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ARDEA RESOURCES LIMITED — Capital/Financing Update 2017
Jun 12, 2017
64421_rns_2017-06-12_6919086e-a19d-4259-adcc-8d3835dcce34.pdf
Capital/Financing Update
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Cobalt at Black Range exceeds expectations; associated with scandium and platinum group metals
ASX & Media Release
13 June 2017
ASX Symbol
ARL
Extensive and continuous cobalt-nickel mineralisation underlies and is closely associated with newly-discovered scandium and accessory platinum and palladium.
Ardea Resources Limited
Suite 2 / 45 Ord St West Perth WA 6005 PO Box 1433 West Perth WA 6872
- Extensive blanket of strong cobalt and nickel mineralisation intercepted at Black Range.
Telephone
+61 8 6244 5136
- Scandium discovered at Black Range as a significant surface enrichment, with accessory platinum and palladium being widely distributed. Together, these metals form a continuous sheet of mineralisation commonly from surface.
Website
www.ardearesources.com.au
- Cobalt-nickel intercepts include:
Directors
- ABR0006, 10 m at 0.12 % Co and 0.74 % Ni from 16.0 m
Katina Law Chair
- ABR0008, 16 m at 0.16 % Co and 0.74 % Ni from 60.0 m
Matt Painter Managing Director
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ABR0009, 10 m at 0.12 % Co and 0.81 % Ni from 34.0 m
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ABR0013, 10 m at 0.21 % Co and 0.75 % Ni from 4.0 m
Ian Buchhorn Non-Executive Director
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ABR0014, 8 m at 0.20 % Co and 0.87 % Ni from 2.0 m
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Other metals contained in the laterite show potential for added credits during open pit cobalt and nickel mining.
Issued Capital
Shares 67,000,747
- Scandium (45 – 170 g/t)
Unlisted options 12,310,022
- Platinum and palladium (0.5 – 1.29 g/t)
Loyalty options 26,436,923
-
Chromium (0.5 – 2.95 %)
-
Ability to provide payable credits, notably scandium, will be determined during the KNP Cobalt Zone PreFeasibility Study
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Upgraded resource to be modelled incorporating new data.
Cobalt, Scandium & PGM results from Black Range
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The Black Range RC drilling program
Ardea Resources Limited (ASX: ARL, “Ardea” or “the Company”) is pleased to announce that drill results have been received for the recent Reverse Circulation (RC) drilling program at Black Range. Exceptional results confirm high-grade cobalt and nickel mineralisation, and highlight potentially significant occurrences of scandium, with accessory platinum-palladium and chromium mineralisation.
A series of 27 RC drill holes was drilled in March and April 2017. The program totalled 1,996 m with 1007 new assays recorded (not including standards, blanks etc.). The program was designed to progress the Black Range project on several fronts:
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To augment and confirm historic cobalt and nickel results and further define their distributions.
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To upgrade the resource classification (if appropriate) through increased drillhole density.
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To determine whether scandium is present and, if so, define its distribution within the laterite profile.
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To confirm and expand upon historically poorly-defined platinum and palladium mineralisation.
The drill program has been a success.
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High-grade and extensive cobalt and nickel mineralisation was intercepted in numerous holes.
-
Scandium mineralisation was discovered with similar though more extensive distributions than the platinoid metals. Much of the scandium mineralisation is exposed at surface in association with significant chromium.
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Platinum and palladium (PGMs) are widely distributed as a coherent blanket of shallow mineralisation that is exposed at surface in many places and would be mined in any event to access the cobalt-nickel mineralisation. There is commonly high copper anomalism associated with the PGMs, suggesting a nickel-copper primary source.
Work has commenced on upgrading the resource at Black Range.
Cobalt and nickel results from Black Range
Cobalt and nickel mineralisation dominates at Black Range where they will drive any future mining operations. Numerous cobalt-mineralised intervals were detected. Highlights include:
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ABR0003, 8 m at 0.17 % cobalt and 0.69 % nickel from 8.0 m[1]
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ABR0006, 10 m at 0.12 % cobalt and 0.74 % nickel from 16.0 m
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ABR0008, 16 m at 0.16 % cobalt and 0.60 % nickel from 60.0 m
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ABR0009, 10 m at 0.12 % cobalt and 0.81 % nickel from 34.0 m
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ABR0013, 10 m at 0.21 % cobalt and 0.75 % nickel from 4.0 m
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ABR0014, 8 m at 0.20 % cobalt and 0.87 % nickel from 2.0 m
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ABR0022, 10 m at 0.27 % cobalt and 0.91 % nickel from 14.0 m
A full listing of all calculated intercepts is shown in Appendix 1.
1 All newly defined intercepts at Black Range were calculated using the following parameters: • 0.10 % cobalt minimum cutoff • 2 m minimum intercept • 4 m internal waste
Cobalt, Scandium & PGM results from Black Range
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Figure 1 – Map of the outcrop geology of the Black Range project. New drill collars are shown in red. Ultramafic rocks are shown in purple and largely underlie the laterite (R-f) where most drill holes are collared.
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Cobalt, Scandium & PGM results from Black Range
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High-grade cobalt mineralisation
Exceptional high-grade mineralisation is concentrated in several locations, often over thick intervals. A summary of some of the highest-grade zones is shown in Table 1 below.
Table 1 – Examples of high-grade intervals from Black Range. Each assay represents 2 metres downhole thickness. Note that data shown is an excerpt of each drill hole only. Full assay results for Co, Ni, Pt, Pd, and Cr, are listed in Appendix 2. Assay results in excess of 0.20 % Co and 1.00 % Ni are bolded.
| Hole | Easting (mE) |
Northing (mN) |
Azimuth (°) |
Dip (°) |
From (m) To (m) |
Thickness (m) |
Cobalt (%) |
Nickel (%) |
|---|---|---|---|---|---|---|---|---|
| ABR0008, 58 – 78 | metres | |||||||
| ABR0008 | 304763 | 6640878 | 000 | -90 | 58.00 60.00 60.00 62.00 62.00 64.00 64.00 66.00 66.00 68.00 68.00 70.00 70.00 72.00 72.00 74.00 74.00 76.00 76.00 78.00 |
2.00 2.00 2.00 2.00 2.00 2.00 2.00 2.00 2.00 2.00 |
0.059 | 0.38 0.60 0.59 0.63 0.39 0.50 0.67 0.67 0.76 0.66 |
| 0.263 | ||||||||
| 0.229 | ||||||||
| 0.201 | ||||||||
| 0.056 | ||||||||
| 0.081 | ||||||||
| 0.174 | ||||||||
| 0.168 | ||||||||
| 0.134 | ||||||||
| 0.061 | ||||||||
| ABR0013, Surface – 14 metres | ||||||||
| ABR0013 | 304359 | 6640554 | 000 | -90 | 0.00 2.00 |
2.00 | 0.029 | 0.25 |
| 2.00 4.00 |
2.00 | 0.072 | 0.59 | |||||
| 4.00 6.00 |
2.00 | 0.250 | 0.96 | |||||
| 6.00 8.00 |
2.00 | 0.284 | 0.82 | |||||
| 8.00 10.00 |
2.00 | 0.178 | 0.73 | |||||
| 10.00 12.00 |
2.00 | 0.208 | 0.76 | |||||
| 12.00 14.00 |
2.00 | 0.108 | 0.49 | |||||
| ABR0014, Surface – 12 metres | ||||||||
| ABR0014 | 304357 | 6640475 | 000 | -90 | 0.00 2.00 2.00 4.00 4.00 6.00 6.00 8.00 8.00 10.00 10.00 12.00 |
2.00 2.00 2.00 2.00 2.00 2.00 |
0.040 | 0.17 0.83 0.96 0.84 0.86 0.71 |
| 0.222 | ||||||||
| 0.286 | ||||||||
| 0.204 | ||||||||
| 0.102 | ||||||||
| 0.083 | ||||||||
| ABR0022, 14 – 24 | metres | |||||||
| ABR0022 | 303958 | 6640564 | 000 | -90 | 14.00 16.00 |
2.00 | 0.117 | 0.60 |
| 16.00 18.00 |
2.00 | 0.369 | 0.82 | |||||
| 18.00 20.00 |
2.00 | 0.308 | 1.12 | |||||
| 20.00 22.00 |
2.00 | 0.386 | 1.14 | |||||
| 22.00 24.00 |
2.00 | 0.144 | 0.86 |
These examples show that the highest-grade cobalt mineralisation is encased within a lower-grade cobalt shell, and is usually associated with high-grade nickel mineralisation. They also show that cobalt and nickel mineralisation is continuous over broad thicknesses and, in holes ABR0013 and ABR0014, is present in the immediate subsurface.
High cobalt cutoff values illustrate deposit quality
Most lateritic cobalt deposits in Australia use cutoff values of 0.05 % to 0.08 % cobalt to model intercepts and in resource calculations. Cutoff values define the level below which data is disregarded, and is commonly defined on economic grounds. That Black Range shows continuity at a significantly higher cutoff
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Cobalt, Scandium & PGM results from Black Range
value of 0.10% cobalt underscores the high quality of the deposit. Throughout the KNP Cobalt Zone, a 0.10% cutoff is being used to define intercepts and resource models. Using this cutoff at Black Range, cobalt mineralisation is continuous over the 600 x 800 m area of the recent drill program, and extends more than 2.5 km throughout the Black Range area.
Additional metals at Black Range
Within the near-surface laterite profile, assay results show that cobalt and nickel mineralisation is associated with additional metals at Black Range including scandium , platinum and palladium , and chromium .
If they were to be considered as stand-alone deposits, the abundances of scandium, PGMs and chromium would probably be problematic. However, these metals, in particular scandium, could contribute as supplementary payable commodities to the economics of a large, bulk-tonnage cobalt-nickel open pit operation.
At Black Range, scandium, platinum, and palladium are almost always situated above the cobalt-nickel mineralisation (e.g. Figure 2). Chromium is both above and directly associated with the cobalt and nickel. Any cobalt and nickel focussed mining operation will require excavation of the scandium-platinoid envelope and of the chromium bearing material in any event. As such, it makes sense to investigate any means to monetise these additional metals at Black Range. This will be incorporated into future feasibility studies of the deposit.
Scandium mineralisation
Scandium is present throughout the project area as a near-surface sheet that is up to 32 m thick within the laterite. Values within this sub-horizontal blanket vary from 50 to 170 g/t scandium[2] . In many cases, the scandium mineralisation is exposed at surface.
Scandium intercepts at Black Range include:
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ABR0001, 18 m at 97.8 g/t scandium from surface
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ABR0004, 18 m at 70 g/t scandium from surface
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ABR0008, 26 m at 47.7 g/t scandium from 52.0 m
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ABR0015, 32 m at 83.1 g/t scandium from surface
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ABR0021, 20 m at 84 g/t scandium from 4.0 m
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ABR0022, 28 m at 64.3 g/t scandium from surface
With scandium metal presently worth US$15,000 per kg[3] (equivalent to US$15 million per tonne, or US$15 per gram) and scandium trioxide some US$1,500 to 6,000 per kg, there is the potential for substantial cost benefit to any cobalt-nickel mining operation at Black Range, even with only moderate recoveries. As such, low head grades can add significantly to the economics of a project. For example, CleanTeQ’s Syerston project[4] reports an operating head grade of 53 g/t scandium. Black Range contains abundant mineralisation exceeding these grades.
2 Scandium was assayed using the XRF technique. The concentrations present at Black Range are toward the lower limit of detectability of the technique for scandium. Whilst scandium passed all QAQC checks, it should be noted that results are likely to be less accurate than those of other metals.
3 Source: http://mineralprices.com/
4 CleanTeQ Holdings Limited, 5 October 2016, “Syerston Nickel and Cobalt Pre-Feasibilty Study Completed”, p. 14.
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Cobalt, Scandium & PGM results from Black Range
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Figure 2 – The 304760mE section (the easternmost north-south section) at Black Range, showing nickel (Ni), cobalt (Co), platinum + palladium (Pt+Pd or PGM), and scandium (Sc) distributions. Envelopes for the nickel-cobalt and for the scandium-platinum group metal mineralisation show lateral continuity.
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Cobalt, Scandium & PGM results from Black Range
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Figure 3 – The 304360mE section (the central north-south section) at Black Range, showing nickel (Ni), cobalt (Co), platinum + palladium (Pt+Pd or PGM), and scandium (Sc) distributions. Envelopes for the nickel-cobalt and for the scandium-platinum group metal mineralisation show lateral continuity.
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Cobalt, Scandium & PGM results from Black Range
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Figure 4 – The 303630mE section (the westernmost north-south section) at Black Range, showing nickel (Ni), cobalt (Co), platinum + palladium (Pt+Pd or PGM), and scandium (Sc) distributions. Envelopes for the nickel-cobalt and for the scandium-platinum group metal mineralisation show lateral continuity.
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Cobalt, Scandium & PGM results from Black Range
The Ardea exploration program marks the first recorded occurrence of scandium at Black Range. Historically, scandium was not assayed, so very little of the nature of the mineralisation is known. For example, the host mineral to the scandium within the laterite profile must be determined. The liberation of a scandium product from Black Range leachate would be dependent upon industry accepted metallurgical processes being compatible with the Co-Ni processes being assessed. This will be the subject of planned metallurgical investigations.
Scandium is an uncommon metal that is used as a strengthening agent for aluminium, chiefly in the aeronautical industry.
It should be noted that the analytical technique employed for Ardea’s cobalt-nickel laterite reports scandium at a 10g/t detection limit so that replicate assaying using a more precise analytical technique is planned.
Platinum and palladium mineralisation
Platinum and palladium are closely associated with one another at Black Range. Platinum-palladium mineralisation is typically associated with scandium but is not as continuous, and usually occurs in the lower half of the scandium-rich envelope.
Combined platinum and palladium values from the recent drill program are generally less than 1 g/t. Intercepts include:
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ABR0001, 18 m at 0.83 g/t platinum + palladium from surface
-
ABR0003, 12 m at 0.67 g/t platinum + palladium from surface
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ABR0004, 12 m at 0.92 g/t platinum + palladium from 4.0 m
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ABR0015, 16 m at 0.64 g/t platinum + palladium from surface
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ABR0021, 20 m at 0.66 g/t platinum + palladium from 4.0 m
Platinum and palladium mineralisation has been recorded historically in both laterite and fresh rock at Mt Carnage, a part of Black Range.
The precise nature of the platinum and palladium mineralisation within the laterite profile is presently unknown, and will be the subject of investigation as the PFS progresses. Means to liberate these metals will be investigated in detail during the course of the current PFS.
Chromium mineralisation
Chromium intercepts are not quoted here, but all lateritic mineralisation at Black Range is either encased within or is immediately adjacent to a thick sub-horizontal chromium envelope. This chromium-rich band is up to 50 m thick, with chromium grades of between 0.9 % and 2.5 %. This contrasts markedly with grades outside of the cobalt mineralised zones of 0.2–0.8 % Cr.
As with the other accessory metals highlighted by this drill program, the nature of the chromium in the laterite profile at Black Range is unknown and will be the subject of investigation. It is likely that residual grains of chromite from the underlying Ora Banda layered mafic intrusion have remained as resistate minerals within the profile. If this is the case, a simple separation method (e.g. gravity, magnetic) could be used to separate and commodify the chromium at Black Range.
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Cobalt, Scandium & PGM results from Black Range
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Comparison to historic drilling at Black Range.
Prior to Ardea’s recent drill program, historic drilling at Black Range comprised 184 drillholes (mostly RAB) for 7,711 m. Using the parameters for defining intercepts in Ardea’s drilling, newly calculated intercepts from these programs include:
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BKRC0135, 6 m at 0.32 % cobalt and 0.87 % nickel from 24.0 m
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BRR0071, 20 m at 0.25 % cobalt and 0.55 % nickel from 28.0 m
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BRR0074, 8 m at 0.32 % cobalt and 1.15 % nickel from 24.0 m
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BRR0079, 16 m at 0.15 % cobalt and 0.86 % nickel from 16.0 m
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BRR0080, 20 m at 0.15 % cobalt and 0.56 % nickel from 20.0 m
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BRR0081, 16 m at 0.15 % cobalt and 0.36 % nickel from 32.0 m
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BRR0096, 12 m at 0.23 % cobalt and 0.76 % nickel from 40.0 m
The historic data show that our recent drill program is consistent with earlier cobalt and nickel results at Black Range. See Appendix 3 for full listing of newly calculated cobalt and nickel intercepts from historic drill holes.
Platinum and palladium were not systematically assayed throughout historic drill programs, so there are only limited data to compare. These include:
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BRRB061, 16 m at 0.74 g/t platinum + palladium from 8.0 m
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BRRB059, 4 m at 0.9 g/t platinum + palladium from surface.
These are also comparable with data collected in the recent drill program. See Appendix 3 for full listing of newly calculated platinum and palladium intercepts from historic drill holes.
Scandium was not assayed in any previous drilling prior to Ardea’s project tenure.
A new resource for Black Range
Black Range is part of the KNP Cobalt Zone. The KNP Cobalt Zone contains 49.7 Mt at 0.12 % cobalt and 0.86 % nickel (Table 1) for a total contained cobalt metal of just under 60,000 t. With a historic resource of 20.1 Mt at 0.75 % nickel and 0.10 % cobalt (Table 1), Black Range constitutes a significant proportion of the KNP Cobalt Zone resource.
Table 2 – KNP Cobalt Zone, Resource Statement from RMRC consulting group, January 2017.
| Area | Prospect Resource category Cutoff (% Co) Size (Mt) Cobalt (%) Nickel (%) |
|---|---|
| Goongarrie | Goongarrie South Measured 0.08 3.4 0.14 1.19 Indicated 0.08 11.2 0.11 0.92 Inferred 0.08 1.4 0.11 0.76 |
| Big Four Indicated 0.08 4.5 0.11 0.89 Inferred 0.08 0.2 0.11 0.95 |
|
| Scotia Inferred 0.08 2.9 0.14 0.88 |
|
| Goongarrie subtotal 23.6 0.12 0.94 |
|
| Siberia | Black Range Inferred 0.50(Ni) 20.1 0.10 0.75 |
| Yerilla | Aubils Inferred 0.08 6.0 0.15 0.90 |
| KNP Cobalt Zone total resources 49.7 0.12 0.86 |
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Cobalt, Scandium & PGM results from Black Range
This historic resource at Black Range was based on nickel cutoffs. As the results of this recent program show (Figure 2, Figure 3, and Figure 4), cobalt and nickel distributions vary, so it is expected that the historic resource estimation methodology could be under-calling the true cobalt resource.
The Black Range resource estimate is scheduled to be upgraded in the coming months. At Goongarrie South and Big Four, the resource upgrade of the KNP Cobalt Zone based on cobalt cutoffs is nearing completion and is expected to be announced soon. Work has commenced on upgrading the cobalt resources at Goongarrie Hill and Scotia Dam (which are contiguous with Goongarrie South and Big Four). These are smaller resources that are expected to be completed quickly. Work will then commence on the upgrade of the Black Range resource, which will include all new data generated by the recent drill program.
Once re-estimated and likely Black Range head-grades defined, a program of core drilling will be done, to obtain material for metallurgical test-work.
For further information regarding Ardea, please visit www.ardearesources.com.au or contact:
Ardea Resources:
Dr Matt Painter
Managing Director, Ardea Resources Limited Tel +61 8 6500 9200
Media or Investor Inquiries:
FTI Consulting Jon Snowball Tel +61 2 8298 6100 or +61 477 946 068
Compliance Statement (JORC 2012)
A competent person’s statement for the purposes of Listing Rule 5.22 has previously been announced by the Company for:
1. Kalgoorlie Nickel Project on 21 October 2013 and 31 June 2014, October 2016, 2016 Heron Resources Annual Report and 6 January 2017;
2. KNP Cobalt Zone Study on 6 January 2017
The Company confirms that it is not aware of any new information or data that materially affects information included in previous announcements, and all material assumptions and technical parameters underpinning the estimates continue to apply and have not materially changed. All projects will be subject to new work programs following the listing of Ardea, notably drilling, metallurgy and JORC Code 2012 resource estimation as applicable.
The information in this report that relates to the Black Range Exploration Results is based on information originally compiled by current full time employees of Ardea Resources Limited. The Exploration Results and data collection processes have been reviewed, verified and reinterpreted by Mr Ian Buchhorn who is a Member of the Australasian Institute of Mining and Metallurgy and a director of Ardea Resources Limited. Mr Buchhorn has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the exploration activities undertaken 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 Buchhorn consents to the inclusion in this report of the matters based on his information in the form and context that it appears.
The exploration and industry benchmarking summaries are based on information reviewed by Dr Matthew Painter, who is a Member of the Australian Institute of Geoscientists. Dr Painter is a full-time employee and a director of Ardea Resources Limited and has sufficient experience, which is relevant to the style of 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’. Dr Painter has reviewed this press release and consents to the inclusion in this report of the information in the form and context in which it appears.
