467 | 440573.19 | 6830893 | 474.42 | 286 | 60 | 10 | |
| MMSGC468 | 440532.82 | 6830904.4 | 476.4 | 286 | 60 | 20 | |
| MMSGC470 | 440530.63 | 6830915.3 | 476.08 | 286 | 60 | 15 | |
| MMSGC471 | 440537.32 | 6830913.4 | 475.76 | 286 | 60 | 25 | |
| MMSGC472 | 440554.67 | 6830908.6 | 475.1 | 286 | 60 | 55 | |
| MMSGC473 | 440538.21 | 6830923.6 | 475.2 | 286 | 60 | 20 | |
| MMSGC474 | 440544.89 | 6830921.6 | 475.2 | 286 | 60 | 40 | |
| MMSGC475 | 440551.65 | 6830919.8 | 475.06 | 286 | 60 | 45 | |
| MMSGC476 | 440566.07 | 6830915.8 | 474.78 | 286 | 60 | 60 | |
| MMSGC477 | 440572.73 | 6830913.9 | 474.62 | 286 | 60 | 70 | |
| MMSGC479 | 440540.74 | 6830943.6 | 475.25 | 286 | 60 | 20 | |
| MMSGC480 | 440547.33 | 6830941.7 | 475.19 | 286 | 60 | 30 | |
| MMSGC481 | 440554.13 | 6830939.9 | 475.15 | 286 | 60 | 40 | |
| MMSGC482 | 440560.84 | 6830937.9 | 474.96 | 286 | 60 | 55 | |
| MMSGC483 | 440575.23 | 6830933.8 | 474.75 | 286 | 60 | 70 | |
| MMSGC484 | 440547.28 | 6830952.2 | 475.29 | 286 | 60 | 35 | |
| MMSGC485 | 440558.78 | 6830948.9 | 475.16 | 286 | 60 | 40 | |
| MMSGC486 | 440567.47 | 6830946.5 | 474.98 | 286 | 60 | 50 | |
| MMSGC487 | 440574.15 | 6830944.6 | 474.82 | 286 | 60 | 55 | |
| MMSGC488 | 440551.85 | 6830961.2 | 475.45 | 286 | 60 | 15 | |
| MMSGC489 | 440580.68 | 6830953.1 | 474.78 | 286 | 60 | 70 | |
| MMSGC490 | 440573.62 | 6830975.9 | 475.28 | 286 | 60 | 40 | |
| MMSGC491 | 440589.98 | 6830971.3 | 475.03 | 286 | 60 | 70 | |
| MMSGC492 | 440596.79 | 6830969.4 | 474.96 | 286 | 60 | 50 | |
| MMSGC493 | 440603.51 | 6830967.6 | 474.9 | 286 | 60 | 50 | |
| MMSGC494 | 440610.14 | 6830965.7 | 474.76 | 286 | 60 | 40 | |
| MMSGC495 | 440582.07 | 6830984 | 475.33 | 286 | 60 | 60 | |
| MMSGC496 | 440600.39 | 6830978.7 | 475.18 | 286 | 60 | 70 | |
| MMSGC497 | 440591.22 | 6831012.5 | 475.9 | 286 | 60 | 50 | |
| MMSGC498 | 440596.91 | 6831011 | 475.89 | 286 | 60 | 70 | |
| MMSGC499 | 440613.37 | 6831006.2 | 475.74 | 286 | 60 | 70 | |
| Data aggregation methods |
• Mineralised intersections are reported at a 0.5g/t Au cut-off with a minimum reporting width of 1m for RC holes and 0.2m for diamond holes, composited to 1m. |
Data aggregation • Mineralised intersections are reported at a 0.5g/t Au cut-off with a minimum reporting width of 1m for methods RC holes and 0.2m for diamond holes, composited to 1m.