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Cobalt, Scandium & PGM results from Black Range
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CAUTIONARY NOTE REGARDING FORWARD-LOOKING INFORMATION
This news release contains forward-looking statements and forward-looking information within the meaning of applicable Australian securities laws, which are based on expectations, estimates and projections as of the date of this news release.
This forward-looking information includes, or may be based upon, without limitation, estimates, forecasts and statements as to management’s expectations with respect to, among other things, development and business plans, capital and exploration expenditures, the effect on the Company of any changes to existing legislation or policy, government regulation of mining operations, the length of time required to obtain permits, certifications and approvals, the success of exploration, development and mining activities, the geology of the Company’s properties, environmental risks, the availability of labour, the focus of the Company in the future, demand and market outlook for metals and the prices thereof, progress in development of mineral properties, the Company’s ability to raise funding privately or on a public market in the future, the Company’s future growth, results of operations, performance, and business prospects and opportunities. Wherever possible, words such as “anticipate”, “believe”, “expect”, “intend”, “may” and similar expressions have been used to identify such forwardlooking information. Forward-looking information is based on the opinions and estimates of management at the date the information is given, and on information available to management at such time. Forward-looking information involves significant risks, uncertainties, assumptions and other factors that could cause actual results, performance or achievements to differ materially from the results discussed or implied in the forward-looking information. These factors, including, but not limited to, fluctuations in currency markets, fluctuations in commodity prices, the ability of the Company to access sufficient capital on favourable terms or at all, changes in national and local government legislation, taxation, controls, regulations, political or economic developments in Australia or other countries in which the Company does business or may carry on business in the future, operational or technical difficulties in connection with exploration or development activities, employee relations, the speculative nature of mineral exploration and development, obtaining necessary licenses and permits, diminishing quantities and grades of mineral reserves, contests over title to properties, especially title to undeveloped properties, the inherent risks involved in the exploration and development of mineral properties, the uncertainties involved in interpreting drill results and other geological data, environmental hazards, industrial accidents, unusual or unexpected formations, pressures, cave-ins and flooding, limitations of insurance coverage and the possibility of project cost overruns or unanticipated costs and expenses, and should be considered carefully. Many of these uncertainties and contingencies can affect the Company’s actual results and could cause actual results to differ materially from those expressed or implied in any forward-looking statements made by, or on behalf of, the Company. Prospective investors should not place undue reliance on any forward-looking information.
Although the forward-looking information contained in this news release is based upon what management believes, or believed at the time, to be reasonable assumptions, the Company cannot assure prospective purchasers that actual results will be consistent with such forwardlooking information, as there may be other factors that cause results not to be as anticipated, estimated or intended, and neither the Company nor any other person assumes responsibility for the accuracy and completeness of any such forward-looking information. The Company does not undertake, and assumes no obligation, to update or revise any such forward-looking statements or forward-looking information contained herein to reflect new events or circumstances, except as may be required by law.
No stock exchange, regulation services provider, securities commission or other regulatory authority has approved or disapproved the information contained in this news release.
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Cobalt, Scandium & PGM results from Black Range
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Appendix 1 – Collar location data, Black Range
New drill holes by Ardea Resources at Black Range
| Drill hole | Type | Depth (m) |
Date completed |
Grid |
Easting (mE) |
Northing (mN) |
RL (mASL) |
Dip (°) |
Azimuth (°) |
|---|---|---|---|---|---|---|---|---|---|
| ABR0001 | RC | 73 | 06-Apr-17 | MGA94_51 | 304750.44 | 6640322.98 | 440.32 | -90 | 000 |
| ABR0002 | RC | 79 | 06-Apr-17 | MGA94_51 | 304759.37 | 6640399.68 | 440.34 | -90 | 000 |
| ABR0003 | RC | 80 | 07-Apr-17 | MGA94_51 | 304761.72 | 6640472.35 | 437.38 | -90 | 000 |
| ABR0004 | RC | 80 | 07-Apr-17 | MGA94_51 | 304762.08 | 6640557.29 | 438.91 | -90 | 000 |
| ABR0005 | RC | 80 | 08-Apr-17 | MGA94_51 | 304763.49 | 6640632.52 | 436.09 | -90 | 000 |
| ABR0006 | RC | 80 | 08-Apr-17 | MGA94_51 | 304758.59 | 6640719.21 | 431.80 | -90 | 000 |
| ABR0007 | RC | 110 | 09-Apr-17 | MGA94_51 | 304755.97 | 6640796.23 | 431.07 | -90 | 000 |
| ABR0008 | RC | 120 | 09-Apr-17 | MGA94_51 | 304758.42 | 6640877.83 | 429.83 | -90 | 000 |
| ABR0009 | RC | 91 | 10-Apr-17 | MGA94_51 | 304358.69 | 6640877.75 | 432.60 | -90 | 000 |
| ABR0010 | RC | 80 | 10-Apr-17 | MGA94_51 | 304363.07 | 6640789.59 | 433.09 | -90 | 000 |
| ABR0011 | RC | 73 | 10-Apr-17 | MGA94_51 | 304358.13 | 6640719.77 | 436.20 | -90 | 000 |
| ABR0012 | RC | 73 | 10-Apr-17 | MGA94_51 | 304347.76 | 6640642.69 | 435.78 | -90 | 000 |
| ABR0013 | RC | 73 | 11-Apr-17 | MGA94_51 | 304354.56 | 6640555.11 | 437.24 | -90 | 000 |
| ABR0014 | RC | 61 | 11-Apr-17 | MGA94_51 | 304354.85 | 6640478.58 | 438.08 | -90 | 000 |
| ABR0015 | RC | 67 | 11-Apr-17 | MGA94_51 | 304360.99 | 6640398.66 | 438.85 | -90 | 000 |
| ABR0016 | RC | 55 | 11-Apr-17 | MGA94_51 | 304357.33 | 6640322.40 | 440.89 | -90 | 000 |
| ABR0017 | RC | 41 | 11-Apr-17 | MGA94_51 | 304357.69 | 6640248.27 | 443.15 | -90 | 000 |
| ABR0018 | RC | 41 | 12-Apr-17 | MGA94_51 | 303963.32 | 6640240.77 | 445.57 | -90 | 000 |
| ABR0019 | RC | 54 | 12-Apr-17 | MGA94_51 | 303968.07 | 6640319.48 | 443.08 | -90 | 000 |
| ABR0020 | RC | 55 | 12-Apr-17 | MGA94_51 | 303959.49 | 6640401.21 | 444.90 | -90 | 000 |
| ABR0021 | RC | 73 | 12-Apr-17 | MGA94_51 | 303957.29 | 6640481.29 | 444.26 | -90 | 000 |
| ABR0022 | RC | 73 | 12-Apr-17 | MGA94_51 | 303959.79 | 6640564.29 | 442.73 | -90 | 000 |
| ABR0023 | RC | 79 | 13-Apr-17 | MGA94_51 | 303961.37 | 6640639.40 | 440.77 | -90 | 000 |
| ABR0024 | RC | 74 | 13-Apr-17 | MGA94_51 | 303966.81 | 6640719.59 | 436.15 | -90 | 000 |
| ABR0025 | RC | 73 | 13-Apr-17 | MGA94_51 | 303966.99 | 6640790.96 | 433.71 | -90 | 000 |
| ABR0026 | RC | 73 | 13-Apr-17 | MGA94_51 | 303957.42 | 6640874.40 | 432.00 | -90 | 000 |
| ABR0027 | RC | 85 | 14-Apr-17 | MGA94_51 | 303962.47 | 6640952.19 | 430.75 | -90 | 000 |
Historic drill holes at Black Range
| Drill hole | Type | Depth (m) |
Date completed |
Grid |
Easting (mE) |
Northing (mN) |
RL (mASL) |
Dip (°) |
Azimuth (°) |
|---|---|---|---|---|---|---|---|---|---|
| BKRC0072 | RC | 18 | 29-Oct-00 | MGA94_51 | 302527.65 | 6640642.08 | 437.67 | -90 | 000 |
| BKRC0073 | RC | 16 | 29-Oct-00 | MGA94_51 | 302539.76 | 6640553.95 | 439.38 | -90 | 000 |
| BKRC0074 | RC | 22 | 29-Oct-00 | MGA94_51 | 302937.04 | 6640646.38 | 439.46 | -90 | 000 |
| BKRC0075 | RC | 60 | 29-Oct-00 | MGA94_51 | 302928.63 | 6640753.94 | 434.88 | -90 | 000 |
| BKRC0076 | RC | 42 | 29-Oct-00 | MGA94_51 | 302931.77 | 6640845.35 | 431.49 | -90 | 000 |
| BKRC0077 | RC | 60 | 29-Oct-00 | MGA94_51 | 302931.76 | 6640936.52 | 429.24 | -90 | 000 |
| BKRC0078 | RC | 54 | 29-Oct-00 | MGA94_51 | 302930.70 | 6641048.85 | 428.96 | -90 | 000 |
| BKRC0079 | RC | 12 | 29-Oct-00 | MGA94_51 | 303333.16 | 6640555.18 | 436.66 | -90 | 000 |
| BKRC0080 | RC | 12 | 29-Oct-00 | MGA94_51 | 303331.67 | 6640661.98 | 435.24 | -90 | 000 |
| BKRC0081 | RC | 18 | 29-Oct-00 | MGA94_51 | 303325.99 | 6640752.31 | 434.70 | -90 | 000 |
| BKRC0082 | RC | 30 | 29-Oct-00 | MGA94_51 | 303336.12 | 6640848.66 | 432.70 | -90 | 000 |
| BKRC0083 | RC | 30 | 29-Oct-00 | MGA94_51 | 303327.86 | 6640939.17 | 431.55 | -90 | 000 |
| BKRC0084 | RC | 36 | 30-Oct-00 | MGA94_51 | 304138.90 | 6640950.81 | 431.27 | -90 | 000 |
| BKRC0085 | RC | 24 | 30-Oct-00 | MGA94_51 | 304135.62 | 6640848.60 | 432.88 | -90 | 000 |
| BKRC0086 | RC | 28 | 30-Oct-00 | MGA94_51 | 304135.10 | 6640756.02 | 436.50 | -90 | 000 |
| BKRC0087 | RC | 24 | 30-Oct-00 | MGA94_51 | 304136.96 | 6640659.67 | 439.62 | -90 | 000 |
| BKRC0088 | RC | 24 | 30-Oct-00 | MGA94_51 | 304138.01 | 6640550.83 | 439.97 | -90 | 000 |
| BKRC0089 | RC | 32 | 30-Oct-00 | MGA94_51 | 304139.40 | 6640457.42 | 442.94 | -90 | 000 |
| BKRC0090 | RC | 24 | 30-Oct-00 | MGA94_51 | 304144.07 | 6640358.41 | 440.81 | -90 | 000 |
| BKRC0091 | RC | 30 | 30-Oct-00 | MGA94_51 | 304944.35 | 6640356.65 | 440.07 | -90 | 000 |
| BKRC0092 | RC | 30 | 30-Oct-00 | MGA94_51 | 304933.47 | 6640271.05 | 440.40 | -90 | 000 |
13
Cobalt, Scandium & PGM results from Black Range
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
| Drill hole | Type | Depth (m) |
Date completed |
Grid |
Easting (mE) |
Northing (mN) |
RL (mASL) |
Dip (°) |
Azimuth (°) |
|---|---|---|---|---|---|---|---|---|---|
| BKRC0093 | RC | 24 | 30-Oct-00 | MGA94_51 | 304934.99 | 6640167.53 | 436.64 | -90 | 000 |
| BKRC0094 | RC | 24 | 30-Oct-00 | MGA94_51 | 304938.24 | 6640070.31 | 435.15 | -90 | 000 |
| BKRC0095 | RC | 48 | 30-Oct-00 | MGA94_51 | 304936.10 | 6640466.23 | 438.41 | -90 | 000 |
| BKRC0096 | RC | 60 | 31-Oct-00 | MGA94_51 | 305733.42 | 6640459.29 | 429.22 | -90 | 000 |
| BKRC0097 | RC | 54 | 31-Oct-00 | MGA94_51 | 305734.49 | 6640357.48 | 426.63 | -90 | 000 |
| BKRC0098 | RC | 18 | 31-Oct-00 | MGA94_51 | 305736.30 | 6640272.22 | 427.01 | -90 | 000 |
| BKRC0099 | RC | 6 | 31-Oct-00 | MGA94_51 | 305743.22 | 6640072.01 | 429.70 | -90 | 000 |
| BKRC0116 | RC | 66 | 31-Oct-00 | MGA94_51 | 306530.32 | 6639578.77 | 419.51 | -90 | 000 |
| BKRC0117 | RC | 72 | 31-Oct-00 | MGA94_51 | 306536.44 | 6639365.65 | 419.64 | -90 | 000 |
| BKRC0118 | RC | 72 | 01-Nov-00 | MGA94_51 | 302927.75 | 6641165.36 | 427.99 | -90 | 000 |
| BKRC0119 | RC | 12 | 01-Nov-00 | MGA94_51 | 302930.37 | 6640555.88 | 444.41 | -90 | 000 |
| BKRC0120 | RC | 48 | 01-Nov-00 | MGA94_51 | 302935.62 | 6640453.38 | 448.27 | -90 | 000 |
| BKRC0121 | RC | 18 | 01-Nov-00 | MGA94_51 | 302936.19 | 6640342.39 | 443.58 | -90 | 000 |
| BKRC0122 | RC | 6 | 01-Nov-00 | MGA94_51 | 302937.08 | 6640156.55 | 441.69 | -90 | 000 |
| BKRC0123 | RC | 42 | 04-Dec-00 | MGA94_51 | 306136.07 | 6640355.03 | 422.60 | -90 | 000 |
| BKRC0124 | RC | 36 | 04-Dec-00 | MGA94_51 | 305335.47 | 6640456.93 | 428.95 | -90 | 000 |
| BKRC0125 | RC | 18 | 04-Dec-00 | MGA94_51 | 305340.86 | 6640350.07 | 429.81 | -90 | 000 |
| BKRC0126 | RC | 36 | 04-Dec-00 | MGA94_51 | 305333.91 | 6640269.24 | 430.86 | -90 | 000 |
| BKRC0127 | RC | 18 | 04-Dec-00 | MGA94_51 | 305334.80 | 6640177.29 | 432.07 | -90 | 000 |
| BKRC0128 | RC | 48 | 04-Dec-00 | MGA94_51 | 304936.55 | 6640566.16 | 435.32 | -90 | 000 |
| BKRC0129 | RC | 31 | 04-Dec-00 | MGA94_51 | 304940.85 | 6640659.25 | 432.76 | -90 | 000 |
| BKRC0130 | RC | 24 | 05-Dec-00 | MGA94_51 | 304538.02 | 6640270.77 | 440.65 | -90 | 000 |
| BKRC0131 | RC | 36 | 05-Dec-00 | MGA94_51 | 304534.52 | 6640357.56 | 439.66 | -90 | 000 |
| BKRC0132 | RC | 30 | 05-Dec-00 | MGA94_51 | 304535.41 | 6640452.82 | 437.47 | -90 | 000 |
| BKRC0133 | RC | 18 | 05-Dec-00 | MGA94_51 | 304534.06 | 6640552.62 | 436.74 | -90 | 000 |
| BKRC0134 | RC | 54 | 05-Dec-00 | MGA94_51 | 304536.83 | 6640653.99 | 436.94 | -90 | 000 |
| BKRC0135 | RC | 84 | 05-Dec-00 | MGA94_51 | 304536.21 | 6640755.00 | 432.28 | -90 | 000 |
| BKRC0136 | RC | 84 | 06-Dec-00 | MGA94_51 | 304537.69 | 6640852.99 | 430.21 | -90 | 000 |
| BKRC0137 | RC | 18 | 06-Dec-00 | MGA94_51 | 303731.47 | 6640356.34 | 443.10 | -90 | 000 |
| BKRC0138 | RC | 12 | 06-Dec-00 | MGA94_51 | 303733.24 | 6640452.70 | 444.85 | -90 | 000 |
| BKRC0139 | RC | 18 | 06-Dec-00 | MGA94_51 | 303736.00 | 6640551.75 | 442.30 | -90 | 000 |
| BKRC0140 | RC | 24 | 06-Dec-00 | MGA94_51 | 303733.41 | 6640653.29 | 438.71 | -90 | 000 |
| BKRC0141 | RC | 6 | 06-Dec-00 | MGA94_51 | 303337.54 | 6640259.66 | 442.51 | -90 | 000 |
| BKRC0142 | RC | 18 | 06-Dec-00 | MGA94_51 | 303333.88 | 6640362.15 | 439.57 | -90 | 000 |
| BKRC0143 | RC | 18 | 06-Dec-00 | MGA94_51 | 302534.96 | 6640447.67 | 435.78 | -90 | 000 |
| BKRC0144 | RC | 66 | 06-Dec-00 | MGA94_51 | 303740.18 | 6640843.96 | 433.65 | -90 | 000 |
| BKRC0145 | RC | 84 | 07-Dec-00 | MGA94_51 | 303734.91 | 6640941.92 | 432.16 | -90 | 000 |
| BKRC0146 | RC | 60 | 07-Dec-00 | MGA94_51 | 303736.98 | 6640744.62 | 435.30 | -90 | 000 |
| BKRC0147 | RC | 72 | 07-Dec-00 | MGA94_51 | 303727.00 | 6641054.62 | 431.04 | -90 | 000 |
| BKRC0148 | RC | 30 | 07-Dec-00 | MGA94_51 | 303334.09 | 6640465.57 | 437.79 | -90 | 000 |
| BRDD001 | DD |
246.3 | 06-Dec-11 | MGA94_51 | 305920.00 | 6640380.00 | -65 | 035 |
|
| BRR0049 | RAB | 50 |
18-Oct-97 | MGA94_51 | 306262.72 | 6639991.10 | 500.00 | -90 | 000 |
| BRR0050 | RAB | 44 |
19-Oct-97 | MGA94_51 | 306271.93 | 6640014.49 | 500.00 | -90 | 000 |
| BRR0051 | RAB | 44 |
19-Oct-97 | MGA94_51 | 306280.04 | 6640035.07 | 500.00 | -90 | 000 |