| Criteria | Explanation |
|---|---|
| Relationship between mineralisation widths and intercept lengths |
• Holes were drilled orthogonal to mineralisation as much as possible, however the exact relationship between intercept width and true width cannot be estimated exactly in all cases. |
| Diagrams | • Refer to Figures and Tables in body of the release. |
| Balanced reporting |
• All drill assay results used in this estimation are published in previous news releases. • Historic drill hole results available on WAMEX. |
| Other substantive exploration data |
• There is no other material exploration data to report at this time. |
| Further work | • The company is designing drill programs to follow up on the results of these re-models. |
Market Announcement | Page 41 of 50
Section 3 Estimation and Reporting of Mineral Resources
(Criteria listed in section 1, and where relevant in section 2, also apply to this section)
| Criteria | Explanation |
|---|---|
| Database integrity | • Data was geologically logged electronically; collar and downhole surveys were also received electronically as was the laboratory analysis results. These electronic files were loaded into an acQuire database by the company in-house Database Administrator. Data was routinely extracted to Microsoft Access during the drilling program for validation by the geologist in charge of the project. • FML’s database is a Microsoft SQL Server database (acQuire), which is case sensitive, relational and normalised to the Third Normal Form. Because of normalisation, the following data integrity categories exist: • Entity Integrity: no duplicate rows in a table, eliminated redundancy and chance of error. • Domain Integrity: Enforces valid entries for a given column by restricting the type, the format or a range of values. • Referential Integrity: Rows cannot be deleted which are used by other records. • User-Defined Integrity: business rules enforced by acQuire and validation codes set up by FML. • Additionally, in-house validation scripts are routinely run in acQuire on FML’s database and they include the following checks: • Missing collar information • Missing logging, sampling, downhole survey data and hole diameter • Overlapping intervals in geological logging, sampling, down hole surveys • Checks for character data in numeric fields • Data extracted from the database were validated visually in GEOVIA Surpac software and ARANZ Geo Leapfrog software. Also, when loading the data any errors regarding missing values and overlaps are highlighted. • Historic data has been validated against WAMEX reports where possible. |
| Site visits | • Alex Aaltonen, the Competent Person for Sections 1 and 2 of Table 1 is FML’s General Manager - Exploration and conducts regular site visits. • Hannah Kosovich, the Competent Person for Section 3 of Table 1 is FML’s Resource Geologist and last visited site in September 2019. |
| Geological interpretation | • All available drill hole and historic mining data was used to guide the geological interpretation of the mineralisation. • The mineralised geological interpretation was completed using Seequent Leapfrog software on a section-by-section basis. All available drill hole and pit mapping data was used with an approximate 0.5g/t Au value cut-off to guide the interpretation. • Mineralisation along the Chatterbox Trend has previously been modelled as discrete and discontinuous individual deposits. Not with a view of the structural controls over the whole trend. The aim of this remodel was to look at the shear zone as one large deposit that is later sub-divided into the historically defined individual deposits. oA total of 56 individual lodes have been modelled along the Chatterbox trend. o10 closely spaced lodes were modelled within the Rumor deposit that strike NNE curving towards the NE to the north, dipping 60° to the East. The three most southern lodes have a flatter 45° easterly dip. oApollo is the longest of the three deposits and had 32 individual lodes modelled along its strike. The mineralisation has been interpreted from the end of what is considered the Rumor footprint striking NE before curving to a Northerly trend at the northern extents. Two corepervasive |