| BRR0052 | RAB | 33 |
19-Oct-97 | MGA94_51 | 306288.15 | 6640055.66 | 500.00 | -90 | 000 |
| BRR0053 | RAB | 36 |
19-Oct-97 | MGA94_51 | 306294.04 | 6640070.63 | 500.00 | -90 | 000 |
| BRR0054 | RAB | 15 |
19-Oct-97 | MGA94_51 | 306189.01 | 6639803.97 | 500.00 | -90 | 000 |
| BRR0055 | RAB | 59 |
19-Oct-97 | MGA94_51 | 306191.22 | 6639809.58 | 500.00 | -90 | 000 |
| BRR0056 | RAB | 56 |
19-Oct-97 | MGA94_51 | 306201.91 | 6639836.72 | 500.00 | -90 | 000 |
| BRR0057 | RAB | 53 |
20-Oct-97 | MGA94_51 | 306210.38 | 6639858.24 | 500.00 | -90 | 000 |
| BRR0058 | RAB | 47 |
20-Oct-97 | MGA94_51 | 306219.96 | 6639882.56 | 500.00 | -90 | 000 |
| BRR0059 | RAB | 32 |
20-Oct-97 | MGA94_51 | 305366.76 | 6639911.67 | 500.00 | -90 | 000 |
| BRR0060 | RAB | 18 |
20-Oct-97 | MGA94_51 | 305372.66 | 6639926.64 | 500.00 | -90 | 000 |
| BRR0061 | RAB | 20 |
20-Oct-97 | MGA94_51 | 305375.98 | 6639935.06 | 500.00 | -90 | 000 |
| BRR0062 | RAB | 20 |
20-Oct-97 | MGA94_51 | 305379.66 | 6639944.42 | 500.00 | -90 | 000 |
| BRR0063 | RAB | 34 |
20-Oct-97 | MGA94_51 | 305384.45 | 6639956.58 | 500.00 | -90 | 000 |
| BRR0064 | RAB | 32 |
20-Oct-97 | MGA94_51 | 305390.72 | 6639972.49 | 500.00 | -90 | 000 |
| BRR0065 | RAB | 38 |
20-Oct-97 | MGA94_51 | 305396.62 | 6639987.46 | 500.00 | -90 | 000 |
| BRR0066 | RAB | 16 |
10-Oct-97 | MGA94_51 | 304135.86 | 6640313.26 | 500.00 | -90 | 000 |
| BRR0067 | RAB | 21 |
20-Oct-97 | MGA94_51 | 304135.84 | 6640321.31 | 500.00 | -90 | 000 |
| BRR0068 | RAB | 24 |
20-Oct-97 | MGA94_51 | 304135.83 | 6640331.38 | 500.00 | -90 | 000 |
| BRR0069 | RAB | 24 |
20-Oct-97 | MGA94_51 | 304135.81 | 6640343.46 | 500.00 | -90 | 000 |
| BRR0070 | RAB | 57 |
20-Oct-97 | MGA94_51 | 304135.79 | 6640355.54 | 500.00 | -90 | 000 |
| BRR0071 | RAB | 69 |
20-Oct-97 | MGA94_51 | 304135.73 | 6640393.79 | 500.00 | -90 | 000 |
| BRR0072 | RAB | 68 |
21-Oct-97 | MGA94_51 | 304135.69 | 6640417.96 | 500.00 | -90 | 000 |
| BRR0073 | RAB | 67 |
21-Oct-97 | MGA94_51 | 304135.64 | 6640452.18 | 500.00 | -90 | 000 |
14
Cobalt, Scandium & PGM results from Black Range
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
| Drill hole | Type | Depth (m) |
Date completed |
Grid |
Easting (mE) |
Northing (mN) |
RL (mASL) |
Dip (°) |
Azimuth (°) |
|---|---|---|---|---|---|---|---|---|---|
| BRR0074 | RAB | 59 |
21-Oct-97 | MGA94_51 | 304034.83 | 6640539.61 | 500.00 | -90 | 000 |
| BRR0075 | RAB | 57 |
21-Oct-97 | MGA94_51 | 304034.79 | 6640568.80 | 500.00 | -90 | 000 |
| BRR0076 | RAB | 50 |
21-Oct-97 | MGA94_51 | 304034.74 | 6640596.99 | 500.00 | -90 | 000 |
| BRR0077 | RAB | 31 |
21-Oct-97 | MGA94_51 | 304034.70 | 6640622.16 | 500.00 | -90 | 000 |
| BRR0078 | RAB | 66 |
21-Oct-97 | MGA94_51 | 303934.20 | 6640514.28 | 500.00 | -90 | 000 |
| BRR0079 | RAB | 64 |
21-Oct-97 | MGA94_51 | 303934.15 | 6640547.50 | 500.00 | -90 | 000 |
| BRR0080 | RAB | 56 |
21-Oct-97 | MGA94_51 | 303934.10 | 6640579.72 | 500.00 | -90 | 000 |
| BRR0081 | RAB | 54 |
21-Oct-97 | MGA94_51 | 303934.06 | 6640607.90 | 500.00 | -90 | 000 |
| BRR0082 | RAB | 29 |
22-Oct-97 | MGA94_51 | 303495.45 | 6640648.76 | 500.00 | -90 | 000 |
| BRR0083 | RAB | 13 |
22-Oct-97 | MGA94_51 | 303500.98 | 6640662.80 | 500.00 | -90 | 000 |
| BRR0084 | RAB | 14 |
22-Oct-97 | MGA94_51 | 303503.19 | 6640668.41 | 500.00 | -90 | 000 |
| BRR0085 | RAB | 12 |
22-Oct-97 | MGA94_51 | 303505.77 | 6640674.96 | 500.00 | -90 | 000 |
| BRR0086 | RAB | 30 |
22-Oct-97 | MGA94_51 | 303507.98 | 6640680.57 | 500.00 | -90 | 000 |
| BRR0087 | RAB | 18 |
22-Oct-97 | MGA94_51 | 303513.51 | 6640694.61 | 500.00 | -90 | 000 |
| BRR0088 | RAB | 27 |
22-Oct-97 | MGA94_51 | 303520.88 | 6640713.32 | 500.00 | -90 | 000 |
| BRR0089 | RAB | 23 |
22-Oct-97 | MGA94_51 | 303084.33 | 6640702.61 | 500.00 | -90 | 000 |
| BRR0090 | RAB | 25 |
22-Oct-97 | MGA94_51 | 303088.38 | 6640712.91 | 500.00 | -90 | 000 |
| BRR0091 | RAB | 22 |
22-Oct-97 | MGA94_51 | 303092.80 | 6640724.13 | 500.00 | -90 | 000 |
| BRR0092 | RAB | 22 |
22-Oct-97 | MGA94_51 | 303096.86 | 6640734.43 | 500.00 | -90 | 000 |
| BRR0093 | RAB | 25 |
23-Oct-97 | MGA94_51 | 303100.91 | 6640744.72 | 500.00 | -90 | 000 |
| BRR0094 | RAB | 25 |
23-Oct-97 | MGA94_51 | 303111.97 | 6640772.79 | 500.00 | -90 | 000 |
| BRR0095 | RAB | 32 |
23-Oct-97 | MGA94_51 | 303121.18 | 6640796.18 | 500.00 | -90 | 000 |
| BRR0096 | RAB | 66 |
23-Oct-97 | MGA94_51 | 302973.76 | 6640421.92 | 500.00 | -90 | 000 |
| BRR0097 | RAB | 11 |
23-Oct-97 | MGA94_51 | 302985.93 | 6640452.79 | 500.00 | -90 | 000 |
| BRR0098 | RAB | 57 |
23-Oct-97 | MGA94_51 | 302989.61 | 6640462.15 | 500.00 | -90 | 000 |
| BRRB001 | RAB | 7 |
10-Dec-11 | MGA94_51 | 300480.00 | 6637750.00 | -90 | 000 |
|
| BRRB002 | RAB | 8 |
10-Dec-11 | MGA94_51 | 300400.00 | 6637750.00 | -90 | 000 |
|
| BRRB003 | RAB | 27 |
10-Dec-11 | MGA94_51 | 300320.00 | 6637750.00 | -90 | 000 |
|
| BRRB004 | RAB | 66 |
10-Dec-11 | MGA94_51 | 300240.00 | 6637750.00 | -90 | 000 |
|
| BRRB005 | RAB | 45 |
10-Dec-11 | MGA94_51 | 300640.00 | 6638560.00 | -90 | 000 |
|
| BRRB006 | RAB | 48 |
10-Dec-11 | MGA94_51 | 300800.00 | 6638560.00 | -90 | 000 |
|
| BRRB007 | RAB | 43 |
10-Dec-11 | MGA94_51 | 300960.00 | 6638560.00 | -90 | 000 |
|
| BRRB008 | RAB | 15 |
10-Dec-11 | MGA94_51 | 301040.00 | 6638560.00 | -90 | 000 |
|
| BRRB009 | RAB | 24 |
10-Dec-11 | MGA94_51 | 300120.00 | 6638560.00 | -90 | 000 |
|
| BRRB010 | RAB | 17 |
10-Dec-11 | MGA94_51 | 301200.00 | 6638560.00 | -90 | 000 |
|
| BRRB011 | RAB | 21 |
11-Dec-11 | MGA94_51 | 301360.00 | 6638560.00 | -90 | 000 |
|
| BRRB012 | RAB | 44 |
11-Dec-11 | MGA94_51 | 301520.00 | 6638720.00 | -90 | 000 |
|
| BRRB013 | RAB | 10 |
11-Dec-11 | MGA94_51 | 301360.00 | 6638720.00 | -90 | 000 |
|
| BRRB014 | RAB | 6 |
11-Dec-11 | MGA94_51 | 301280.00 | 6638720.00 | -90 | 000 |
|
| BRRB015 | RAB | 39 |
11-Dec-11 | MGA94_51 | 301200.00 | 6638720.00 | -90 | 000 |
|
| BRRB016 | RAB | 36 |
11-Dec-11 | MGA94_51 | 301120.00 | 6638720.00 | -90 | 000 |
|
| BRRB017 | RAB | 29 |
11-Dec-11 | MGA94_51 | 300960.00 | 6638720.00 | -90 | 000 |
|
| BRRB018 | RAB | 44 |
11-Dec-11 | MGA94_51 | 300800.00 | 6638720.00 | -90 | 000 |
|
| BRRB019 | RAB | 27 |
11-Dec-11 | MGA94_51 | 301040.00 | 6638880.00 | -90 | 000 |
|
| BRRB020 | RAB | 38 |
11-Dec-11 | MGA94_51 | 301200.00 | 6638880.00 | -90 | 000 |
|
| BRRB021 | RAB | 45 |
11-Dec-11 | MGA94_51 | 301289.00 | 6638875.00 | -90 | 000 |
|
| BRRB022 | RAB | 46 |
11-Dec-11 | MGA94_51 | 301360.00 | 6638880.00 | -90 | 000 |
|
| BRRB023 | RAB | 50 |
11-Dec-11 | MGA94_51 | 301440.00 | 6638880.00 | -90 | 000 |
|
| BRRB024 | RAB | 35 |
11-Dec-11 | MGA94_51 | 301520.00 | 6638880.00 | -90 | 000 |
|
| BRRB025 | RAB | 30 |
11-Dec-11 | MGA94_51 | 301700.00 | 6638880.00 | -90 | 000 |
|
| BRRB026 | RAB | 46 |
11-Dec-11 | MGA94_51 | 301760.00 | 6639040.00 | -90 | 000 |
|
| BRRB027 | RAB | 47 |
11-Dec-11 | MGA94_51 | 301600.00 | 6639040.00 | -90 | 000 |
|
| BRRB028 | RAB | 48 |
11-Dec-11 | MGA94_51 | 301520.00 | 6639040.00 | -90 | 000 |
|
| BRRB029 | RAB | 44 |
11-Dec-11 | MGA94_51 | 301440.00 | 6639040.00 | -90 | 000 |
|
| BRRB030 | RAB | 9 |
11-Dec-11 | MGA94_51 | 301280.00 | 6639040.00 | -90 | 000 |
|
| BRRB031 | RAB | 42 |
11-Dec-11 | MGA94_51 | 301120.00 | 6639040.00 | -90 | 000 |
|
| BRRB032 | RAB | 29 |
11-Dec-11 | MGA94_51 | 300640.00 | 6638960.00 | -90 | 000 |
|
| BRRB033 | RAB | 16 |
11-Dec-11 | MGA94_51 | 300480.00 | 6638960.00 | -90 | 000 |
|
| BRRB034 | RAB | 10 |
11-Dec-11 | MGA94_51 | 300400.00 | 6638960.00 | -90 | 000 |
|
| BRRB035 | RAB | 10 |
11-Dec-11 | MGA94_51 | 300320.00 | 6638960.00 | -90 | 000 |
|
| BRRB036 | RAB | 10 |
11-Dec-11 | MGA94_51 | 300160.00 | 6638960.00 | -90 | 000 |
|
| BRRB037 | RAB | 18 |
12-Dec-11 | MGA94_51 | 300640.00 | 6641680.00 | -90 | 000 |
|
| BRRB038 | RAB | 22 |
12-Dec-11 | MGA94_51 | 300800.00 | 6641680.00 | -90 | 000 |
|
| BRRB039 | RAB | 12 |
12-Dec-11 | MGA94_51 | 301040.00 | 6641680.00 | -90 | 000 |
|
| BRRB040 | RAB | 8 |
12-Dec-11 | MGA94_51 | 300720.00 | 6641360.00 | -90 | 000 |
|
| BRRB041 | RAB | 11 |
12-Dec-11 | MGA94_51 | 300240.00 | 6640320.00 | -90 | 000 |
15
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Cobalt, Scandium & PGM results from Black Range
| Drill hole | Type | Depth (m) |
Date completed |
Grid |
Easting (mE) |
Northing (mN) |
RL (mASL) |
Dip (°) |
Azimuth (°) |
|---|---|---|---|---|---|---|---|---|---|
| BRRB042 | RAB | 21 |
12-Dec-11 | MGA94_51 | 301240.00 | 6639600.00 | -90 | 000 |
|
| BRRB043 | RAB | 18 |
12-Dec-11 | MGA94_51 | 301320.00 | 6639600.00 | -90 | 000 |
|
| BRRB044 | RAB | 15 |
12-Dec-11 | MGA94_51 | 301400.00 | 6639600.00 | -90 | 000 |
|
| BRRB045 | RAB | 12 |
12-Dec-11 | MGA94_51 | 301480.00 | 6639600.00 | -90 | 000 |
|
| BRRB046 | RAB | 36 |
12-Dec-11 | MGA94_51 | 301680.00 | 6639840.00 | -90 | 000 |
|
| BRRB047 | RAB | 15 |
12-Dec-11 | MGA94_51 | 301840.00 | 6639840.00 | -90 | 000 |
|
| BRRB048 | RAB | 15 |
12-Dec-11 | MGA94_51 | 302000.00 | 6639840.00 | -90 | 000 |
|
| BRRB049 | RAB | 30 |
12-Dec-11 | MGA94_51 | 302160.00 | 6639840.00 | -90 | 000 |
|
| BRRB050 | RAB | 15 |
12-Dec-11 | MGA94_51 | 302240.00 | 6639920.00 | -90 | 000 |
|
| BRRB051 | RAB | 6 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640080.00 | -90 | 000 |
|
| BRRB052 | RAB | 15 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640160.00 | -90 | 000 |
|
| BRRB053 | RAB | 9 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640240.00 | -90 | 000 |
|
| BRRB054 | RAB | 6 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640320.00 | -90 | 000 |
|
| BRRB055 | RAB | 9 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640400.00 | -90 | 000 |
|
| BRRB056 | RAB | 9 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640560.00 | -90 | 000 |
|
| BRRB057 | RAB | 28 |
12-Dec-11 | MGA94_51 | 302240.00 | 6640720.00 | -90 | 000 |
|
| BRRB058 | RAB | 15 |
12-Dec-11 | MGA94_51 | 304960.00 | 6640560.00 | -90 | 000 |
|
| BRRB059 | RAB | 15 |
13-Dec-11 | MGA94_51 | 304960.00 | 6640400.00 | -90 | 000 |
|
| BRRB060 | RAB | 42 |
13-Dec-11 | MGA94_51 | 304960.00 | 6640320.00 | -90 | 000 |
|
| BRRB061 | RAB | 30 |
13-Dec-11 | MGA94_51 | 304960.00 | 6640240.00 | -90 | 000 |
|
| BRRB062 | RAB | 33 |
13-Dec-11 | MGA94_51 | 304960.00 | 6640160.00 | -90 | 000 |
|
| BRRB063 | RAB | 9 |
13-Dec-11 | MGA94_51 | 304960.00 | 6640000.00 | -90 | 000 |
|
| BRRB064 | RAB | 14 |
13-Dec-11 | MGA94_51 | 304960.00 | 6639840.00 | -90 | 000 |
|
| BRRB065 | AC | 87 | 13-Dec-11 | MGA94_51 | 300320.00 | 6639840.00 | -90 | 000 |
|
| BRRB066 | AC | 69 | 13-Dec-11 | MGA94_51 | 300160.00 | 6639840.00 | -90 | 000 |
|
| BRRB067 | AC | 76 | 13-Dec-11 | MGA94_51 | 300480.00 | 6639840.00 | -90 | 000 |
|
| BRRB068 | AC | 66 | 13-Dec-11 | MGA94_51 | 300640.00 | 6639840.00 | -90 | 000 |
|
| BRRB069 | AC | 72 | 13-Dec-11 | MGA94_51 | 300800.00 | 6639840.00 | -90 | 000 |
|
| BRRB070 | AC | 42 | 13-Dec-11 | MGA94_51 | 300160.00 | 6640160.00 | -90 | 000 |
|
| BRRB071 | AC | 69 | 13-Dec-11 | MGA94_51 | 300320.00 | 6640160.00 | -90 | 000 |
|
| BRRB072 | AC | 90 | 02-Feb-12 | MGA94_51 | 300480.00 | 6640160.00 | -90 | 000 |
|
| BRRB073 | AC | 74 | 02-Feb-12 | MGA94_51 | 300560.00 | 6640160.00 | -90 | 000 |
|
| BRRB074 | AC | 70 | 02-Feb-12 | MGA94_51 | 300640.00 | 6640160.00 | -90 | 000 |
|
| BRRB075 | AC | 75 | 02-Feb-12 | MGA94_51 | 300720.00 | 6640160.00 | -90 | 000 |
|
| BRRB076 | AC | 75 | 03-Feb-12 | MGA94_51 | 300880.00 | 6640160.00 | -90 | 000 |
|
| BRRB077 | AC | 84 | 03-Feb-12 | MGA94_51 | 300880.00 | 6640000.00 | -90 | 000 |
|
| BRRB078 | AC | 102 | 03-Feb-12 | MGA94_51 | 300720.00 | 6640000.00 | -90 | 000 |
|
| BRRB079 | AC | 78 | 03-Feb-12 | MGA94_51 | 300560.00 | 6640000.00 | -90 | 000 |
|
| BRRB080 | AC | 81 | 03-Feb-12 | MGA94_51 | 300480.00 | 6640000.00 | -90 | 000 |
|
| BRRB081 | AC | 83 | 03-Feb-12 | MGA94_51 | 300320.00 | 6640000.00 | -90 | 000 |
|
| BRRB082 | AC | 69 | 03-Feb-12 | MGA94_51 | 300240.00 | 6640000.00 | -90 | 000 |
|
| BRRB083 | AC | 66 | 04-Feb-12 | MGA94_51 | 300160.00 | 6640000.00 | -90 | 000 |
|
| BRRB084 | AC | 63 | 04-Feb-12 | MGA94_51 | 300080.00 | 6639840.00 | -90 | 000 |
|
| BRRB085 | AC | 68 | 04-Feb-12 | MGA94_51 | 300240.00 | 6639840.00 | -90 | 000 |
|
| BRRB086 | AC | 60 | 04-Feb-12 | MGA94_51 | 300240.00 | 6640320.00 | -90 | 000 |
|
| BRRB087 | AC | 87 | 04-Feb-12 | MGA94_51 | 300400.00 | 6640320.00 | -90 | 000 |
|
| BRRB088 | AC | 77 | 04-Feb-12 | MGA94_51 | 300560.00 | 6640320.00 | -90 | 000 |
|
| BRRB089 | AC | 78 | 04-Feb-12 | MGA94_51 | 300720.00 | 6640320.00 | -90 | 000 |
|
| BRRB090 | AC | 96 | 04-Feb-12 | MGA94_51 | 300880.00 | 6640320.00 | -90 | 000 |
|
| BRRB091 | AC | 81 | 05-Feb-12 | MGA94_51 | 300640.00 | 6641680.00 | -90 | 000 |
|
| BRRB092 | AC | 93 | 05-Feb-12 | MGA94_51 | 300800.00 | 6641680.00 | -90 | 000 |
|
| BRRB093 | AC | 90 | 05-Feb-12 | MGA94_51 | 300960.00 | 6641680.00 | -90 | 000 |
|
| BRRB094 | AC | 78 | 05-Feb-12 | MGA94_51 | 301120.00 | 6641680.00 | -90 | 000 |
|
| BRRB095 | AC | 84 | 05-Feb-12 | MGA94_51 | 301280.00 | 6641680.00 | -90 | 000 |
|
| BRRB096 | AC | 82 | 06-Feb-12 | MGA94_51 | 300720.00 | 6641360.00 | -90 | 000 |
|
| BRRB097 | AC | 78 | 06-Feb-12 | MGA94_51 | 300880.00 | 6641360.00 | -90 | 000 |
|
| BRRB098 | AC | 66 | 06-Feb-12 | MGA94_51 | 301040.00 | 6641360.00 | -90 | 000 |
|
| BRRB099 | AC | 63 | 06-Feb-12 | MGA94_51 | 301200.00 | 6641360.00 | -90 | 000 |
|
| BRRB100 | AC | 70 | 06-Feb-12 | MGA94_51 | 301360.00 | 6641360.00 | -90 | 000 |
16
Cobalt, Scandium & PGM results from Black Range
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Appendix 2 – Assay results from Black Range
All assays from the 2017 drilling program at Black Range.
Abbreviations used: Co – cobalt, Ni – nickel, Sc – scandium, Pt – platinum, Pd – palladium, Cr – chromium, m – metre, g/t – grams per tonne, ppb – parts per billion, b.d. – below detection.