| lodes have been modelled dipping 65° to the east, with numerous closely spaced smaller lodes in the footwall and hanging wall dipping from 30° to 70° to the east along the entire Apollo strike. To the west of the main Apollo trend two NNE trending lodes dipping 45° to the east have been modelled. oSlightly offset to the East from Apollo in the north lies the Eclipse (Garden Well) deposit that has one N-S, 60° dipping lode modelled through the historic pit area and to the east, two N-NNW trending closely spaced lodes dipping 55° to the east. oInnuendo to the north has ten lodes modelled, in the south five stacked lodes trend NNE and dipping 60°to the east. The mineralisation then swings to the NNW where four stacked lodes dip ~ 55° to the NE. Approx 150m to the North of this a further two NNW trending 60° dipping lodes have been interpreted. • Along the West Laverton Trend, a total of 13 individual lodes were modelled. oAt Rega two lodes were modelled, one main lode within the existing pit and a second lode ~ 150m to the west. Both strike NNW with a gentle ~25° dip to the ESE and gently plunging to the east. Within the main in- pit lode, two higher grade internal “core” lodes were modelled. These HG core lodes have hard boundaries between themselves and the surrounding main lode. There is no defined northing or cut-off for the Rega / West Laverton mineralisation extents and the two deposits interlace each other at the southern edge of the Rega pit wall. oSix lodes were modelled at West Laverton, two hanging wall and two footwall lodes adjacent to two splay lodes. All lodes are closely spaced and sub-parallel to each other, striking NNE, gently dipping ~ 25° to the ESE and gently plunging to the east, similarly to Rega. Bulldog sits some 900m along strike to the south of West Laverton and consists of five lodes. All are closely spaced, sub-parallel with similar orientations to West Laverton and Rega. oBulldog sits some 900m along strike to the south of West Laverton and consists of five lodes. All are closely spaced, sub-parallel with similar orientations to West Laverton and Rega. • Gladiator Trend had a total of 54 individual lodes have been modelled. oGladiator West is closely associated with Gladiator Underground footwall, 21 closely spaced lodes were modelled within the Gladiator West deposit that strike NNE, dipping 45° to the East. The three most southern lodes have a flatter 27° easterly dip. oMurrays deposit was modelled in 4 lodes striking NNE, dipping 51° to the East. oCousin Murray was modelled in 7 lodes striking NW, dipping 75° to the SW. oGladiator south was modelled in 19 lodes overall striking North, dipping 70° to the East with northeastern lodes striking NNW. oCentral BIF was modelled in 1 lode striking NNW dipping 53° to the East. NE BIF was modelled in 1 lode striking north, dipping 79° to the East. • Mineralisation at Craigiemore and Mary Mac is commonly associated with quartz veining and disseminated pyrite within the silica altered chert horizons of the BIF. It can also be found in the mafic host rocks near the BIF contact. Understanding the relationship between gold mineralisation and the BIF was used to guide the interpretation. Lithological logging of BIF and mafic host rocks was consistent across drill holes and allowed for an accurate lithological model to be constructed. This model highlighted the contacts and thickened zones of BIF where gold mineralisation is prevalent. Geophysics was also used to guide the interpretation with the BIF highlighted by regional and project scale surveys. A site visit and pit analysis confirmed the vein orientation. oAt Craigiemore and Mary Mac numerous tightly spaced sub vertical |
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Market Announcement | Page 43 of 50
| lodes were identified striking north-south with a moderate plunge to the north. Minor northwest striking sub vertical splays were also identified. oIncreased thrust faulting and drag folding enhances the structural complexity at Mary Mac Hill. Two orientations were identified, north south striking BIF hosted lodes that dip steeply to the east and more moderate east dipping quartz and shear hosted lodes. oA total of 23 individual lodes were modelled at Craigiemore. Two sets of closely spaced north trending sub-vertically dipping lodes that gently plunge to the north. oIn the “gap” between Craigiemore and Mary Mac, two NNW trending, sub-vertical lodes have been interpreted. oA remnant ROM Pad stockpile exists and has been modelled to the immediate East of the current open pit berm. The triangular shaped stockpile extends 275m at its longest, 190m at its widest and averages 5m thick. oCovering the entire CM-MM-GP resource area a thin continuous Supergene layer of mineralised enrichment has been modelled as a surface. However, lack of RC/DD drilling away from the pits has affected its estimation. oA total of 59 individual lodes have been modelled along the MM/GP trend. oMary Mac South consists of 12 stacked, NNW trending, sub-vertically dipping lodes that extend over 470m from near surface to approx. 210m below ground. oMary Mac North consists of 5 stacked NW trending sub-vertical lodes intersected by 5 flatter dipping lodes modelled over 270m from near surface to 180m below. oMary Mac Hill consists of 11 stacked flat dipping lodes intersected by 20 steep NNW trending lodes that has been modelled over 385m from near surface to 150m below surface. oGolden Pinnacles consists of 6 lodes of variable orientations and limited strike that has been modelled from near surface to approx. 100m below. • |
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| Dimensions | • The entire Chatterbox Trend was remodelled as one project in Leapfrog, over a 5.7 km NNE – North - NNW strike length. oRumor has been interpreted over a 1.5km NE – NNE trending strike from near surface to 230m below ground, however the average depth modelled is 120m. Widths vary from 1m to 17m. oApollo trends NNE over a 1.5km strike before swinging to the North for a further 900m. Lodes average 150m depth but have been interpreted to 330m at the deepest point of drill penetration. Lode widths vary from 1m to 20m wide. oEclipse is the smallest of the deposits – inferred over a 600m N to NNW strike from near surface to 150m below ground with 1m – 10m wide lodes. oInnuendo extends over 1.4km, 300m striking to the NNE before swinging to the NNW for 1.1km. Mineralisation has been modelled from near surface to 230m below surface and vary from 1m 10 16m wide. • Overall, the West Laverton Trend has been modelled over a 2.2km strike length. oWest Laverton/Rega has been modelled over 850m with a gap of 900m before Bulldog has been interpreted over 500m strike. The lodes are interpreted from near surface to approximately 150m below surface, limited by depth of drilling. Lodes have been interpreted from 1m to 25m thick. |
| • The Gladiator deposits were remodelled as one project in Leapfrog, over a 2 km NNE – North - NNW strike length. oGladiator West has been interpreted over 570m NNW trending strike from near surface to 300m below ground level, however the average depth approximates 170m. Width vary from 2.5m to 15m. oMurrays has been interpreted over 950m NNE trending strike from near surface to 130m below ground level. Widths vary from 2.5m to 25m. oCousin Murray has been interpreted over 275m NNW trending strike from near surface to 167m below ground level. Widths vary from 1m to 8m. oGladiator South has been interpreted over 1080m NNW trending strike from near surface to 160m below ground level. Widths vary from 1m to 15m. oCentral BIF and NE BIF have been interpreted over 800m and 500m respectively North trending strike from near surface to 150m and 50m below ground level Width vary from 1m to 4m. • The entire Craigiemore – Mary Mac – Golden Pinnacles Trend was remodelled as one project in Leapfrog, over a 2.8km N to NNW strike length. The lodes are interpreted from near surface to approximately 230m below surface, limited by depth of drilling. Lodes have been interpreted from 1m to 15m thick. oCraigiemore has been modelled over 960m with a gap of 75m before a further two lodes have been interpreted over 185m strike. oMary Mac South through to Golden Pinnacles (MM/GP) extends over 1.6km NNW trending strike. |
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| Estimation and modelling techniques |
• All deposits used an Ordinary Kriging (OK) estimate run in Datamine software. Snowden Supervisor software was used for geostatistical analysis and variography of the individual lode composited samples. Chatterbox: • Drill hole data was selected within mineralised lodes. Boundaries between lodes were considered hard boundaries and no data is shared between lodes. All drill hole data was composited to 1m downhole intervals – 1m is the dominant raw sampling interval. • Samples flagged as unreliable or wet were set to absent and ignored in the estimation process. • A review of histograms, probability plots and mean/variance plots for the individual lodes revealed outlier sample values. A maximum top-cut of 20ppm Au and an average of 7ppm Au was used for Apollo, only two lodes were top- capped at Eclipse – 25ppm and 8ppm Au, a max of 15ppm Au and average of 9ppm Au for Rumor and a max of 8ppm and average of 4ppm Au for Innuendo. Assays above the top-cut are set to the top-cut value. • Variography was modelled on data transformed to normal scores, the variogram models were back transformed to original units before exporting. • Variography was performed on the individual lodes with larger sample numbers, a total of 26 variograms were modelled along the Chatterbox trend. • These models were shared with the other lodes of similar orientation and proximity. • The back-transformed variogram models had moderate nugget effects (12% to 48% of total sill), with a range from 28m for the smaller lodes through to 170m for the largest lodes at Apollo. • Estimation (via Ordinary Kriging) was into a non-rotated block model in MGA94 grid, with a parent block size about the average drill spacing within the deposit areas, Apollo and Eclipse was 5 mE x 10 mN x 5 mRL with the infill RC grade control holes; Rumor and Innuendo was 10 mE x 25 mN x 5 mRL. Sub-blocking was used to best fill the wireframes and inherit the grade of the parent block. |