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
Hole |
From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ABR0001 | 0.00 |
2.00 | 2.00 | R102918 | 0.002 | 0.08 | 90 |
635 | 533 | 0.43 | ABR0003 |
6.00 |
8.00 | 2.00 | RC537866 | 0.050 | 0.35 | 80 |
230 | 288 | 0.60 |
| ABR0001 | 2.00 |
4.00 | 2.00 | R102919 | 0.002 | 0.07 | 80 |
602 | 528 | 0.46 | ABR0003 |
8.00 |
10.00 | 2.00 | RC537867 | 0.189 | 0.52 | 90 |
404 | 440 | 0.65 |
| ABR0001 | 4.00 |
6.00 | 2.00 | R102920 | b.d. | 0.25 | 120 | 413 |
259 | 0.96 | ABR0003 |
10.00 |
12.00 | 2.00 | RC537868 | 0.217 | 0.89 | 60 |
288 | 443 | 1.14 |
| ABR0001 | 6.00 |
8.00 | 2.00 | R102921 | 0.002 | 0.14 | 100 | 841 |
449 | 0.79 | ABR0003 |
12.00 |
14.00 | 2.00 | RC537869 | 0.098 | 0.66 | 30 |
45 | 105 | 1.20 |
| ABR0001 | 8.00 |
10.00 | 2.00 |
R102922 | 0.006 | 0.21 | 90 |
523 | 435 | 0.52 | ABR0003 |
14.00 |
16.00 | 2.00 | RC537870 | 0.158 | 0.68 | 20 |
61 | 111 | 0.94 |
| ABR0001 | 10.00 |
12.00 | 2.00 |
R102923 | 0.018 | 0.24 | 100 | 235 |
195 | 1.07 | ABR0003 |
16.00 |
18.00 | 2.00 | RC537872 | 0.061 | 0.74 | 30 |
55 | 88 | 0.93 |
| ABR0001 | 12.00 |
14.00 | 2.00 |
R102924 | 0.028 | 0.20 | 130 | 326 |
274 | 1.39 | ABR0003 |
18.00 |
20.00 | 2.00 | RC537873 | 0.016 | 0.37 | 10 |
30 | 71 | 0.53 |
| ABR0001 | 14.00 |
16.00 | 2.00 |
R102925 | 0.052 | 0.27 | 120 | 287 |
224 | 1.57 | ABR0003 |
20.00 |
22.00 | 2.00 | RC537874 | 0.025 | 0.36 | 20 |
33 | 51 | 0.75 |
| ABR0001 | 16.00 |
18.00 | 2.00 |
R102926 | 0.047 | 0.25 | 50 |
328 | 369 | 1.49 | ABR0003 |
22.00 |
24.00 | 2.00 | RC537875 | 0.040 | 0.38 | 30 |
82 | 105 | 0.86 |
| ABR0001 | 18.00 |
20.00 | 2.00 |
R102927 | 0.106 | 0.38 | 40 |
97 | 83 | 0.80 | ABR0003 |
24.00 |
26.00 | 2.00 | RC537876 | 0.028 | 0.32 | 20 |
59 | 53 | 1.10 |
| ABR0001 | 20.00 |
22.00 | 2.00 |
R102928 | 0.074 | 0.38 | 20 |
72 | 105 | 0.73 | ABR0003 |
26.00 |
28.00 | 2.00 | RC537877 | 0.024 | 0.23 | 10 |
29 | 47 | 0.78 |
| ABR0001 | 22.00 |
24.00 | 2.00 |
R102929 | 0.095 | 0.46 | 30 |
94 | 84 | 0.72 | ABR0003 |
28.00 |
30.00 | 2.00 | RC537878 | 0.018 | 0.18 | 10 |
46 | 54 | 0.75 |
| ABR0001 | 24.00 |
26.00 | 2.00 |
R102930 | 0.058 | 0.47 | 30 |
168 | 191 | 0.83 | ABR0003 |
30.00 |
32.00 | 2.00 | RC537879 | 0.020 | 0.18 | 20 |
21 | 34 | 0.67 |
| ABR0001 | 26.00 |
28.00 | 2.00 |
R102932 | 0.035 | 0.30 | 30 |
79 | 98 | 0.64 | ABR0003 |
32.00 |
34.00 | 2.00 | RC537880 | 0.021 | 0.18 | 30 |
21 | 42 | 0.79 |
| ABR0001 | 28.00 |
30.00 | 2.00 |
R102933 | 0.032 | 0.24 | 10 |
68 | 150 | 0.55 | ABR0003 |
34.00 |
36.00 | 2.00 | RC537881 | 0.020 | 0.18 | 10 |
34 | 27 | 0.73 |
| ABR0001 | 30.00 |
32.00 | 2.00 |
R102934 | 0.028 | 0.23 | 30 |
96 | 118 | 0.54 | ABR0003 |
36.00 |
38.00 | 2.00 | RC537882 | 0.019 | 0.18 | 10 |
52 | 37 | 0.76 |
| ABR0001 | 32.00 |
34.00 | 2.00 |
R102935 | 0.023 | 0.20 | 20 |
48 | 76 | 0.54 | ABR0003 |
38.00 |
40.00 | 2.00 | RC537883 | 0.020 | 0.18 | 10 |
31 | 29 | 0.74 |
| ABR0001 | 34.00 |
36.00 | 2.00 |
R102936 | 0.016 | 0.18 | 20 |
76 | 82 | 0.60 | ABR0003 |
40.00 |
42.00 | 2.00 | RC537884 | 0.015 | 0.14 | b.d. | 24 |
37 | 0.55 |
| ABR0001 | 36.00 |
38.00 | 2.00 |
R102937 | 0.014 | 0.14 | 20 |
44 | 58 | 0.49 | ABR0003 |
42.00 |
44.00 | 2.00 | RC537885 | 0.011 | 0.10 | 10 |
19 | 23 | 0.38 |
| ABR0001 | 38.00 |
40.00 | 2.00 |
R102938 | 0.010 | 0.10 | 10 |
46 | 92 | 0.38 | ABR0003 |
44.00 |
46.00 | 2.00 | RC537886 | 0.008 | 0.09 | b.d. | 23 |
21 | 0.32 |
| ABR0001 | 40.00 |
42.00 | 2.00 |
R102939 | 0.011 | 0.12 | 20 |
218 | 296 | 0.37 | ABR0003 |
46.00 |
48.00 | 2.00 | RC537887 | 0.008 | 0.09 | b.d. | 16 |
17 | 0.31 |
| ABR0001 | 42.00 |
44.00 | 2.00 |
R102940 | 0.009 | 0.10 | 10 |
283 | 175 | 0.36 | ABR0003 |
48.00 |
50.00 | 2.00 | RC537888 | 0.007 | 0.08 | b.d. | 12 |
15 | 0.31 |
| ABR0001 | 44.00 |
46.00 | 2.00 |
R102941 | 0.009 | 0.10 | 10 |
38 | 46 | 0.36 | ABR0003 |
50.00 |
52.00 | 2.00 | RC537889 | 0.006 | 0.08 | b.d. | 14 |
15 | 0.30 |
| ABR0001 | 46.00 |
48.00 | 2.00 |
R102942 | 0.009 | 0.09 | 20 |
69 | 53 | 0.33 | ABR0003 |
52.00 |
54.00 | 2.00 | RC537891 | 0.011 | 0.10 | b.d. | 18 |
21 | 0.35 |
| ABR0001 | 48.00 |
50.00 | 2.00 |
R102943 | 0.011 | 0.11 | 30 |
49 | 60 | 0.39 | ABR0003 |
54.00 |
56.00 | 2.00 | RC537892 | 0.012 | 0.11 | 10 |
18 | 13 | 0.42 |
| ABR0001 | 50.00 |
52.00 | 2.00 |
R102944 | 0.011 | 0.11 | 20 |
24 | 23 | 0.41 | ABR0003 |
56.00 |
58.00 | 2.00 | RC537893 | 0.013 | 0.12 | 10 |
20 | 14 | 0.46 |
| ABR0001 | 52.00 |
54.00 | 2.00 |
R102945 | 0.013 | 0.12 | 20 |
35 | 37 | 0.42 | ABR0003 |
58.00 |
60.00 | 2.00 | RC537894 | 0.014 | 0.12 | 20 |
19 | 21 | 0.46 |
| ABR0001 | 54.00 |
56.00 | 2.00 |
R102946 | 0.012 | 0.12 | 30 |
20 | 41 | 0.39 | ABR0003 |
60.00 |
62.00 | 2.00 | RC537895 | 0.014 | 0.12 | 10 |
25 | 24 | 0.46 |
| ABR0001 | 56.00 |
58.00 | 2.00 |
R102947 | 0.013 | 0.12 | 30 |
32 | 43 | 0.42 | ABR0003 |
62.00 |
64.00 | 2.00 | RC537896 | 0.013 | 0.12 | 20 |
23 | 23 | 0.47 |
| ABR0001 | 58.00 |
60.00 | 2.00 |
R102948 | 0.013 | 0.12 | 20 |
20 | 26 | 0.44 | ABR0003 |
64.00 |
66.00 | 2.00 | RC537897 | 0.014 | 0.12 | 10 |
18 | 19 | 0.43 |
| ABR0001 | 60.00 |
62.00 | 2.00 |
R102949 | 0.014 | 0.12 | 30 |
62 | 83 | 0.44 | ABR0003 |
66.00 |
68.00 | 2.00 | RC537898 | 0.014 | 0.13 | 20 |
26 | 25 | 0.46 |
| ABR0001 | 62.00 |
64.00 | 2.00 |
R102951 | 0.013 | 0.12 | 20 |
40 | 43 | 0.45 | ABR0003 |
68.00 |
70.00 | 2.00 | RC537899 | 0.012 | 0.12 | 10 |
28 | 31 | 0.45 |
| ABR0001 | 64.00 |
66.00 | 2.00 |
R102952 | 0.013 | 0.12 | 20 |
30 | 38 | 0.43 | ABR0003 |
70.00 |
72.00 | 2.00 | RC537900 | 0.013 | 0.12 | 20 |
38 | 37 | 0.44 |
| ABR0001 | 66.00 |
68.00 | 2.00 |
R102953 | 0.013 | 0.12 | 20 |
33 | 56 | 0.43 | ABR0003 |
72.00 |
74.00 | 2.00 | RC537901 | 0.013 | 0.10 | 20 |
63 | 60 | 0.40 |
| ABR0001 | 68.00 |
70.00 | 2.00 |
R102954 | 0.013 | 0.12 | 20 |
53 | 56 | 0.43 | ABR0003 |
74.00 |
76.00 | 2.00 | RC537902 | 0.014 | 0.12 | 10 |
37 | 48 | 0.42 |
| ABR0001 | 70.00 |
72.00 | 2.00 |
R102955 | 0.013 | 0.12 | 20 |
36 | 37 | 0.44 | ABR0003 |
76.00 |
78.00 | 2.00 | RC537903 | 0.013 | 0.12 | b.d. | 149 |
158 | 0.40 |
| ABR0001 | 72.00 |
73.00 | 1.00 |
R102956 | 0.013 | 0.12 | 30 |
40 | 46 | 0.45 | ABR0003 |
78.00 |
80.00 | 2.00 | RC537904 | 0.013 | 0.12 | 20 |
132 | 136 | 0.44 |
| ABR0002 | 0.00 |
2.00 | 2.00 | R102957 | 0.013 | 0.51 | 50 |
83 | 111 | 1.59 | ABR0004 |
0.00 |
2.00 | 2.00 | RC537905 | 0.009 | 0.16 | 60 |
165 | 180 | 1.16 |
| ABR0002 | 2.00 |
4.00 | 2.00 | R102958 | 0.027 | 0.54 | 60 |
186 | 231 | 1.39 | ABR0004 |
2.00 |
4.00 | 2.00 | RC537906 | 0.009 | 0.23 | 50 |
210 | 259 | 0.73 |
| ABR0002 | 4.00 |
6.00 | 2.00 | R102959 | 0.026 | 0.38 | 30 |
109 | 108 | 1.44 | ABR0004 |
4.00 |
6.00 | 2.00 | RC537907 | 0.022 | 0.32 | 50 |
344 | 434 | 0.62 |
| ABR0002 | 6.00 |
8.00 | 2.00 | R102960 | 0.053 | 0.54 | 30 |
92 | 96 | 0.86 | ABR0004 |
6.00 |
8.00 | 2.00 | RC537908 | 0.017 | 0.30 | 80 |
504 | 702 | 0.73 |
| ABR0002 | 8.00 |
10.00 | 2.00 |
R102961 | 0.084 | 0.61 | 20 |
60 | 67 | 0.76 | ABR0004 |
8.00 |
10.00 | 2.00 | RC537909 | 0.012 | 0.29 | 80 |
419 | 711 | 0.60 |
| ABR0002 | 10.00 |
12.00 | 2.00 |
R102962 | 0.134 | 0.68 | 40 |
85 | 69 | 0.75 | ABR0004 |
10.00 |
12.00 | 2.00 | RC537911 | 0.013 | 0.31 | 90 |
388 | 567 | 0.94 |
| ABR0002 | 12.00 |
14.00 | 2.00 |
R102963 | 0.067 | 0.58 | 20 |
88 | 86 | 0.86 | ABR0004 |
12.00 |
14.00 | 2.00 | RC537912 | 0.013 | 0.28 | 100 | 394 |
495 | 1.09 |
| ABR0002 | 14.00 |
16.00 | 2.00 |
R102964 | 0.019 | 0.43 | 20 |
65 | 91 | 0.77 | ABR0004 |
14.00 |
16.00 | 2.00 | RC537913 | 0.021 | 0.43 | 60 |
235 | 300 | 1.42 |
| ABR0002 | 16.00 |
18.00 | 2.00 |
R102965 | 0.021 | 0.39 | 30 |
52 | 73 | 0.76 | ABR0004 |
16.00 |
18.00 | 2.00 | RC537914 | 0.018 | 0.42 | 60 |
246 | 249 | 1.09 |
| ABR0002 | 18.00 |
20.00 | 2.00 |
R102966 | 0.055 | 0.38 | 30 |
74 | 78 | 0.74 | ABR0004 |
18.00 |
20.00 | 2.00 | RC537915 | 0.013 | 0.37 | 30 |
139 | 138 | 1.05 |
| ABR0002 | 20.00 |
22.00 | 2.00 |
R102967 | 0.036 | 0.33 | 20 |
50 | 59 | 0.72 | ABR0004 |
20.00 |
22.00 | 2.00 | RC537916 | 0.064 | 0.44 | 30 |
161 | 139 | 0.71 |
| ABR0002 | 22.00 |
24.00 | 2.00 |
R102968 | 0.049 | 0.31 | 20 |
47 | 54 | 0.73 | ABR0004 |
22.00 |
24.00 | 2.00 | RC537917 | 0.066 | 0.59 | 20 |
143 | 137 | 0.69 |
| ABR0002 | 24.00 |
26.00 | 2.00 |
R102969 | 0.031 | 0.29 | 20 |
52 | 56 | 0.78 | ABR0004 |
24.00 |
26.00 | 2.00 | RC537918 | 0.052 | 0.73 | 30 |
110 | 114 | 1.03 |
| ABR0002 | 26.00 |
28.00 | 2.00 |
R102971 | 0.024 | 0.27 | 20 |
35 | 47 | 0.73 | ABR0004 |
26.00 |
28.00 | 2.00 | RC537919 | 0.029 | 0.45 | 30 |
99 | 121 | 0.80 |
| ABR0002 | 28.00 |
30.00 | 2.00 |
R102972 | 0.019 | 0.21 | 20 |
41 | 54 | 0.66 | ABR0004 |
28.00 |
30.00 | 2.00 | RC537920 | 0.018 | 0.19 | 10 |
87 | 109 | 0.55 |
| ABR0002 | 30.00 |
32.00 | 2.00 |
R102973 | 0.016 | 0.18 | 20 |
44 | 57 | 0.63 | ABR0004 |
30.00 |
32.00 | 2.00 | RC537921 | 0.017 | 0.18 | 10 |
64 | 94 | 0.56 |
| ABR0002 | 32.00 |
34.00 | 2.00 |
R102974 | 0.016 | 0.17 | 20 |
57 | 61 | 0.63 | ABR0004 |
32.00 |
34.00 | 2.00 | RC537922 | 0.019 | 0.18 | 10 |
47 | 101 | 0.63 |
| ABR0002 | 34.00 |
36.00 | 2.00 |
R102975 | 0.016 | 0.15 | 10 |
51 | 60 | 0.64 | ABR0004 |
34.00 |
36.00 | 2.00 | RC537923 | 0.019 | 0.19 | b.d. | 31 |
67 | 0.63 |
| ABR0002 | 36.00 |
38.00 | 2.00 |
R102976 | 0.016 | 0.16 | 20 |
41 | 47 | 0.62 | ABR0004 |
36.00 |
38.00 | 2.00 | RC537924 | 0.011 | 0.16 | 10 |
42 | 96 | 0.61 |
| ABR0002 | 38.00 |
40.00 | 2.00 |
R102977 | 0.017 | 0.17 | 30 |
41 | 55 | 0.57 | ABR0004 |
38.00 |
40.00 | 2.00 | RC537925 | 0.019 | 0.19 | b.d. | 53 |
90 | 0.61 |
| ABR0002 | 40.00 |
42.00 | 2.00 |
R102978 | 0.009 | 0.09 | 10 |
21 | 26 | 0.32 | ABR0004 |
40.00 |
42.00 | 2.00 | RC537926 | 0.017 | 0.17 | 20 |
68 | 59 | 0.60 |
| ABR0002 | 42.00 |
44.00 | 2.00 |
R102979 | 0.007 | 0.08 | b.d. | 13 |
20 | 0.30 | ABR0004 |
42.00 |
44.00 | 2.00 | RC537927 | 0.016 | 0.15 | 10 |
59 | 75 | 0.56 |
| ABR0002 | 44.00 |
46.00 | 2.00 |
R102980 | 0.007 | 0.08 | 10 |
23 | 27 | 0.28 | ABR0004 |
44.00 |
46.00 | 2.00 | RC537928 | 0.017 | 0.16 | 10 |
49 | 68 | 0.57 |
| ABR0002 | 46.00 |
48.00 | 2.00 |
R102981 | 0.007 | 0.08 | 10 |
18 | 21 | 0.29 | ABR0004 |
46.00 |
48.00 | 2.00 | RC537929 | 0.011 | 0.14 | b.d. | 27 |
37 | 0.58 |
| ABR0002 | 48.00 |
50.00 | 2.00 |
R102982 | 0.009 | 0.09 | 10 |
26 | 31 | 0.33 | ABR0004 |
48.00 |
50.00 | 2.00 | RC537930 | 0.008 | 0.10 | b.d. | 16 |
24 | 0.34 |
| ABR0002 | 50.00 |
52.00 | 2.00 |
R102983 | 0.008 | 0.08 | 10 |
19 | 25 | 0.29 | ABR0004 |
50.00 |
52.00 | 2.00 | RC537932 | 0.006 | 0.07 | 10 |
8 | 16 | 0.21 |
| ABR0002 | 52.00 |
54.00 | 2.00 |
R102984 | 0.009 | 0.09 | 10 |
20 | 28 | 0.35 | ABR0004 |
52.00 |
54.00 | 2.00 | RC537933 | 0.006 | 0.07 | b.d. | 8 |
18 | 0.27 |
| ABR0002 | 54.00 |
56.00 | 2.00 |
R102985 | 0.006 | 0.08 | b.d. | 24 |
27 | 0.31 | ABR0004 |
54.00 |
56.00 | 2.00 | RC537934 | 0.006 | 0.07 | b.d. | 11 |
15 | 0.26 |
| ABR0002 | 56.00 |
58.00 | 2.00 |
R102986 | 0.009 | 0.09 | 10 |
16 | 25 | 0.35 | ABR0004 |
56.00 |
58.00 | 2.00 | RC537935 | 0.007 | 0.08 | b.d. | 12 |
10 | 0.30 |
| ABR0002 | 58.00 |
60.00 | 2.00 |
R102987 | 0.012 | 0.12 | 10 |
24 | 35 | 0.43 | ABR0004 |
58.00 |
60.00 | 2.00 | RC537936 | 0.009 | 0.09 | b.d. | 14 |
10 | 0.33 |
| ABR0002 | 60.00 |
62.00 | 2.00 |
R102988 | 0.010 | 0.12 | 20 |
25 | 41 | 0.42 | ABR0004 |
60.00 |
62.00 | 2.00 | RC537937 | 0.014 | 0.12 | 20 |
20 | 38 | 0.46 |
| ABR0002 | 62.00 |
64.00 | 2.00 |
R102989 | 0.006 | 0.07 | 10 |
20 | 28 | 0.24 | ABR0004 |
62.00 |
64.00 | 2.00 | RC537938 | 0.013 | 0.12 | 10 |
17 | 17 | 0.43 |
| ABR0002 | 64.00 |
66.00 | 2.00 |
R102990 | 0.013 | 0.12 | 20 |
23 | 36 | 0.46 | ABR0004 |
64.00 |