Market Announcement | Page 45 of 50
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The ellipsoid search parameters used the variogram ranges, with a minimum of 6 and maximum of 16-18 samples per block estimate was used. After the first pass for un-estimated blocks, the search distance was expanded by a factor of two and the minimum number of samples dropped to 4. A third pass was then run with an increased search distance by a factor of four and the same minimum number of samples. A few lodes across all deposits had blocks not fill after the third pass, this was in areas at the extents of strike or in outside the main strike in the FW and HW lodes. For a small number of missing blocks in a lode, the average of the surrounding blocks was used. This was below cut-off grade and the blocks assigned sub-inferred, unclassified. For large numbers of absent blocks, a 0.01ppm Au was assigned.
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Along the main strike, lodes had high numbers of blocks filling in the first pass, 99% in a few lodes at Apollo. Smaller lodes along FW or HW had lower first pass estimation ~ 50% of blocks had estimated. In the second pass an average of 46% of blocks estimated. an average of 11% of blocks estimated in the third search pass.
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The estimate was validated by visually stepping through the estimated blocks and sample data in Datamine. Comparing the estimated block statistics with composited sample data and generate trend (Swath) plots to ensure the estimate was honouring the trends of the data. Also, a review of the output parameters from the estimation process like kriging variance, negative weights, search distances and sample numbers.
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Following a review of estimated lode grades vs composite lode grades, a “distance limited search” was applied to lodes that had high grades being spread into areas of fewer lower grade samples artificially influencing the grades of these blocks.
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The process is to apply a distance limit, 10m for Eclipse, 20m for Apollo and 25m for Rumor and Innuendo, to samples above a cut-off grade. Outside the 10m – 25m search ellipse, assays above cut-off are removed from the estimation, resulting in blocks better honouring the low grades in areas of less drilling. Different grades were used for different deposits, Apollo = 10ppm Au, Rumor = 8ppm Au, Eclipse = 6ppm and Innuendo = 4.5ppm Au top-cut applied.
West Laverton:
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Drill hole data was selected within mineralised domains and then within the internal vein set lodes. Boundaries between veins and the surrounding domain were considered hard boundaries and no data is shared between lodes or between domains and lodes. All drill hole data was composited to 1m downhole intervals – 1m is the dominant raw sampling interval.
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outlier sample values. A maximum top-cut of 15ppm Au and an average of 10ppm Au was used for the different lodes, with assays above the top-cut set to the top-cut value.
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Normal scores variography was performed on the individual lodes with larger sample numbers, in total 9 variograms were modelled and shared with the other lodes of similar orientation and proximity.
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The back-transformed variogram models had moderate to high nugget effects (26 to 36% of total sill), with a range from 20m to 100m for the lodes. In general, the ranges for the variograms were quite short, averaging 40m.
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• Estimation (via Ordinary Kriging) was into a non-rotated block model in MGA94 grid, with a parent block size of 10 mE x 10 mN x 5 mRL – this is about the average drill spacing in the deposit. Sub-blocking was used to best fill the wireframes and inherit the grade of the parent block.
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The ellipsoid search parameters used the variogram ranges, with a minimum of 8 and maximum of 14 samples per block estimate was used. After the first pass 57% of blocks had estimated, primarily due to the short search range used. For un-estimated blocks after this first pass, the search distance was
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expanded by a factor of two and the minimum number of samples dropped to 4. In the second pass 30% of blocks estimated. A third pass was then run with an increased search distance by a factor of four and the same minimum number of samples, 13% of blocks estimated in the third search pass.
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The estimate was validated by the same process described above.
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Following the review, a “distance limited search” described in Chatterbox was applied to 5 lodes that had high grades being spread into areas of fewer lower grade samples artificially influencing the grades of these blocks. A distance limit of 20m was selected based on a visual review of sample spacing in affected lodes and a grade cut-off above 5ppm.
Gladiator:
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Drill hole data was selected within mineralised lodes. Boundaries between lodes were considered hard boundaries and no data is shared between lodes. All drill hole data was composited to 1m downhole intervals – 1m is the dominant raw sampling interval.
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A review of histograms, probability plots and mean/variance plots for the individual lodes revealed outlier sample values. A maximum top-cut of 12ppm Au was applied to a Gladiator lode, an average of 5ppm Au was used for Gladiator and Murrays with an average of 4ppm Au at Cousin Murray. Topcapping was lower at Gladiator West with an average of 2.75ppm Au used. Assays above the top-cut are set to the top-cut value.
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Variography was performed on the individual lodes with larger sample numbers. The skewed data sets were transformed to normal scores, the variogram models were back transformed to original units before exporting. Nine variograms were modelled at Gladiator, three at Murrays, one at Cousin Murray and two variograms modelled at Gladiator West. The variogram models were shared with the other lodes of similar orientation and proximity. The back-transformed variogram models had moderate to high nugget effects (18% to 48% of total sill), with a range from 31m for the smaller lodes through to 100m for the largest lodes at Gladiator.
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Estimation (via Ordinary Kriging) was into a non-rotated block model in MGA94 grid, with a parent block size of 5 mE x 10 mN x 5 mRL – this is about the average drill spacing in the deposit. Sub-blocking was used to best fill the wireframes and inherit the grade of the parent block.
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The ellipsoid search parameters used the variogram ranges, with a minimum of 6 and maximum of 12 - 18 samples per block estimate was used. The variable maximum sample numbers used depended on size of the lode and drill spacing. After the first pass 60% of blocks had estimated, for unestimated blocks after this first pass, the search distance was expanded by a factor of two and the minimum number of samples dropped to 4. In the second pass 35% of blocks estimated. A third pass was then run with an increased search distance by a factor of four and the same minimum number of samples, 5% of blocks estimated in the third search pass.
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The estimate was validated by the same process described in the Chatterbox estimate.
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Following a review of estimated lode grades vs composite lode grades, the “distance limited search” method was applied to 2 lodes that had high grades being spread into areas of fewer lower grade samples artificially influencing the grades of these blocks. A distance limit of 10m was selected and a grade cut-off above 5ppm.
Craigiemore/Mary Mac:
- Drill hole data was selected within mineralised lodes. Boundaries between lodes were considered hard boundaries and no data is shared between lodes. All drill hole data was composited to 1m downhole intervals – 1m is the dominant raw sampling interval.