66.00 | 2.00 | RC537939 | 0.014 | 0.12 | 10 |
21 | 27 | 0.46 |
| ABR0002 | 66.00 |
68.00 | 2.00 |
R102992 | 0.013 | 0.12 | 30 |
18 | 24 | 0.45 | ABR0004 |
66.00 |
68.00 | 2.00 | RC537940 | 0.013 | 0.12 | 20 |
21 | 21 | 0.46 |
| ABR0002 | 68.00 |
70.00 | 2.00 |
R102993 | 0.014 | 0.12 | 20 |
27 | 36 | 0.46 | ABR0004 |
68.00 |
70.00 | 2.00 | RC537941 | 0.014 | 0.12 | 20 |
22 | 15 | 0.45 |
| ABR0002 | 70.00 |
72.00 | 2.00 |
R102994 | 0.013 | 0.12 | 30 |
35 | 36 | 0.44 | ABR0004 |
70.00 |
72.00 | 2.00 | RC537942 | 0.013 | 0.12 | 10 |
20 | 10 | 0.43 |
| ABR0002 | 72.00 |
74.00 | 2.00 |
R102995 | 0.013 | 0.12 | 20 |
20 | 36 | 0.44 | ABR0004 |
72.00 |
74.00 | 2.00 | RC537943 | 0.014 | 0.12 | 10 |
15 | 10 | 0.45 |
| ABR0002 | 74.00 |
76.00 | 2.00 |
R102996 | 0.013 | 0.13 | 20 |
40 | 44 | 0.46 | ABR0004 |
74.00 |
76.00 | 2.00 | RC537944 | 0.014 | 0.13 | 10 |
29 | 24 | 0.45 |
| ABR0002 | 76.00 |
78.00 | 2.00 |
R102997 | 0.014 | 0.12 | 30 |
27 | 39 | 0.46 | ABR0004 |
76.00 |
78.00 | 2.00 | RC537945 | 0.013 | 0.12 | 10 |
35 | 20 | 0.47 |
| ABR0002 | 78.00 |
79.00 | 1.00 |
R102998 | 0.013 | 0.12 | 30 |
39 | 74 | 0.45 | ABR0004 |
78.00 |
80.00 | 2.00 | RC537946 | 0.014 | 0.12 | 20 |
30 | 26 | 0.45 |
| ABR0003 | 0.00 |
2.00 | 2.00 | R102999 | 0.019 | 0.27 | 60 |
483 | 325 | 1.19 | |||||||||||
| ABR0005 | 0.00 |
2.00 | 2.00 | RC537947 | 0.007 | 0.15 | 50 |
177 | 160 | 0.86 | |||||||||||
| ABR0003 | 2.00 |
4.00 | 2.00 | R103000 | 0.036 | 0.32 | 60 |
260 | 193 | 1.53 | ABR0005 |
2.00 |
4.00 | 2.00 | RC537948 | 0.008 | 0.18 | 60 |
232 | 252 | 1.02 |
| ABR0003 | 4.00 |
6.00 | 2.00 | RC537865 | 0.040 | 0.37 | 60 |
339 | 306 | 1.06 | ABR0005 |
4.00 |
6.00 | 2.00 | RC537949 | 0.011 | 0.28 | 60 |
449 | 536 | 1.06 |
17
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Cobalt, Scandium & PGM results from Black Range
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
Hole |
From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ABR0005 | 6.00 |
8.00 | 2.00 | RC537951 | 0.021 | 0.52 | 40 |
295 | 445 | 1.32 | ABR0007 |
42.00 |
44.00 | 2.00 | S200053 | 0.120 | 1.21 | 10 |
85 | 126 | 1.13 |
| ABR0005 | 8.00 |
10.00 | 2.00 |
RC537952 | 0.024 | 0.66 | 40 |
309 | 351 | 1.58 | ABR0007 |
44.00 |
46.00 | 2.00 | S200054 | 0.123 | 0.74 | 30 |
80 | 98 | 1.02 |
| ABR0005 | 10.00 |
12.00 | 2.00 |
RC537953 | 0.039 | 0.74 | 40 |
167 | 173 | 1.63 | ABR0007 |
46.00 |
48.00 | 2.00 | S200055 | 0.057 | 0.38 | 30 |
52 | 77 | 0.71 |
| ABR0005 | 12.00 |
14.00 | 2.00 |
RC537954 | 0.089 | 0.84 | 50 |
231 | 178 | 1.21 | ABR0007 |
48.00 |
50.00 | 2.00 | S200056 | 0.081 | 0.46 | 10 |
42 | 58 | 0.75 |
| ABR0005 | 14.00 |
16.00 | 2.00 |
RC537955 | 0.114 | 0.86 | 30 |
182 | 232 | 1.33 | ABR0007 |
50.00 |
52.00 | 2.00 | S200057 | 0.087 | 0.41 | b.d. | 46 |
72 | 0.82 |
| ABR0005 | 16.00 |
18.00 | 2.00 |
RC537956 | 0.027 | 0.79 | 30 |
186 | 180 | 0.98 | ABR0007 |
52.00 |
54.00 | 2.00 | S200058 | 0.066 | 0.35 | 20 |
68 | 125 | 1.03 |
| ABR0005 | 18.00 |
20.00 | 2.00 |
RC537957 | 0.022 | 0.64 | 40 |
143 | 180 | 1.23 | ABR0007 |
54.00 |
56.00 | 2.00 | S200059 | 0.052 | 0.38 | 20 |
49 | 91 | 0.97 |
| ABR0005 | 20.00 |
22.00 | 2.00 |
RC537958 | 0.017 | 0.39 | 40 |
119 | 141 | 1.01 | ABR0007 |
56.00 |
58.00 | 2.00 | S200061 | 0.042 | 0.37 | 20 |
39 | 63 | 1.10 |
| ABR0005 | 22.00 |
24.00 | 2.00 |
RC537959 | 0.013 | 0.20 | 30 |
70 | 106 | 0.56 | ABR0007 |
58.00 |
60.00 | 2.00 | S200062 | 0.052 | 0.37 | 20 |
68 | 103 | 1.15 |
| ABR0005 | 24.00 |
26.00 | 2.00 |
RC537960 | 0.021 | 0.19 | 10 |
54 | 94 | 0.58 | ABR0007 |
60.00 |
62.00 | 2.00 | S200063 | 0.042 | 0.37 | 30 |
65 | 97 | 1.31 |
| ABR0005 | 26.00 |
28.00 | 2.00 |
RC537961 | 0.018 | 0.18 | 10 |
48 | 95 | 0.58 | ABR0007 |
62.00 |
64.00 | 2.00 | S200064 | 0.047 | 0.44 | 20 |
57 | 83 | 1.19 |
| ABR0005 | 28.00 |
30.00 | 2.00 |
RC537962 | 0.022 | 0.19 | 20 |
46 | 90 | 0.58 | ABR0007 |
64.00 |
66.00 | 2.00 | S200065 | 0.031 | 0.28 | 10 |
37 | 60 | 1.01 |
| ABR0005 | 30.00 |
32.00 | 2.00 |
RC537963 | 0.015 | 0.17 | b.d. | 65 |
105 | 0.63 | ABR0007 |
66.00 |
68.00 | 2.00 | S200066 | 0.024 | 0.26 | 30 |
30 | 58 | 0.90 |
| ABR0005 | 32.00 |
34.00 | 2.00 |
RC537964 | 0.014 | 0.13 | 20 |
72 | 100 | 0.53 | ABR0007 |
68.00 |
70.00 | 2.00 | S200067 | 0.021 | 0.23 | 20 |
31 | 64 | 0.96 |
| ABR0005 | 34.00 |
36.00 | 2.00 |
RC537965 | 0.014 | 0.14 | 10 |
47 | 77 | 0.56 | ABR0007 |
70.00 |
72.00 | 2.00 | S200068 | 0.017 | 0.22 | 10 |
28 | 44 | 0.79 |
| ABR0005 | 36.00 |
38.00 | 2.00 |
RC537966 | 0.017 | 0.17 | 20 |
67 | 75 | 0.57 | ABR0007 |
72.00 |
74.00 | 2.00 | S200069 | 0.016 | 0.18 | 10 |
21 | 49 | 0.68 |
| ABR0005 | 38.00 |
40.00 | 2.00 |
RC537967 | 0.014 | 0.18 | 10 |
39 | 67 | 0.61 | ABR0007 |
74.00 |
76.00 | 2.00 | S200070 | 0.015 | 0.17 | 10 |
27 | 46 | 0.60 |
| ABR0005 | 40.00 |
42.00 | 2.00 |
RC537968 | 0.012 | 0.14 | 10 |
23 | 58 | 0.52 | ABR0007 |
76.00 |
78.00 | 2.00 | S200071 | 0.021 | 0.19 | 10 |
35 | 75 | 0.79 |
| ABR0005 | 42.00 |
44.00 | 2.00 |
RC537969 | 0.014 | 0.13 | 20 |
29 | 66 | 0.46 | ABR0007 |
78.00 |
80.00 | 2.00 | S200072 | 0.021 | 0.20 | 20 |
31 | 45 | 0.86 |
| ABR0005 | 44.00 |
46.00 | 2.00 |
RC537971 | 0.009 | 0.10 | 10 |
28 | 29 | 0.31 | ABR0007 |
80.00 |
82.00 | 2.00 | S200073 | 0.022 | 0.19 | 20 |
25 | 28 | 0.89 |
| ABR0005 | 46.00 |
48.00 | 2.00 |
RC537972 | 0.004 | 0.06 | b.d. | 12 |
17 | 0.19 | ABR0007 |
82.00 |
84.00 | 2.00 | S200074 | 0.019 | 0.19 | 10 |
25 | 53 | 0.74 |
| ABR0005 | 48.00 |
50.00 | 2.00 |
RC537973 | 0.006 | 0.08 | b.d. | 24 |
34 | 0.32 | ABR0007 |
84.00 |
86.00 | 2.00 | S200075 | 0.021 | 0.19 | 10 |
30 | 59 | 0.68 |
| ABR0005 | 50.00 |
52.00 | 2.00 |
RC537974 | 0.007 | 0.07 | b.d. | 15 |
27 | 0.27 | ABR0007 |
86.00 |
88.00 | 2.00 | S200076 | 0.012 | 0.13 | 10 |
18 | 37 | 0.50 |
| ABR0005 | 52.00 |
54.00 | 2.00 |
RC537975 | 0.006 | 0.08 | b.d. | 25 |
35 | 0.29 | ABR0007 |
88.00 |
90.00 | 2.00 | S200077 | 0.012 | 0.11 | b.d. | 26 |
35 | 0.44 |
| ABR0005 | 54.00 |
56.00 | 2.00 |
RC537976 | 0.005 | 0.07 | b.d. | 19 |
31 | 0.29 | ABR0007 |
90.00 |
92.00 | 2.00 | S200078 | 0.009 | 0.10 | 10 |
16 | 31 | 0.33 |
| ABR0005 | 56.00 |
58.00 | 2.00 |
RC537977 | 0.009 | 0.10 | 10 |
24 | 39 | 0.36 | ABR0007 |
92.00 |
94.00 | 2.00 | S200079 | 0.013 | 0.12 | 20 |
17 | 23 | 0.44 |
| ABR0005 | 58.00 |
60.00 | 2.00 |
RC537978 | 0.011 | 0.11 | 20 |
33 | 42 | 0.42 | ABR0007 |
94.00 |
96.00 | 2.00 | S200080 | 0.010 | 0.10 | b.d. | 20 |
23 | 0.35 |
| ABR0005 | 60.00 |
62.00 | 2.00 |
RC537979 | 0.011 | 0.11 | 10 |
40 | 47 | 0.41 | ABR0007 |
96.00 |
98.00 | 2.00 | S200082 | 0.013 | 0.13 | 20 |
19 | 22 | 0.45 |
| ABR0005 | 62.00 |
64.00 | 2.00 |
RC537980 | 0.009 | 0.09 | 10 |
24 | 27 | 0.35 | ABR0007 |
98.00 |
100.00 | 2.00 |
S200083 | 0.013 | 0.13 | 10 |
16 | 22 | 0.44 |
| ABR0005 | 64.00 |
66.00 | 2.00 |
RC537981 | 0.012 | 0.11 | b.d. | 31 |
29 | 0.41 | ABR0007 |
100.00 | 102.00 | 2.00 |
S200084 | 0.009 | 0.09 | 10 |
12 | 17 | 0.36 |
| ABR0005 | 66.00 |
68.00 | 2.00 |
RC537982 | 0.012 | 0.12 | 10 |
31 | 37 | 0.44 | ABR0007 |
102.00 | 104.00 | 2.00 |
S200085 | 0.013 | 0.13 | 20 |
21 | 19 | 0.46 |
| ABR0005 | 68.00 |
70.00 | 2.00 |
RC537983 | 0.012 | 0.11 | 10 |
12 | 19 | 0.44 | ABR0007 |
104.00 | 106.00 | 2.00 |
S200086 | 0.013 | 0.13 | 10 |
18 | 22 | 0.44 |
| ABR0005 | 70.00 |
72.00 | 2.00 |
RC537984 | 0.013 | 0.12 | 30 |
20 | 25 | 0.44 | ABR0007 |
106.00 | 108.00 | 2.00 |
S200087 | 0.013 | 0.12 | 10 |
15 | 20 | 0.43 |
| ABR0005 | 72.00 |
74.00 | 2.00 |
RC537985 | 0.012 | 0.12 | 20 |
18 | 18 | 0.45 | ABR0007 |
108.00 | 110.00 | 2.00 |
S200088 | 0.013 | 0.12 | 20 |
20 | 32 | 0.43 |
| ABR0005 | 74.00 |
76.00 | 2.00 |
RC537986 | 0.012 | 0.12 | 20 |
14 | 18 | 0.46 | |||||||||||
| ABR0005 | 76.00 |
78.00 | 2.00 |
RC537987 | 0.013 | 0.12 | 20 |
18 | 23 | 0.45 | ABR0008 |
0.00 |
2.00 | 2.00 | S200089 | 0.003 | 0.06 | 30 |
156 | 97 | 0.34 |
| ABR0005 | 78.00 |
80.00 | 2.00 |
RC537988 | 0.012 | 0.12 | 30 |
22 | 33 | 0.44 | ABR0008 |
2.00 |
4.00 | 2.00 | S200090 | 0.004 | 0.05 | 40 |
156 | 92 | 0.53 |
| ABR0008 | 4.00 |
6.00 | 2.00 | S200091 | 0.002 | 0.04 | 30 |
105 | 66 | 0.50 | |||||||||||
| ABR0006 | 0.00 |
2.00 | 2.00 | RC537989 | 0.003 | 0.06 | 90 |
116 | 104 | 0.88 | ABR0008 |
6.00 |
8.00 | 2.00 | S200092 | 0.002 | 0.02 | 20 |
42 | 29 | 0.27 |
| ABR0006 | 2.00 |
4.00 | 2.00 | RC537990 | 0.002 | 0.08 | 100 | 82 |
80 | 0.98 | ABR0008 |
8.00 |
10.00 | 2.00 | S200093 | b.d. | 0.02 | 20 |
30 | 19 | 0.24 |
| ABR0006 | 4.00 |
6.00 | 2.00 | RC537992 | 0.002 | 0.08 | 130 | 94 |
120 | 0.96 | ABR0008 |
10.00 |
12.00 | 2.00 | S200094 | b.d. | 0.02 | 10 |
36 | 19 | 0.27 |
| ABR0006 | 6.00 |
8.00 | 2.00 | RC537993 | 0.002 | 0.08 | 80 |
111 | 155 | 1.04 | ABR0008 |
12.00 |
14.00 | 2.00 | S200095 | b.d. | 0.02 | 20 |
34 | 15 | 0.23 |
| ABR0006 | 8.00 |
10.00 | 2.00 |
RC537994 | 0.004 | 0.14 | 70 |
119 | 198 | 0.84 | ABR0008 |
14.00 |
16.00 | 2.00 | S200096 | 0.001 | 0.03 | 30 |
29 | 12 | 0.27 |
| ABR0006 | 10.00 |
12.00 | 2.00 |
RC537995 | 0.049 | 0.31 | 40 |
439 | 421 | 0.56 | ABR0008 |
16.00 |
18.00 | 2.00 | S200097 | 0.002 | 0.10 | 30 |
25 | 14 | 0.25 |
| ABR0006 | 12.00 |
14.00 | 2.00 |
RC537996 | 0.071 | 0.30 | 10 |
146 | 273 | 0.23 | ABR0008 |
18.00 |
20.00 | 2.00 | S200098 | 0.001 | 0.04 | 10 |
22 | 20 | 0.25 |
| ABR0006 | 14.00 |
16.00 | 2.00 |
RC537997 | 0.092 | 0.51 | 40 |
98 | 267 | 0.66 | ABR0008 |
20.00 |
22.00 | 2.00 | S200099 | 0.001 | 0.06 | b.d. | 23 |
39 | 0.28 |
| ABR0006 | 16.00 |
18.00 | 2.00 |
RC537998 | 0.132 | 0.70 | 50 |
25 | 32 | 1.53 | ABR0008 |
22.00 |
24.00 | 2.00 | S200101 | 0.002 | 0.06 | 10 |
119 | 79 | 0.31 |
| ABR0006 | 18.00 |
20.00 | 2.00 |
RC537999 | 0.099 | 0.63 | 70 |
92 | 197 | 1.17 | ABR0008 |
24.00 |
26.00 | 2.00 | S200102 | 0.002 | 0.06 | 40 |
29 | 75 | 0.49 |
| ABR0006 | 20.00 |
22.00 | 2.00 |
RC538000 | 0.140 | 0.76 | 60 |
13 | 17 | 1.54 | ABR0008 |
26.00 |
28.00 | 2.00 | S200103 | 0.004 | 0.08 | 30 |
34 | 23 | 0.81 |
| ABR0006 | 22.00 |
24.00 | 2.00 |
S200001 | 0.130 | 0.78 | 60 |
36 | 106 | 1.81 | ABR0008 |
28.00 |
30.00 | 2.00 | S200104 | 0.008 | 0.11 | 40 |
66 | 60 | 0.79 |
| ABR0006 | 24.00 |
26.00 | 2.00 |
S200002 | 0.116 | 0.84 | 70 |
74 | 164 | 1.85 | ABR0008 |
30.00 |
32.00 | 2.00 | S200105 | 0.006 | 0.13 | 40 |
65 | 90 | 0.75 |
| ABR0006 | 26.00 |
28.00 | 2.00 |
S200003 | 0.069 | 0.79 | 40 |
64 | 184 | 1.61 | ABR0008 |
32.00 |
34.00 | 2.00 | S200106 | 0.006 | 0.20 | 50 |
39 | 98 | 0.66 |
| ABR0006 | 28.00 |
30.00 | 2.00 |
S200004 | 0.049 | 0.70 | 40 |
60 | 195 | 1.19 | ABR0008 |
34.00 |
36.00 | 2.00 | S200107 | 0.006 | 0.23 | 50 |
41 | 112 | 0.93 |
| ABR0006 | 30.00 |
32.00 | 2.00 |
S200005 | 0.035 | 0.67 | 30 |
55 | 150 | 1.16 | ABR0008 |
36.00 |
38.00 | 2.00 | S200108 | 0.004 | 0.30 | 80 |
49 | 106 | 0.86 |
| ABR0006 | 32.00 |
34.00 | 2.00 |
S200006 | 0.035 | 0.52 | 30 |
54 | 142 | 0.94 | ABR0008 |
38.00 |
40.00 | 2.00 | S200109 | 0.004 | 0.36 | 70 |
30 | 109 | 0.89 |
| ABR0006 | 34.00 |
36.00 | 2.00 |
S200007 | 0.025 | 0.46 | 20 |
45 | 88 | 1.00 | ABR0008 |
40.00 |
42.00 | 2.00 | S200110 | 0.006 | 0.47 | 50 |
46 | 105 | 0.71 |
| ABR0006 | 36.00 |
38.00 | 2.00 |
S200008 | 0.025 | 0.42 | 20 |
40 | 121 | 0.97 | ABR0008 |
42.00 |
44.00 | 2.00 | S200111 | 0.006 | 0.48 | 40 |
43 | 122 | 0.76 |
| ABR0006 | 38.00 |
40.00 | 2.00 |
S200009 | 0.018 | 0.26 | 20 |
35 | 93 | 0.60 | ABR0008 |
44.00 |
46.00 | 2.00 | S200112 | 0.004 | 0.31 | 30 |
38 | 118 | 0.42 |
| ABR0006 | 40.00 |
42.00 | 2.00 |
S200010 | 0.016 | 0.21 | 20 |
31 | 88 | 0.56 | ABR0008 |
46.00 |
48.00 | 2.00 | S200113 | 0.006 | 0.36 | 40 |
61 | 121 | 0.60 |
| ABR0006 | 42.00 |
44.00 | 2.00 |
S200011 | 0.016 | 0.19 | 30 |
35 | 79 | 0.55 | ABR0008 |
48.00 |
50.00 | 2.00 | S200114 | 0.005 | 0.23 | 40 |
50 | 85 | 0.30 |
| ABR0006 | 44.00 |
46.00 | 2.00 |
S200012 | 0.016 | 0.21 | 20 |
37 | 110 | 0.61 | ABR0008 |
50.00 |
52.00 | 2.00 | S200115 | 0.008 | 0.32 | 40 |
53 | 73 | 0.49 |
| ABR0006 | 46.00 |
48.00 | 2.00 |
S200013 | 0.017 | 0.18 | 20 |
25 | 63 | 0.54 | ABR0008 |
52.00 |
54.00 | 2.00 | S200116 | 0.013 | 0.36 | 50 |
68 | 69 | 0.48 |
| ABR0006 | 48.00 |
50.00 | 2.00 |
S200014 | 0.018 | 0.16 | 10 |
25 | 47 | 0.54 | ABR0008 |
54.00 |
56.00 | 2.00 | S200117 | 0.014 | 0.33 | 40 |
51 | 68 | 0.48 |
| ABR0006 | 50.00 |
52.00 | 2.00 |
S200015 | 0.010 | 0.13 | 10 |
13 | 20 | 0.44 | ABR0008 |
56.00 |
58.00 | 2.00 | S200118 | 0.016 | 0.36 | 50 |
55 | 92 | 0.91 |
| ABR0006 | 52.00 |
54.00 | 2.00 |
S200016 | 0.009 | 0.08 | 10 |
11 | 13 | 0.27 | ABR0008 |
58.00 |
60.00 | 2.00 | S200119 | 0.059 | 0.38 | 50 |
54 | 80 | 0.83 |
| ABR0006 | 54.00 |
56.00 | 2.00 |
S200017 | 0.008 | 0.08 | 20 |
13 | 14 | 0.29 | ABR0008 |
60.00 |
62.00 | 2.00 | S200120 | 0.263 | 0.61 | 50 |
73 | 119 | 0.95 |
| ABR0006 | 56.00 |
58.00 | 2.00 |
S200018 | 0.008 | 0.09 | 10 |
13 | 14 | 0.35 | ABR0008 |
62.00 |
64.00 | 2.00 | S200122 | 0.229 | 0.59 | 50 |
64 | 119 | 0.79 |
| ABR0006 | 58.00 |
60.00 | 2.00 |
S200019 | 0.008 | 0.09 | 10 |
13 | 16 | 0.33 | ABR0008 |
64.00 |
66.00 | 2.00 | S200123 | 0.201 | 0.63 | 40 |
57 | 117 | 0.81 |
| ABR0006 | 60.00 |
62.00 | 2.00 |
S200020 | 0.007 | 0.08 | 10 |
12 | 12 | 0.30 | ABR0008 |
66.00 |
68.00 | 2.00 | S200124 | 0.056 | 0.39 | 50 |
59 | 106 | 1.15 |
| ABR0006 | 62.00 |
64.00 | 2.00 |
S200022 | 0.011 | 0.11 | 20 |
16 | 21 | 0.38 | ABR0008 |
68.00 |
70.00 | 2.00 | S200125 | 0.081 | 0.50 | 70 |
63 | 89 | 0.84 |
| ABR0006 | 64.00 |
66.00 | 2.00 |
S200023 | 0.012 | 0.11 | 20 |
16 | 15 | 0.42 | ABR0008 |
70.00 |
72.00 | 2.00 | S200126 | 0.174 | 0.67 | 60 |
76 | 102 | 1.18 |
| ABR0006 | 66.00 |
68.00 | 2.00 |
S200024 | 0.011 | 0.12 | 20 |
17 | 18 | 0.42 | ABR0008 |
72.00 |
74.00 | 2.00 | S200127 | 0.168 | 0.67 | 50 |
50 | 77 | 1.55 |
| ABR0006 | 68.00 |
70.00 | 2.00 |
S200025 | 0.012 | 0.12 | 10 |
17 | 19 | 0.44 | ABR0008 |
74.00 |
76.00 | 2.00 | S200128 | 0.134 | 0.76 | 40 |
48 | 85 | 1.12 |
| ABR0006 | 70.00 |
72.00 | 2.00 |
S200026 | 0.013 | 0.12 | 30 |
19 | 22 | 0.45 | ABR0008 |
76.00 |
78.00 | 2.00 | S200129 | 0.061 | 0.66 | 50 |
44 | 58 | 1.64 |
| ABR0006 | 72.00 |
74.00 | 2.00 |
S200027 | 0.013 | 0.12 | 20 |
19 | 21 | 0.45 | ABR0008 |
78.00 |
80.00 | 2.00 | S200130 | 0.051 | 0.41 | 40 |
56 | 99 | 1.21 |
| ABR0006 | 74.00 |
76.00 | 2.00 |
S200028 | 0.013 | 0.13 | 20 |
28 | 27 | 0.45 | ABR0008 |
80.00 |
82.00 | 2.00 | S200131 | 0.066 | 0.68 | 40 |
72 | 74 | 1.78 |
| ABR0006 | 76.00 |
78.00 | 2.00 |
S200029 | 0.010 | 0.12 | 20 |
19 | 21 | 0.43 | ABR0008 |
82.00 |
84.00 | 2.00 | S200132 | 0.053 | 0.45 | 50 |
54 | 83 | 1.29 |
| ABR0006 | 78.00 |
80.00 | 2.00 |
S200030 | 0.012 | 0.12 | 10 |
14 | 20 | 0.44 | ABR0008 |
84.00 |
86.00 | 2.00 | S200133 | 0.093 | 0.76 | 40 |
49 | 76 | 1.61 |
| ABR0008 | 86.00 |
88.00 | 2.00 | S200134 | 0.095 | 0.97 | 40 |
41 | 62 | 1.40 | |||||||||||
| ABR0007 | 0.00 |
2.00 | 2.00 | S200031 | 0.016 | 0.10 | 60 |
311 | 152 | 0.39 | ABR0008 |
88.00 |
90.00 | 2.00 | S200135 | 0.124 | 0.97 | 20 |
30 | 58 | 1.38 |
| ABR0007 | 2.00 |
4.00 | 2.00 | S200032 | 0.002 | 0.06 | 70 |
425 | 160 | 0.59 | ABR0008 |
90.00 |
92.00 | 2.00 | S200136 | 0.073 | 0.83 | 20 |
24 | 65 | 1.36 |
| ABR0007 | 4.00 |
6.00 | 2.00 | S200033 | 0.001 | 0.04 | 30 |
84 | 76 | 0.38 | ABR0008 |
92.00 |
94.00 | 2.00 | S200137 | 0.060 | 0.71 | 40 |
34 | 46 | 1.34 |
| ABR0007 | 6.00 |
8.00 | 2.00 | S200034 | 0.002 | 0.04 | 20 |
63 | 46 | 0.35 | ABR0008 |
94.00 |
96.00 | 2.00 | S200138 | 0.044 | 0.58 | 20 |
19 | 32 | 1.12 |
| ABR0007 | 8.00 |
10.00 | 2.00 |
S200035 | 0.002 | 0.04 | 10 |
51 | 27 | 0.43 | ABR0008 |
96.00 |
98.00 | 2.00 | S200139 | 0.045 | 0.54 | 30 |
20 | 39 | 1.11 |
| ABR0007 | 10.00 |
12.00 | 2.00 |
S200036 | 0.001 | 0.04 | 10 |
32 | 21 | 0.30 | ABR0008 |
98.00 |
100.00 | 2.00 |
S200140 | 0.188 | 0.55 | 10 |
19 | 46 | 0.54 |
| ABR0007 | 12.00 |
14.00 | 2.00 |
S200037 | 0.002 | 0.05 | 40 |
32 | 17 | 1.22 | ABR0008 |
100.00 | 102.00 | 2.00 |
S200142 | 0.224 | 0.47 | b.d. | 24 |
46 | 0.36 |
| ABR0007 | 14.00 |
16.00 | 2.00 |
S200038 | 0.001 | 0.04 | 50 |
26 | 14 | 1.31 | ABR0008 |
102.00 | 104.00 | 2.00 |
S200143 | 0.102 | 0.37 | 10 |
11 | 28 | 0.36 |
| ABR0007 | 16.00 |
18.00 | 2.00 |
S200039 | 0.005 | 0.13 | 50 |
37 | 50 | 1.10 | ABR0008 |
104.00 | 106.00 | 2.00 |
S200144 | 0.046 | 0.30 | 10 |
18 | 50 | 0.53 |
| ABR0007 | 18.00 |
20.00 | 2.00 |
S200041 | 0.007 | 0.13 | 50 |
62 | 113 | 1.08 | ABR0008 |
106.00 | 108.00 | 2.00 |
S200145 | 0.028 | 0.18 | 10 |
16 | 27 | 0.43 |
| ABR0007 | 20.00 |
22.00 | 2.00 |
S200042 | 0.009 | 0.14 | 50 |
90 | 154 | 0.92 | ABR0008 |
108.00 | 110.00 | 2.00 |
S200146 | 0.027 | 0.18 | 20 |
12 | 22 | 0.46 |
| ABR0007 | 22.00 |
24.00 | 2.00 |
S200043 | 0.011 | 0.15 | 30 |
59 | 113 | 1.16 | ABR0008 |
110.00 | 112.00 | 2.00 |
S200147 | 0.014 | 0.12 | 30 |
34 | 59 | 0.40 |
| ABR0007 | 24.00 |
26.00 | 2.00 |
S200044 | 0.013 | 0.19 | 50 |
53 | 63 | 1.04 | ABR0008 |
112.00 | 114.00 | 2.00 |
S200148 | 0.011 | 0.11 | 10 |
11 | 31 | 0.35 |
| ABR0007 | 26.00 |
28.00 | 2.00 |
S200045 | 0.013 | 0.29 | 60 |
31 | 48 | 1.23 | ABR0008 |
114.00 | 116.00 | 2.00 |
S200149 | 0.012 | 0.11 | 20 |
13 | 26 | 0.38 |
| ABR0007 | 28.00 |
30.00 | 2.00 |
S200046 | 0.021 | 0.31 | 60 |
37 | 57 | 0.73 | ABR0008 |
116.00 | 118.00 | 2.00 |
S200150 | 0.010 | 0.10 | 10 |
13 | 19 | 0.36 |
| ABR0007 | 30.00 |
32.00 | 2.00 |
S200047 | 0.038 | 0.34 | 30 |
136 | 98 | 0.70 | ABR0008 |
118.00 | 120.00 | 2.00 |
S200151 | 0.011 | 0.10 | 10 |
12 | 15 | 0.35 |
| ABR0007 | 32.00 |
34.00 | 2.00 |
S200048 | 0.031 | 0.40 | 40 |
135 | 106 | 0.64 | |||||||||||
| ABR0007 | 34.00 |
36.00 | 2.00 |
S200049 | 0.046 | 1.18 | 50 |
101 | 106 | 1.28 | ABR0009 |
0.00 |
2.00 | 2.00 | S200152 | 0.008 | 0.06 | 30 |
163 | 78 | 0.41 |
| ABR0007 | 36.00 |
38.00 | 2.00 |
S200050 | 0.030 | 0.89 | 10 |
39 | 66 | 0.85 | ABR0009 |
2.00 |
4.00 | 2.00 | S200153 | 0.003 | 0.04 | 20 |
109 | 61 | 0.51 |
| ABR0007 | 38.00 |
40.00 | 2.00 |
S200051 | 0.022 | 0.76 | 30 |
50 | 95 | 0.99 | ABR0009 |
4.00 |
6.00 | 2.00 | S200154 | 0.002 | 0.03 | 20 |
82 | 46 | 0.29 |
| ABR0007 | 40.00 |
42.00 | 2.00 |
S200052 | 0.174 | 1.12 | 10 |
62 | 100 | 1.01 | ABR0009 |
6.00 |
8.00 | 2.00 | S200155 | 0.001 | 0.02 | 20 |
55 | 29 | 0.30 |
18
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Cobalt, Scandium & PGM results from Black Range
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
Hole |
From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ABR0009 | 8.00 |
10.00 | 2.00 |
S200156 | 0.002 | 0.03 | 10 |
50 | 28 | 0.39 | ABR0011 |
32.00 |
34.00 | 2.00 | S200259 | 0.014 | 0.15 | 10 |
29 | 37 | 0.56 |
| ABR0009 | 10.00 |
12.00 | 2.00 |
S200157 | 0.002 | 0.03 | 10 |
46 | 23 | 0.53 | ABR0011 |
34.00 |
36.00 | 2.00 | S200260 | 0.012 | 0.15 | 10 |
20 | 27 | 0.54 |
| ABR0009 | 12.00 |
14.00 | 2.00 |
S200158 | 0.002 | 0.03 | b.d. | 34 |
21 | 0.56 | ABR0011 |
36.00 |
38.00 | 2.00 | S200262 | 0.013 | 0.16 | 10 |
21 | 29 | 0.55 |
| ABR0009 | 14.00 |
16.00 | 2.00 |
S200159 | 0.001 | 0.07 | 40 |
15 | 14 | 1.22 | ABR0011 |
38.00 |
40.00 | 2.00 | S200263 | 0.016 | 0.17 | 20 |
24 | 30 | 0.58 |
| ABR0009 | 16.00 |
18.00 | 2.00 |
S200161 | 0.002 | 0.06 | 60 |
17 | 34 | 1.33 | ABR0011 |
40.00 |
42.00 | 2.00 | S200264 | 0.015 | 0.17 | 20 |
25 | 37 | 0.57 |
| ABR0009 | 18.00 |
20.00 | 2.00 |
S200162 | 0.002 | 0.08 | 30 |
43 | 99 | 1.36 | ABR0011 |
42.00 |
44.00 | 2.00 | S200265 | 0.016 | 0.18 | 30 |
27 | 39 | 0.57 |
| ABR0009 | 20.00 |
22.00 | 2.00 |
S200163 | 0.006 | 0.07 | 20 |
32 | 93 | 1.44 | ABR0011 |
44.00 |
46.00 | 2.00 | S200266 | 0.013 | 0.16 | 20 |
24 | 40 | 0.60 |
| ABR0009 | 22.00 |
24.00 | 2.00 |
S200164 | 0.006 | 0.09 | 20 |
33 | 79 | 1.73 | ABR0011 |
46.00 |
48.00 | 2.00 | S200267 | 0.012 | 0.14 | 10 |
27 | 42 | 0.61 |
| ABR0009 | 24.00 |
26.00 | 2.00 |
S200165 | 0.005 | 0.17 | 50 |
70 | 70 | 1.36 | ABR0011 |
48.00 |
50.00 | 2.00 | S200268 | 0.013 | 0.14 | 10 |
50 | 51 | 0.61 |
| ABR0009 | 26.00 |
28.00 | 2.00 |
S200166 | 0.010 | 0.28 | 60 |
93 | 80 | 0.98 | ABR0011 |
50.00 |
52.00 | 2.00 | S200269 | 0.015 | 0.15 | 20 |
33 | 35 | 0.68 |
| ABR0009 | 28.00 |
30.00 | 2.00 |
S200167 | 0.009 | 0.24 | 30 |
45 | 72 | 0.72 | ABR0011 |
52.00 |
54.00 | 2.00 | S200270 | 0.015 | 0.15 | 20 |
24 | 30 | 0.61 |
| ABR0009 | 30.00 |
32.00 | 2.00 |
S200168 | 0.009 | 0.43 | 30 |
56 | 47 | 0.72 | ABR0011 |
54.00 |
56.00 | 2.00 | S200271 | 0.014 | 0.14 | 10 |
27 | 30 | 0.52 |
| ABR0009 | 32.00 |
34.00 | 2.00 |
S200169 | 0.055 | 0.54 | 40 |
168 | 133 | 0.73 | ABR0011 |
56.00 |
58.00 | 2.00 | S200272 | 0.007 | 0.09 | b.d. | 10 |
21 | 0.33 |
| ABR0009 | 34.00 |
36.00 | 2.00 |
S200170 | 0.169 | 0.60 | 40 |
90 | 117 | 0.67 | ABR0011 |
58.00 |
60.00 | 2.00 | S200273 | 0.008 | 0.10 | b.d. | 9 |
19 | 0.37 |
| ABR0009 | 36.00 |
38.00 | 2.00 |
S200171 | 0.096 | 0.75 | 40 |
42 | 68 | 1.65 | ABR0011 |
60.00 |
62.00 | 2.00 | S200274 | 0.007 | 0.08 | b.d. | 10 |
17 | 0.30 |
| ABR0009 | 38.00 |
40.00 | 2.00 |
S200172 | 0.095 | 0.92 | 30 |
50 | 86 | 1.46 | ABR0011 |
62.00 |
64.00 | 2.00 | S200275 | 0.013 | 0.11 | 20 |
23 | 26 | 0.41 |
| ABR0009 | 40.00 |
42.00 | 2.00 |
S200173 | 0.118 | 0.72 | 30 |
48 | 95 | 1.84 | ABR0011 |
64.00 |
66.00 | 2.00 | S200276 | 0.009 | 0.09 | 10 |
14 | 14 | 0.36 |
| ABR0009 | 42.00 |
44.00 | 2.00 |
S200174 | 0.127 | 1.09 | 20 |
31 | 50 | 1.37 | ABR0011 |
66.00 |
68.00 | 2.00 | S200277 | 0.012 | 0.11 | b.d. | 13 |
16 | 0.42 |
| ABR0009 | 44.00 |
46.00 | 2.00 |
S200175 | 0.093 | 1.30 | 20 |
28 | 50 | 1.28 | ABR0011 |
68.00 |
70.00 | 2.00 | S200278 | 0.012 | 0.11 | 10 |
18 | 19 | 0.44 |
| ABR0009 | 46.00 |
48.00 | 2.00 |
S200176 | 0.041 | 0.87 | 10 |
31 | 58 | 1.04 | ABR0011 |
70.00 |
72.00 | 2.00 | S200279 | 0.012 | 0.11 | 10 |
21 | 20 | 0.43 |
| ABR0009 | 48.00 |
50.00 | 2.00 |
S200177 | 0.033 | 0.50 | 20 |
29 | 48 | 0.94 | ABR0011 |
72.00 |
73.00 | 1.00 | S200281 | 0.008 | 0.10 | 10 |
32 | 27 | 0.39 |
| ABR0009 | 50.00 |
52.00 | 2.00 |
S200178 | 0.033 | 0.44 | 20 |
36 | 64 | 1.04 | |||||||||||
| ABR0009 | 52.00 |
54.00 | 2.00 |
S200179 | 0.020 | 0.33 | 20 |
34 | 68 | 0.85 | ABR0012 |
0.00 |
2.00 | 2.00 | S200282 | 0.040 | 0.26 | 30 |
141 | 214 | 0.55 |
| ABR0009 | 54.00 |
56.00 | 2.00 |
S200181 | 0.024 | 0.33 | 20 |
35 | 61 | 0.97 | ABR0012 |
2.00 |
4.00 | 2.00 | S200283 | 0.194 | 0.73 | 30 |
144 | 290 | 0.90 |
| ABR0009 | 56.00 |
58.00 | 2.00 |
S200182 | 0.018 | 0.25 | 10 |
25 | 47 | 1.05 | ABR0012 |
4.00 |
6.00 | 2.00 | S200284 | 0.154 | 0.73 | 40 |
134 | 322 | 1.20 |
| ABR0009 | 58.00 |
60.00 | 2.00 |
S200183 | 0.019 | 0.25 | 10 |
28 | 46 | 0.76 | ABR0012 |
6.00 |
8.00 | 2.00 | S200285 | 0.092 | 0.65 | 30 |
105 | 243 | 1.60 |
| ABR0009 | 60.00 |
62.00 | 2.00 |
S200184 | 0.015 | 0.18 | 10 |
26 | 46 | 0.62 | ABR0012 |
8.00 |
10.00 | 2.00 | S200286 | 0.052 | 0.60 | 30 |
60 | 137 | 1.68 |
| ABR0009 | 62.00 |
64.00 | 2.00 |
S200185 | 0.016 | 0.16 | 20 |
21 | 50 | 0.54 | ABR0012 |
10.00 |
12.00 | 2.00 | S200287 | 0.053 | 0.67 | 20 |
46 | 83 | 1.14 |
| ABR0009 | 64.00 |
66.00 | 2.00 |
S200186 | 0.013 | 0.16 | b.d. | 32 |
51 | 0.52 | ABR0012 |
12.00 |
14.00 | 2.00 | S200288 | 0.036 | 0.53 | 20 |
36 | 61 | 0.73 |
| ABR0009 | 66.00 |
68.00 | 2.00 |
S200187 | 0.015 | 0.16 | 10 |
23 | 40 | 0.51 | ABR0012 |
14.00 |
16.00 | 2.00 | S200289 | 0.020 | 0.32 | 20 |
31 | 46 | 0.77 |
| ABR0009 | 68.00 |
70.00 | 2.00 |
S200188 | 0.013 | 0.16 | b.d. | 42 |
73 | 0.56 | ABR0012 |