Market Announcement | Page 47 of 50
| • A review of histograms, probability plots and mean/variance plots for the individual lodes revealed outlier sample values. A maximum top-cut of 25ppm Au and an average of 9.5ppm Au was used for Craigiemore and an average of 7ppm Au for Mary Mac. Assays above the top-cut are set to the top-cut value. • Normal Scores variography was performed on the individual lodes with larger sample numbers, 17 variograms were modelled at Craigiemore and 37 variograms at Mary Mac. These models were shared with the other lodes of similar orientation and proximity. • The back-transformed variogram models had low to moderate nugget effects (6% to 35% of total sill), with a range from 25m for the smaller lodes through to 127m for the largest lodes. • Estimation (via Ordinary Kriging) was into a non-rotated block model in MGA94 grid, with a parent block size of 5 mE x 10 mN x 5 mRL – this is about the average drill spacing in the deposit. Sub-blocking was used to best fill the wireframes and inherit the grade of the parent block. • The ellipsoid search parameters used the variogram ranges, with a minimum of 6 and maximum of 14 samples per block estimate was used. After the first pass 88% of blocks had estimated, for un-estimated blocks after this first pass, the search distance was expanded by a factor of two and the minimum number of samples dropped to 4. In the second pass 11% of blocks estimated. A third pass was then run with an increased search distance by a factor of four and the same minimum number of samples, 1% of blocks estimated in the third search pass. • The estimate was validated by methods described above at Chatterbox. • Following the review, a “distance limited search” was applied to 5 lodes that had high grades being spread into areas of fewer lower grade samples artificially influencing the grades of these blocks. A distance limit of 10m and a grade cut-off above 5ppm was used. |
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| Moisture | • Tonnages are estimated on a dry basis. |
| Cut-off parameters | • The mineral resource has been reported above a 0.6g/t Au cut-off for open pit for all deposits. |
| Mining factors or assumptions |
• It has been assumed in this report that all deposits would be mined by open pit methods, with most requiring a cut-back on existing open pits before continuing to extend the pits deeper. • Maiden pits would be at Rumor, Innuendo, Cousin Murray Gladiator West and Golden Pinnacle. |
| Metallurgical factors or assumptions |
• Various test work has been conducted across all the deposit trends over the years by various companies. • At the Chatterbox as part of the PFS trial pit by PDJV, metallurgical test work was carried out on Apollo ore with excellent recovery (94.4%) and fast leaching observed. In November 2011 Crescent Gold submitted samples from Eclipse to ALS Ammtec that represented the 3 different weathering profile ore types. Overall gravity gold recovery was moderate, gravity separation/cyanide leach recovery was good (92.7-98.6%) with low cyanide consumption. • Historical metallurgical test work has been carried out at West Laverton prior to mining by Ashton. Test work on oxide samples reported 9.8% gravity Au recovery and high (+92%) recovery from cyanidation. Transitional samples had an 89.9% recovery post 24hr cyanidation. Milling data was unavailable as ore had been blended with other sources. In 2009 Crescent gold commissioned a series of test work on oxide, transitional and fresh ore samples from West Laverton. Test work included gravity separation and direct cyanidation, rock properties for mill performance on two diamond composite samples and mineralogical studies on gold bearing samples by thin section and XRD. The samples for gold extraction indicated gravity gold recovery ~ 20% and high total extraction of +94% for all ore weathering types. |
| • Gladiator test work was conducted on samples by Asthon prior to mining in 1989 using Normet Pty Ltd and again in April 1991 using Ammtec and Murrays was tested in May 1991 but was not included in the WAMEX reports. Gladiator/Murrays ore was blended during milling and data is unavailable. • At Craigiemore and Mary Mac metallurgical test work was carried out by AMMTEC on behalf of Hill Minerals NL in February 1989. Crescent Gold also carried out test work through AMMTEC prior to mining commencing at both Craigiemore and Mary Mac. With recoveries over 94%. A mineralogical analysis was conducted in June 2010 through AMMTEC. A total of 4 samples from Craigiemore, representing the main lode and SE lode’s oxide layer and fresh rock were submitted and showed high gold liberation. |
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| Environmental factors or assumptions |