16.00 |
18.00 | 2.00 | S200290 | 0.015 | 0.19 | 10 |
26 | 42 | 0.57 |
| ABR0009 | 70.00 |
72.00 | 2.00 |
S200189 | 0.011 | 0.14 | 10 |
12 | 28 | 0.41 | ABR0012 |
18.00 |
20.00 | 2.00 | S200291 | 0.014 | 0.16 | b.d. | 25 |
43 | 0.52 |
| ABR0009 | 72.00 |
74.00 | 2.00 |
S200190 | 0.008 | 0.10 | b.d. | 19 |
43 | 0.32 | ABR0012 |
20.00 |
22.00 | 2.00 | S200292 | 0.012 | 0.13 | b.d. | 17 |
27 | 0.49 |
| ABR0009 | 74.00 |
76.00 | 2.00 |
S200191 | 0.013 | 0.13 | 10 |
16 | 26 | 0.44 | ABR0012 |
22.00 |
24.00 | 2.00 | S200293 | 0.010 | 0.12 | b.d. | 19 |
33 | 0.38 |
| ABR0009 | 76.00 |
78.00 | 2.00 |
S200192 | 0.011 | 0.12 | 10 |
12 | 32 | 0.40 | ABR0012 |
24.00 |
26.00 | 2.00 | S200294 | 0.013 | 0.15 | b.d. | 22 |
29 | 0.51 |
| ABR0009 | 78.00 |
80.00 | 2.00 |
S200193 | 0.013 | 0.13 | 20 |
57 | 30 | 0.45 | ABR0012 |
26.00 |
28.00 | 2.00 | S200295 | 0.014 | 0.15 | 10 |
20 | 29 | 0.55 |
| ABR0009 | 80.00 |
82.00 | 2.00 |
S200194 | 0.013 | 0.13 | 10 |
10 | 17 | 0.43 | ABR0012 |
28.00 |
30.00 | 2.00 | S200296 | 0.014 | 0.16 | 10 |
27 | 37 | 0.54 |
| ABR0009 | 82.00 |
84.00 | 2.00 |
S200195 | 0.012 | 0.12 | 20 |
10 | 21 | 0.43 | ABR0012 |
30.00 |
32.00 | 2.00 | S200297 | 0.013 | 0.15 | 10 |
22 | 38 | 0.52 |
| ABR0009 | 84.00 |
86.00 | 2.00 |
S200196 | 0.012 | 0.12 | 20 |
12 | 12 | 0.43 | ABR0012 |
32.00 |
34.00 | 2.00 | S200298 | 0.014 | 0.16 | 10 |
33 | 38 | 0.58 |
| ABR0009 | 86.00 |
88.00 | 2.00 |
S200197 | 0.013 | 0.12 | 20 |
17 | 19 | 0.43 | ABR0012 |
34.00 |
36.00 | 2.00 | S200299 | 0.015 | 0.15 | 10 |
25 | 41 | 0.56 |
| ABR0009 | 88.00 |
90.00 | 2.00 |
S200198 | 0.013 | 0.12 | 30 |
14 | 40 | 0.44 | ABR0012 |
36.00 |
38.00 | 2.00 | S200301 | 0.014 | 0.15 | 10 |
42 | 47 | 0.59 |
| ABR0009 | 90.00 |
91.00 | 1.00 |
S200199 | 0.012 | 0.12 | 20 |
10 | 26 | 0.44 | ABR0012 |
38.00 |
40.00 | 2.00 | S200302 | 0.014 | 0.14 | 10 |
35 | 39 | 0.59 |
| ABR0012 | 40.00 |
42.00 | 2.00 | S200303 | 0.010 | 0.10 | b.d. | 15 |
20 | 0.37 | |||||||||||
| ABR0010 | 0.00 |
2.00 | 2.00 | S200200 | 0.004 | 0.09 | 40 |
109 | 56 | 0.70 | ABR0012 |
42.00 |
44.00 | 2.00 | S200304 | 0.008 | 0.09 | b.d. | 15 |
20 | 0.31 |
| ABR0010 | 2.00 |
4.00 | 2.00 | S200202 | 0.001 | 0.05 | 30 |
84 | 49 | 0.75 | ABR0012 |
44.00 |
46.00 | 2.00 | S200305 | 0.008 | 0.08 | 10 |
16 | 21 | 0.30 |
| ABR0010 | 4.00 |
6.00 | 2.00 | S200203 | 0.002 | 0.11 | 20 |
54 | 57 | 1.18 | ABR0012 |
46.00 |
48.00 | 2.00 | S200306 | 0.006 | 0.08 | b.d. | 13 |
25 | 0.32 |
| ABR0010 | 6.00 |
8.00 | 2.00 | S200204 | 0.004 | 0.09 | 50 |
49 | 67 | 1.38 | ABR0012 |
48.00 |
50.00 | 2.00 | S200307 | 0.009 | 0.10 | b.d. | 20 |
23 | 0.38 |
| ABR0010 | 8.00 |
10.00 | 2.00 |
S200205 | 0.014 | 0.35 | 40 |
66 | 126 | 1.04 | ABR0012 |
50.00 |
52.00 | 2.00 | S200308 | 0.009 | 0.10 | b.d. | 13 |
15 | 0.36 |
| ABR0010 | 10.00 |
12.00 | 2.00 |
S200206 | 0.029 | 0.81 | 20 |
192 | 427 | 0.48 | ABR0012 |
52.00 |
54.00 | 2.00 | S200309 | 0.007 | 0.08 | b.d. | 15 |
23 | 0.30 |
| ABR0010 | 12.00 |
14.00 | 2.00 |
S200207 | 0.028 | 0.45 | 20 |
227 | 399 | 0.47 | ABR0012 |
54.00 |
56.00 | 2.00 | S200310 | 0.009 | 0.08 | b.d. | 15 |
28 | 0.29 |
| ABR0010 | 14.00 |
16.00 | 2.00 |
S200208 | 0.057 | 0.50 | 10 |
65 | 82 | 0.49 | ABR0012 |
56.00 |
58.00 | 2.00 | S200311 | 0.009 | 0.10 | 10 |
17 | 30 | 0.37 |
| ABR0010 | 16.00 |
18.00 | 2.00 |
S200209 | 0.054 | 0.48 | 10 |
66 | 64 | 0.49 | ABR0012 |
58.00 |
60.00 | 2.00 | S200312 | 0.010 | 0.11 | b.d. | 27 |
45 | 0.38 |
| ABR0010 | 18.00 |
20.00 | 2.00 |
S200210 | 0.029 | 0.31 | 30 |
57 | 50 | 0.44 | ABR0012 |
60.00 |
62.00 | 2.00 | S200313 | 0.008 | 0.09 | b.d. | 11 |
17 | 0.35 |
| ABR0010 | 20.00 |
22.00 | 2.00 |
S200211 | 0.019 | 0.19 | 10 |
59 | 47 | 0.45 | ABR0012 |
62.00 |
64.00 | 2.00 | S200314 | 0.007 | 0.08 | b.d. | 11 |
21 | 0.32 |
| ABR0010 | 22.00 |
24.00 | 2.00 |
S200212 | 0.011 | 0.14 | b.d. | 34 |
29 | 0.34 | ABR0012 |
64.00 |
66.00 | 2.00 | S200315 | 0.010 | 0.11 | b.d. | 34 |
18 | 0.40 |
| ABR0010 | 24.00 |
26.00 | 2.00 |
S200213 | 0.009 | 0.14 | b.d. | 22 |
27 | 0.35 | ABR0012 |
66.00 |
68.00 | 2.00 | S200316 | 0.012 | 0.12 | 10 |
12 | 18 | 0.44 |
| ABR0010 | 26.00 |
28.00 | 2.00 |
S200214 | 0.012 | 0.15 | 10 |
24 | 29 | 0.51 | ABR0012 |
68.00 |
70.00 | 2.00 | S200317 | 0.013 | 0.12 | 20 |
19 | 25 | 0.43 |
| ABR0010 | 28.00 |
30.00 | 2.00 |
S200215 | 0.013 | 0.16 | 10 |
32 | 37 | 0.52 | ABR0012 |
70.00 |
72.00 | 2.00 | S200318 | 0.012 | 0.12 | 10 |
22 | 28 | 0.45 |
| ABR0010 | 30.00 |
32.00 | 2.00 |
S200216 | 0.014 | 0.16 | 20 |
20 | 29 | 0.55 | ABR0012 |
72.00 |
73.00 | 1.00 | S200319 | 0.012 | 0.12 | 10 |
16 | 20 | 0.44 |
| ABR0010 | 32.00 |
34.00 | 2.00 |
S200217 | 0.016 | 0.16 | 20 |
22 | 28 | 0.55 | |||||||||||
| ABR0010 | 34.00 |
36.00 | 2.00 |
S200218 | 0.015 | 0.17 | 10 |
22 | 27 | 0.56 | ABR0013 |
0.00 |
2.00 | 2.00 | S200320 | 0.029 | 0.25 | 30 |
111 | 157 | 0.69 |
| ABR0010 | 36.00 |
38.00 | 2.00 |
S200219 | 0.016 | 0.17 | 20 |
20 | 21 | 0.54 | ABR0013 |
2.00 |
4.00 | 2.00 | S200322 | 0.072 | 0.59 | 70 |
175 | 201 | 1.19 |
| ABR0010 | 38.00 |
40.00 | 2.00 |
S200221 | 0.013 | 0.16 | 10 |
23 | 26 | 0.51 | ABR0013 |
4.00 |
6.00 | 2.00 | S200323 | 0.250 | 0.96 | 60 |
113 | 134 | 2.26 |
| ABR0010 | 40.00 |
42.00 | 2.00 |
S200222 | 0.015 | 0.16 | 20 |
23 | 25 | 0.54 | ABR0013 |
6.00 |
8.00 | 2.00 | S200324 | 0.284 | 0.82 | 50 |
93 | 168 | 1.82 |
| ABR0010 | 42.00 |
44.00 | 2.00 |
S200223 | 0.014 | 0.16 | 10 |
21 | 22 | 0.52 | ABR0013 |
8.00 |
10.00 | 2.00 | S200325 | 0.178 | 0.73 | 50 |
75 | 172 | 1.63 |
| ABR0010 | 44.00 |
46.00 | 2.00 |
S200224 | 0.015 | 0.16 | 10 |
20 | 23 | 0.53 | ABR0013 |
10.00 |
12.00 | 2.00 | S200326 | 0.208 | 0.76 | 40 |
64 | 140 | 1.58 |
| ABR0010 | 46.00 |
48.00 | 2.00 |
S200225 | 0.014 | 0.16 | 10 |
20 | 21 | 0.56 | ABR0013 |
12.00 |
14.00 | 2.00 | S200327 | 0.108 | 0.49 | 10 |
60 | 97 | 0.73 |
| ABR0010 | 48.00 |
50.00 | 2.00 |
S200226 | 0.015 | 0.16 | 10 |
23 | 23 | 0.55 | ABR0013 |
14.00 |
16.00 | 2.00 | S200328 | 0.048 | 0.30 | b.d. | 27 |
49 | 0.51 |
| ABR0010 | 50.00 |
52.00 | 2.00 |
S200227 | 0.013 | 0.16 | 10 |
19 | 22 | 0.58 | ABR0013 |
16.00 |
18.00 | 2.00 | S200329 | 0.026 | 0.37 | 20 |
37 | 59 | 0.62 |
| ABR0010 | 52.00 |
54.00 | 2.00 |
S200228 | 0.016 | 0.16 | 20 |
17 | 24 | 0.59 | ABR0013 |
18.00 |
20.00 | 2.00 | S200330 | 0.033 | 0.39 | 20 |
41 | 69 | 0.79 |
| ABR0010 | 54.00 |
56.00 | 2.00 |
S200229 | 0.018 | 0.17 | 30 |
27 | 34 | 0.58 | ABR0013 |
20.00 |
22.00 | 2.00 | S200331 | 0.019 | 0.27 | 20 |
25 | 45 | 0.74 |
| ABR0010 | 56.00 |
58.00 | 2.00 |
S200230 | 0.013 | 0.15 | 10 |
15 | 21 | 0.55 | ABR0013 |
22.00 |
24.00 | 2.00 | S200332 | 0.020 | 0.32 | 20 |
19 | 32 | 0.82 |
| ABR0010 | 58.00 |
60.00 | 2.00 |
S200231 | 0.012 | 0.16 | 10 |
16 | 18 | 0.60 | ABR0013 |
24.00 |
26.00 | 2.00 | S200333 | 0.019 | 0.31 | 10 |
36 | 69 | 0.70 |
| ABR0010 | 60.00 |
62.00 | 2.00 |
S200232 | 0.013 | 0.14 | 20 |
17 | 21 | 0.46 | ABR0013 |
26.00 |
28.00 | 2.00 | S200334 | 0.017 | 0.24 | 20 |
33 | 66 | 0.63 |
| ABR0010 | 62.00 |
64.00 | 2.00 |
S200233 | 0.008 | 0.10 | b.d. | 11 |
13 | 0.34 | ABR0013 |
28.00 |
30.00 | 2.00 | S200335 | 0.019 | 0.20 | 10 |
31 | 52 | 0.66 |
| ABR0010 | 64.00 |
66.00 | 2.00 |
S200234 | 0.010 | 0.10 | 20 |
12 | 11 | 0.36 | ABR0013 |
30.00 |
32.00 | 2.00 | S200336 | 0.016 | 0.17 | 10 |
25 | 39 | 0.57 |
| ABR0010 | 66.00 |
68.00 | 2.00 |
S200235 | 0.009 | 0.09 | 10 |
26 | 34 | 0.42 | ABR0013 |
32.00 |
34.00 | 2.00 | S200337 | 0.012 | 0.12 | 10 |
20 | 33 | 0.40 |
| ABR0010 | 68.00 |
70.00 | 2.00 |
S200236 | 0.009 | 0.10 | b.d. | 19 |
22 | 0.36 | ABR0013 |
34.00 |
36.00 | 2.00 | S200338 | 0.009 | 0.09 | 10 |
17 | 25 | 0.32 |
| ABR0010 | 70.00 |
72.00 | 2.00 |
S200237 | 0.012 | 0.12 | 10 |
23 | 16 | 0.44 | ABR0013 |
36.00 |
38.00 | 2.00 | S200339 | 0.011 | 0.11 | b.d. | 21 |
33 | 0.40 |
| ABR0010 | 72.00 |
74.00 | 2.00 |
S200238 | 0.012 | 0.12 | 20 |
18 | 16 | 0.45 | ABR0013 |
38.00 |
40.00 | 2.00 | S200341 | 0.009 | 0.10 | b.d. | 37 |
37 | 0.35 |
| ABR0010 | 74.00 |
76.00 | 2.00 |
S200239 | 0.013 | 0.12 | 10 |
14 | 21 | 0.44 | ABR0013 |
40.00 |
42.00 | 2.00 | S200342 | 0.009 | 0.09 | b.d. | 18 |
40 | 0.32 |
| ABR0010 | 76.00 |
78.00 | 2.00 |
S200241 | 0.013 | 0.12 | 20 |
22 | 27 | 0.45 | ABR0013 |
42.00 |
44.00 | 2.00 | S200343 | 0.009 | 0.09 | 10 |
14 | 23 | 0.33 |
| ABR0010 | 78.00 |
80.00 | 2.00 |
S200242 | 0.012 | 0.12 | 10 |
21 | 14 | 0.44 | ABR0013 |
44.00 |
46.00 | 2.00 | S200344 | 0.009 | 0.09 | b.d. | 12 |
23 | 0.29 |
| ABR0013 | 46.00 |
48.00 | 2.00 | S200345 | 0.007 | 0.08 | b.d. | 17 |
28 | 0.30 | |||||||||||
| ABR0011 | 0.00 |
2.00 | 2.00 | S200243 | 0.007 | 0.11 | 100 | 89 |
143 | 1.76 | ABR0013 |
48.00 |
50.00 | 2.00 | S200346 | 0.007 | 0.07 | b.d. | 19 |
24 | 0.24 |
| ABR0011 | 2.00 |
4.00 | 2.00 | S200244 | 0.006 | 0.10 | 80 |
93 | 150 | 1.47 | ABR0013 |
50.00 |
52.00 | 2.00 | S200347 | 0.007 | 0.08 | b.d. | 22 |
24 | 0.26 |
| ABR0011 | 4.00 |
6.00 | 2.00 | S200245 | 0.004 | 0.08 | 40 |
57 | 95 | 1.46 | ABR0013 |
52.00 |
54.00 | 2.00 | S200348 | 0.009 | 0.09 | b.d. | 18 |
28 | 0.29 |
| ABR0011 | 6.00 |
8.00 | 2.00 | S200246 | 0.005 | 0.07 | 50 |
48 | 81 | 1.50 | ABR0013 |
54.00 |
56.00 | 2.00 | S200349 | 0.009 | 0.09 | 10 |
14 | 27 | 0.28 |
| ABR0011 | 8.00 |
10.00 | 2.00 |
S200247 | 0.004 | 0.08 | 20 |
51 | 99 | 0.97 | ABR0013 |
56.00 |
58.00 | 2.00 | S200350 | 0.011 | 0.11 | b.d. | 14 |
28 | 0.37 |
| ABR0011 | 10.00 |
12.00 | 2.00 |
S200248 | 0.008 | 0.09 | 10 |
55 | 58 | 0.40 | ABR0013 |
58.00 |
60.00 | 2.00 | S200351 | 0.009 | 0.10 | b.d. | 10 |
25 | 0.34 |
| ABR0011 | 12.00 |
14.00 | 2.00 |
S200249 | 0.002 | 0.06 | b.d. | 18 |
20 | 0.23 | ABR0013 |
60.00 |
62.00 | 2.00 | S200352 | 0.014 | 0.13 | 20 |
25 | 34 | 0.45 |
| ABR0011 | 14.00 |
16.00 | 2.00 |
S200250 | 0.004 | 0.06 | b.d. | 155 |
167 | 0.21 | ABR0013 |
62.00 |
64.00 | 2.00 | S200353 | 0.013 | 0.12 | 20 |
19 | 38 | 0.43 |
| ABR0011 | 16.00 |
18.00 | 2.00 |
S200251 | 0.009 | 0.08 | 10 |
28 | 91 | 0.33 | ABR0013 |
64.00 |
66.00 | 2.00 | S200354 | 0.014 | 0.13 | 10 |
26 | 30 | 0.44 |
| ABR0011 | 18.00 |
20.00 | 2.00 |
S200252 | 0.008 | 0.10 | b.d. | 14 |
24 | 0.39 | ABR0013 |
66.00 |
68.00 | 2.00 | S200355 | 0.014 | 0.12 | 20 |
20 | 34 | 0.44 |
| ABR0011 | 20.00 |
22.00 | 2.00 |
S200253 | 0.009 | 0.10 | b.d. | 13 |
21 | 0.42 | ABR0013 |
68.00 |
70.00 | 2.00 | S200356 | 0.014 | 0.13 | 20 |
31 | 41 | 0.47 |
| ABR0011 | 22.00 |
24.00 | 2.00 |
S200254 | 0.006 | 0.09 | b.d. | 12 |
15 | 0.31 | ABR0013 |
70.00 |
72.00 | 2.00 | S200357 | 0.013 | 0.12 | 20 |
35 | 43 | 0.43 |
| ABR0011 | 24.00 |
26.00 | 2.00 |
S200255 | 0.007 | 0.10 | b.d. | 14 |
19 | 0.35 | ABR0013 |
72.00 |
73.00 | 1.00 | S200358 | 0.009 | 0.10 | b.d. | 21 |
32 | 0.30 |
| ABR0011 | 26.00 |
28.00 | 2.00 |
S200256 | 0.012 | 0.13 | 10 |
18 | 23 | 0.50 | |||||||||||
| ABR0011 | 28.00 |
30.00 | 2.00 |
S200257 | 0.013 | 0.13 | 30 |
21 | 30 | 0.53 | ABR0014 |
0.00 |
2.00 | 2.00 | S200359 | 0.040 | 0.17 | 30 |
86 | 72 | 0.42 |
| ABR0011 | 30.00 |
32.00 | 2.00 |
S200258 | 0.015 | 0.15 | 20 |
34 | 54 | 0.56 | ABR0014 |
2.00 |
4.00 | 2.00 | S200361 | 0.222 | 0.83 | 60 |
128 | 188 | 1.44 |
19
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Cobalt, Scandium & PGM results from Black Range
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
Hole |
From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ABR0014 | 4.00 |
6.00 | 2.00 | S200362 | 0.286 | 0.96 | 60 |
93 | 131 | 1.90 | ABR0017 |
12.00 |
14.00 | 2.00 | S200464 | 0.018 | 0.11 | 30 |
92 | 46 | 0.29 |
| ABR0014 | 6.00 |
8.00 | 2.00 | S200363 | 0.204 | 0.84 | 50 |
91 | 115 | 1.70 | ABR0017 |
14.00 |
16.00 | 2.00 | S200465 | 0.016 | 0.09 | 40 |