• All deposits have been historically mined by either open pit or underground methods and existing ground disturbances including haul roads and waste dumps exist in the area. There are no unforeseen environmental considerations that would prevent open pit mining from re-commencing in the area. |
| Bulk density | • Density values used across the deposits comes from a mix of diamond core testing to rock sample test work conducted during the mining process, all test work using the water immersion SG test. • Density values were assigned based on weathering profile and/or mineralisation or waste classification. • Along the Chatterbox within the mineralised lodes an average t/m3 of 1.82 was used in oxide, 2.54 Transitional and 2.75 Fresh. In the waste an average t/m3 of 1.8 was used in oxide, 2.34 Transitional and 2.75 Fresh. • At West Laverton density values were assigned based on weathering profile using the average results from 2008 test work. The water immersion SG test work was conducted on diamond core samples collected from two Crescent diamond holes. However, no fresh rock was encountered and an average SG for fresh basalt was applied. An average SG of 2.1t/m3 for oxidised, 2.24 t/m3 for transitional material and 2.70 t/m3 for Fresh rock were applied. • Gladiator used average densities applicable to the region after a review of the figures used by Ashton during mining to be too high given the more recent mining by Crescent at nearby deposits. An average SG of 1.80t/m3 for oxidised, 2.40 t/m3 for transitional material and 2.75 t/m3 for Fresh rock were applied. • CM/MM density values were assigned based on weathering profile and rock type using water immersion SG test work on rock samples collected during Crescent mining operations. In the Mafic units an average t/m3 of 1.84 was used in oxide, 2.49 Transitional and 2.78 Fresh. In the BIF formation an average t/m3 of 2.2 was used in oxide, 2.5 Transitional and 3.1 Fresh. |
| Classification | • Material has been classified Indicated and Inferred based on a number of criteria such as geological continuity, drill hole spacing, estimation pass and proximity to the existing open pits. • Chatterbox blocks within the 12.5m x 12.5m to 25m x 25m close spaced drill pattern that estimated in the first pass was classified as Indicated. Blocks where drill spacing increased to 25m x 50m to 50m x 50m and estimated in the second or third pass were classified as Inferred. Inferred resources are predominantly at the extents of the deposits and at depth. Rumor was classified as Inferred given the wet sampling issues and lack of more recent Crescent/FML drilling. Blocks in areas where the drilling extends to 100m spacing blocks have not been classified and are used for target generation for future drill programs. • Resources along the West Laverton Trend have been classified as Indicated and Inferred. West Laverton/Rega resources that are within the tight drill spacing of 10m x 10m to 20m x 15m that primarily filled in the first search pass have been classified as Indicated. These blocks are mostly in the transitional weathering zone between and beneath the existing openpits. Inferred |
Market Announcement | Page 49 of 50
resources at West Laverton/Rega are the fringe blocks where the drill spacing has increased to 30m x 30m to 30m x 60m and blocks at depth (~ below 85m from surface) with less drill penetration. Bulldog has been classified as Inferred and requires follow up drilling by FML to confirm the historic Ashton drilling.
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Gladiator resources within the 25m grid drill spacing that predominantly estimated in the first pass were assigned as Indicated. Blocks at depth where drill coverage was patchy and smaller hanging wall lodes supported by less drill holes were assigned Inferred category. Cousin Murray was assigned Inferred given the lack of recent drilling and mining activity. A shape was created at Gladiator West to classify blocks in the predominantly 25m grid drill pattern.
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Along the entire CM/MM trend Indicated Resources were those unmined blocks within the close drill spacing of 10m x 10m and 20m x 10m, these blocks primarily filled in the first search pass. Blocks that were either in areas of less drill density or at depth along the fringes of the lodes where follow up deeper holes are required were classified as Inferred. The two “gap” lodes north of Craigiemore were primarily assigned Inferred status. Golden Pinnacles resource area has been classified as Inferred and warrants further drilling.
Audits or reviews
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No external Audits of the mineral resource have been conducted.
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Discussion of relative • This is addressed in the relevant paragraph on Classification above. accuracy/ confidence • The Mineral Resource relates to global tonnage and grade estimates.