58 | 26 | 0.26 |
| ABR0014 | 8.00 |
10.00 | 2.00 |
S200364 | 0.102 | 0.86 | 70 |
107 | 158 | 1.39 | ABR0017 |
16.00 |
18.00 | 2.00 | S200466 | 0.011 | 0.06 | 40 |
58 | 25 | 0.26 |
| ABR0014 | 10.00 |
12.00 | 2.00 |
S200365 | 0.083 | 0.71 | 50 |
117 | 192 | 1.42 | ABR0017 |
18.00 |
20.00 | 2.00 | S200467 | 0.009 | 0.06 | 40 |
119 | 46 | 0.27 |
| ABR0014 | 12.00 |
14.00 | 2.00 |
S200366 | 0.057 | 0.56 | 20 |
57 | 102 | 0.87 | ABR0017 |
20.00 |
22.00 | 2.00 | S200468 | 0.009 | 0.07 | 40 |
117 | 40 | 0.28 |
| ABR0014 | 14.00 |
16.00 | 2.00 |
S200367 | 0.046 | 0.73 | 30 |
70 | 121 | 0.97 | ABR0017 |
22.00 |
24.00 | 2.00 | S200469 | 0.008 | 0.06 | 20 |
110 | 45 | 0.26 |
| ABR0014 | 16.00 |
18.00 | 2.00 |
S200368 | 0.023 | 0.52 | 30 |
39 | 101 | 0.93 | ABR0017 |
24.00 |
26.00 | 2.00 | S200470 | 0.008 | 0.06 | 30 |
137 | 50 | 0.26 |
| ABR0014 | 18.00 |
20.00 | 2.00 |
S200369 | 0.070 | 0.49 | 30 |
50 | 142 | 0.85 | ABR0017 |
26.00 |
28.00 | 2.00 | S200471 | 0.009 | 0.06 | 30 |
129 | 47 | 0.26 |
| ABR0014 | 20.00 |
22.00 | 2.00 |
S200370 | 0.079 | 0.40 | 40 |
127 | 157 | 1.09 | ABR0017 |
28.00 |
30.00 | 2.00 | S200472 | 0.008 | 0.07 | 40 |
108 | 70 | 0.26 |
| ABR0014 | 22.00 |
24.00 | 2.00 |
S200371 | 0.020 | 0.58 | 20 |
29 | 110 | 0.73 | ABR0017 |
30.00 |
32.00 | 2.00 | S200473 | 0.008 | 0.06 | 30 |
134 | 74 | 0.25 |
| ABR0014 | 24.00 |
26.00 | 2.00 |
S200372 | 0.017 | 0.26 | 10 |
51 | 80 | 0.62 | ABR0017 |
32.00 |
34.00 | 2.00 | S200474 | 0.008 | 0.06 | 40 |
162 | 74 | 0.24 |
| ABR0014 | 26.00 |
28.00 | 2.00 |
S200373 | 0.019 | 0.20 | 30 |
34 | 75 | 0.62 | ABR0017 |
34.00 |
36.00 | 2.00 | S200475 | 0.008 | 0.06 | 30 |
188 | 79 | 0.24 |
| ABR0014 | 28.00 |
30.00 | 2.00 |
S200374 | 0.013 | 0.13 | b.d. | 20 |
53 | 0.48 | ABR0017 |
36.00 |
38.00 | 2.00 | S200476 | 0.008 | 0.05 | 30 |
194 | 101 | 0.25 |
| ABR0014 | 30.00 |
32.00 | 2.00 |
S200375 | 0.013 | 0.11 | b.d. | 18 |
51 | 0.35 | ABR0017 |
38.00 |
40.00 | 2.00 | S200477 | 0.008 | 0.06 | 30 |
133 | 76 | 0.25 |
| ABR0014 | 32.00 |
34.00 | 2.00 |
S200376 | 0.012 | 0.11 | 10 |
28 | 46 | 0.34 | ABR0017 |
40.00 |
41.00 | 1.00 | S200478 | 0.008 | 0.06 | 40 |
148 | 79 | 0.26 |
| ABR0014 | 34.00 |
36.00 | 2.00 |
S200377 | 0.009 | 0.11 | 10 |
36 | 57 | 0.37 | |||||||||||
| ABR0014 | 36.00 |
38.00 | 2.00 |
S200378 | 0.009 | 0.10 | b.d. | 11 |
33 | 0.35 | ABR0018 |
0.00 |
2.00 | 2.00 | S200479 | 0.003 | 0.03 | 40 |
176 | 108 | 0.45 |
| ABR0014 | 38.00 |
40.00 | 2.00 |
S200379 | 0.009 | 0.11 | 10 |
11 | 27 | 0.32 | ABR0018 |
2.00 |
4.00 | 2.00 | S200481 | 0.006 | 0.08 | 20 |
153 | 122 | 0.82 |
| ABR0014 | 40.00 |
42.00 | 2.00 |
S200380 | 0.009 | 0.10 | b.d. | 16 |
24 | 0.32 | ABR0018 |
4.00 |
6.00 | 2.00 | S200482 | 0.006 | 0.11 | 30 |
126 | 85 | 1.10 |
| ABR0014 | 42.00 |
44.00 | 2.00 |
S200382 | 0.009 | 0.10 | b.d. | 20 |
25 | 0.38 | ABR0018 |
6.00 |
8.00 | 2.00 | S200483 | 0.008 | 0.15 | 20 |
157 | 85 | 1.00 |
| ABR0014 | 44.00 |
46.00 | 2.00 |
S200383 | 0.009 | 0.10 | 10 |
10 | 24 | 0.33 | ABR0018 |
8.00 |
10.00 | 2.00 | S200484 | 0.010 | 0.22 | 10 |
123 | 99 | 0.97 |
| ABR0014 | 46.00 |
48.00 | 2.00 |
S200384 | 0.010 | 0.10 | 10 |
13 | 29 | 0.35 | ABR0018 |
10.00 |
12.00 | 2.00 | S200485 | 0.023 | 0.28 | 20 |
146 | 147 | 0.88 |
| ABR0014 | 48.00 |
50.00 | 2.00 |
S200385 | 0.011 | 0.11 | 10 |
15 | 26 | 0.37 | ABR0018 |
12.00 |
14.00 | 2.00 | S200486 | 0.028 | 0.28 | 20 |
131 | 138 | 0.78 |
| ABR0014 | 50.00 |
52.00 | 2.00 |
S200386 | 0.009 | 0.11 | b.d. | 55 |
35 | 0.34 | ABR0018 |
14.00 |
16.00 | 2.00 | S200487 | 0.028 | 0.31 | 20 |
176 | 180 | 0.86 |
| ABR0014 | 52.00 |
54.00 | 2.00 |
S200387 | 0.014 | 0.16 | 10 |
24 | 40 | 0.46 | ABR0018 |
16.00 |
18.00 | 2.00 | S200488 | 0.072 | 0.38 | 30 |
182 | 136 | 0.74 |
| ABR0014 | 54.00 |
56.00 | 2.00 |
S200388 | 0.012 | 0.12 | 10 |
29 | 46 | 0.42 | ABR0018 |
18.00 |
20.00 | 2.00 | S200489 | 0.040 | 0.33 | 20 |
89 | 64 | 0.61 |
| ABR0014 | 56.00 |
58.00 | 2.00 |
S200389 | 0.013 | 0.12 | 10 |
27 | 51 | 0.42 | ABR0018 |
20.00 |
22.00 | 2.00 | S200490 | 0.020 | 0.23 | 30 |
37 | 33 | 0.57 |
| ABR0014 | 58.00 |
60.00 | 2.00 |
S200390 | 0.013 | 0.12 | 10 |
16 | 31 | 0.43 | ABR0018 |
22.00 |
24.00 | 2.00 | S200491 | 0.015 | 0.17 | 20 |
119 | 81 | 0.47 |
| ABR0014 | 60.00 |
61.00 | 1.00 |
S200391 | 0.014 | 0.12 | 10 |
29 | 29 | 0.45 | ABR0018 |
24.00 |
26.00 | 2.00 | S200492 | 0.014 | 0.18 | 30 |
166 | 106 | 0.48 |
| ABR0018 | 26.00 |
28.00 | 2.00 | S200493 | 0.018 | 0.18 | 20 |
157 | 116 | 0.47 | |||||||||||
| ABR0015 | 0.00 |
2.00 | 2.00 | S200392 | 0.006 | 0.11 | 70 |
349 | 381 | 0.47 | ABR0018 |
28.00 |
30.00 | 2.00 | S200494 | 0.016 | 0.16 | 20 |
117 | 103 | 0.49 |
| ABR0015 | 2.00 |
4.00 | 2.00 | S200393 | 0.004 | 0.12 | 80 |
285 | 320 | 0.54 | ABR0018 |
30.00 |
32.00 | 2.00 | S200495 | 0.020 | 0.19 | 20 |
98 | 86 | 0.58 |
| ABR0015 | 4.00 |
6.00 | 2.00 | S200394 | 0.005 | 0.14 | 110 | 360 |
410 | 0.55 | ABR0018 |
32.00 |
34.00 | 2.00 | S200496 | 0.015 | 0.15 | 10 |
85 | 67 | 0.51 |
| ABR0015 | 6.00 |
8.00 | 2.00 | S200395 | 0.008 | 0.17 | 170 | 349 |
406 | 0.61 | ABR0018 |
34.00 |
36.00 | 2.00 | S200497 | 0.019 | 0.19 | 10 |
117 | 131 | 0.57 |
| ABR0015 | 8.00 |
10.00 | 2.00 |
S200396 | 0.009 | 0.39 | 150 | 259 |
369 | 0.97 | ABR0018 |
36.00 |
38.00 | 2.00 | S200498 | 0.013 | 0.13 | 10 |
47 | 42 | 0.47 |
| ABR0015 | 10.00 |
12.00 | 2.00 |
S200397 | 0.012 | 0.45 | 90 |
248 | 344 | 1.25 | ABR0018 |
38.00 |
40.00 | 2.00 | S200499 | 0.015 | 0.15 | 10 |
53 | 44 | 0.51 |
| ABR0015 | 12.00 |
14.00 | 2.00 |
S200398 | 0.013 | 0.38 | 70 |
228 | 291 | 1.81 | ABR0018 |
40.00 |
41.00 | 1.00 | S200500 | 0.016 | 0.15 | 30 |
114 | 109 | 0.49 |
| ABR0015 | 14.00 |
16.00 | 2.00 |
S200399 | 0.009 | 0.43 | 70 |
203 | 315 | 2.19 | |||||||||||
| ABR0015 | 16.00 |
18.00 | 2.00 |
S200401 | 0.009 | 0.38 | 70 |
156 | 221 | 2.76 | ABR0019 |
0.00 |
2.00 | 2.00 | S200502 | 0.009 | 0.10 | 30 |
193 | 117 | 0.33 |
| ABR0015 | 18.00 |
20.00 | 2.00 |
S200402 | 0.011 | 0.37 | 60 |
166 | 207 | 2.63 | ABR0019 |
2.00 |
4.00 | 2.00 | S200503 | 0.008 | 0.10 | 20 |
294 | 160 | 0.29 |
| ABR0015 | 20.00 |
22.00 | 2.00 |
S200403 | 0.009 | 0.11 | 60 |
173 | 210 | 1.99 | ABR0019 |
4.00 |
6.00 | 2.00 | S200504 | 0.010 | 0.07 | 30 |
248 | 131 | 0.32 |
| ABR0015 | 22.00 |
24.00 | 2.00 |
S200404 | 0.009 | 0.10 | 70 |
321 | 280 | 1.57 | ABR0019 |
6.00 |
8.00 | 2.00 | S200505 | 0.011 | 0.08 | 30 |
200 | 138 | 0.31 |
| ABR0015 | 24.00 |
26.00 | 2.00 |
S200405 | 0.024 | 0.25 | 60 |
156 | 218 | 1.14 | ABR0019 |
8.00 |
10.00 | 2.00 | S200506 | 0.012 | 0.08 | 40 |
175 | 133 | 0.30 |
| ABR0015 | 26.00 |
28.00 | 2.00 |
S200406 | 0.056 | 0.31 | 50 |
161 | 201 | 0.96 | ABR0019 |
10.00 |
12.00 | 2.00 | S200507 | 0.011 | 0.07 | 30 |
183 | 109 | 0.27 |
| ABR0015 | 28.00 |
30.00 | 2.00 |
S200407 | 0.052 | 0.25 | 80 |
241 | 336 | 1.98 | ABR0019 |
12.00 |
14.00 | 2.00 | S200508 | 0.012 | 0.07 | 30 |
118 | 116 | 0.24 |
| ABR0015 | 30.00 |
32.00 | 2.00 |
S200408 | 0.184 | 0.35 | 70 |
219 | 326 | 1.79 | ABR0019 |
14.00 |
16.00 | 2.00 | S200509 | 0.010 | 0.07 | 20 |
152 | 124 | 0.28 |
| ABR0015 | 32.00 |
34.00 | 2.00 |
S200409 | 0.037 | 0.29 | 30 |
142 | 197 | 1.02 | ABR0019 |
16.00 |
18.00 | 2.00 | S200510 | 0.012 | 0.07 | 30 |
176 | 92 | 0.27 |
| ABR0015 | 34.00 |
36.00 | 2.00 |
S200410 | 0.031 | 0.30 | 30 |
202 | 175 | 0.85 | ABR0019 |
18.00 |
20.00 | 2.00 | S200511 | 0.009 | 0.07 | 30 |
144 | 91 | 0.29 |
| ABR0015 | 36.00 |
38.00 | 2.00 |
S200411 | 0.020 | 0.22 | 30 |
59 | 142 | 0.70 | ABR0019 |
20.00 |
22.00 | 2.00 | S200512 | 0.009 | 0.07 | 30 |
147 | 87 | 0.28 |
| ABR0015 | 38.00 |
40.00 | 2.00 |
S200412 | 0.013 | 0.13 | 10 |
51 | 86 | 0.46 | ABR0019 |
22.00 |
24.00 | 2.00 | S200513 | 0.010 | 0.07 | 40 |
133 | 106 | 0.28 |
| ABR0015 | 40.00 |
42.00 | 2.00 |
S200413 | 0.010 | 0.11 | 10 |
60 | 117 | 0.40 | ABR0019 |
24.00 |
26.00 | 2.00 | S200514 | 0.009 | 0.08 | 40 |
145 | 116 | 0.28 |
| ABR0015 | 42.00 |
44.00 | 2.00 |
S200414 | 0.010 | 0.11 | b.d. | 87 |
98 | 0.39 | ABR0019 |
26.00 |
28.00 | 2.00 | S200515 | 0.008 | 0.07 | 20 |
318 | 190 | 0.25 |
| ABR0015 | 44.00 |
46.00 | 2.00 |
S200415 | 0.009 | 0.09 | b.d. | 44 |
74 | 0.34 | ABR0019 |
28.00 |
30.00 | 2.00 | S200516 | 0.008 | 0.06 | 20 |
265 | 136 | 0.26 |
| ABR0015 | 46.00 |
48.00 | 2.00 |
S200416 | 0.009 | 0.10 | b.d. | 155 |
80 | 0.40 | ABR0019 |
30.00 |
32.00 | 2.00 | S200517 | 0.007 | 0.06 | 10 |
247 | 132 | 0.26 |
| ABR0015 | 48.00 |
50.00 | 2.00 |
S200417 | 0.011 | 0.11 | b.d. | 112 |
108 | 0.44 | ABR0019 |
32.00 |
34.00 | 2.00 | S200518 | 0.009 | 0.06 | 30 |
325 | 174 | 0.27 |
| ABR0015 | 50.00 |
52.00 | 2.00 |
S200418 | 0.010 | 0.11 | 10 |
68 | 124 | 0.42 | ABR0019 |
34.00 |
36.00 | 2.00 | S200519 | 0.008 | 0.06 | 30 |
255 | 115 | 0.26 |
| ABR0015 | 52.00 |
54.00 | 2.00 |
S200419 | 0.012 | 0.12 | 10 |
45 | 103 | 0.41 | ABR0019 |
36.00 |
38.00 | 2.00 | S200521 | 0.007 | 0.06 | 20 |
279 | 104 | 0.28 |
| ABR0015 | 54.00 |
56.00 | 2.00 |
S200421 | 0.00 | ABR0019 |
38.00 |
40.00 | 2.00 | S200522 | 0.007 | 0.06 | 20 |
271 | 108 | 0.29 | |||||
| ABR0015 | 56.00 |
58.00 | 2.00 |
S200422 | 0.013 | 0.12 | 10 |
59 | 95 | 0.44 | ABR0019 |
40.00 |
42.00 | 2.00 | S200523 | 0.007 | 0.07 | 20 |
265 | 121 | 0.28 |
| ABR0015 | 58.00 |
60.00 | 2.00 |
S200423 | 0.013 | 0.13 | 20 |
38 | 59 | 0.45 | ABR0019 |
42.00 |
44.00 | 2.00 | S200524 | 0.009 | 0.06 | 30 |
146 | 129 | 0.28 |
| ABR0015 | 60.00 |
62.00 | 2.00 |
S200424 | 0.014 | 0.13 | 20 |
65 | 59 | 0.44 | ABR0019 |
44.00 |
46.00 | 2.00 | S200525 | 0.009 | 0.06 | 30 |
143 | 118 | 0.28 |
| ABR0015 | 62.00 |
64.00 | 2.00 |
S200425 | 0.014 | 0.13 | 20 |
165 | 70 | 0.44 | ABR0019 |
46.00 |
48.00 | 2.00 | S200526 | 0.007 | 0.07 | 20 |
127 | 109 | 0.27 |
| ABR0015 | 64.00 |
66.00 | 2.00 |
S200426 | 0.013 | 0.12 | 20 |
34 | 51 | 0.43 | ABR0019 |
48.00 |
50.00 | 2.00 | S200527 | 0.008 | 0.07 | 20 |
137 | 105 | 0.27 |
| ABR0015 | 66.00 |
67.00 | 1.00 |
S200427 | 0.015 | 0.13 | 30 |
27 | 54 | 0.46 | ABR0019 |
50.00 |
52.00 | 2.00 | S200528 | 0.008 | 0.07 | 30 |
132 | 96 | 0.27 |
| ABR0019 | 52.00 |
54.00 | 2.00 | S200529 | 0.008 | 0.07 | 30 |
154 | 101 | 0.27 | |||||||||||
| ABR0016 | 0.00 |
2.00 | 2.00 | S200428 | 0.005 | 0.11 | 70 |
478 | 329 | 0.41 | |||||||||||
| ABR0016 | 2.00 |
4.00 | 2.00 | S200429 | 0.002 | 0.42 | 70 |
562 | 301 | 0.54 | ABR0020 |
0.00 |
2.00 | 2.00 | S200530 | 0.005 | 0.04 | 70 |
627 | 260 | 0.61 |
| ABR0016 | 4.00 |
6.00 | 2.00 | S200430 | 0.004 | 0.80 | 50 |
382 | 195 | 0.69 | ABR0020 |
2.00 |
4.00 | 2.00 | S200531 | 0.008 | 0.05 | 100 | 662 |
285 | 0.66 |
| ABR0016 | 6.00 |
8.00 | 2.00 | S200431 | 0.008 | 0.27 | 60 |
252 | 174 | 0.81 | ABR0020 |
4.00 |
6.00 | 2.00 | S200532 | 0.013 | 0.07 | 130 | 478 |
226 | 1.16 |
| ABR0016 | 8.00 |
10.00 | 2.00 |
S200432 | 0.051 | 0.32 | 50 |
219 | 127 | 1.01 | ABR0020 |
6.00 |
8.00 | 2.00 | S200533 | 0.009 | 0.09 | 60 |
178 | 118 | 0.65 |
| ABR0016 | 10.00 |
12.00 | 2.00 |
S200433 | 0.106 | 0.40 | 50 |
208 | 100 | 0.91 | ABR0020 |
8.00 |
10.00 | 2.00 | S200534 | 0.008 | 0.13 | 40 |
242 | 130 | 0.49 |
| ABR0016 | 12.00 |
14.00 | 2.00 |
S200434 | 0.120 | 0.55 | 40 |
90 | 60 | 0.86 | ABR0020 |
10.00 |
12.00 | 2.00 | S200535 | 0.009 | 0.09 | 40 |
436 | 267 | 0.65 |
| ABR0016 | 14.00 |
16.00 | 2.00 |
S200435 | 0.068 | 0.43 | 50 |
212 | 120 | 0.86 | ABR0020 |
12.00 |
14.00 | 2.00 | S200536 | 0.006 | 0.12 | 30 |
410 | 209 | 0.44 |
| ABR0016 | 16.00 |
18.00 | 2.00 |
S200436 | 0.028 | 0.43 | 50 |
175 | 89 | 0.74 | ABR0020 |
14.00 |
16.00 | 2.00 | S200537 | 0.008 | 0.13 | 30 |
319 | 150 | 0.45 |
| ABR0016 | 18.00 |
20.00 | 2.00 |
S200437 | 0.016 | 0.23 | 40 |
151 | 112 | 0.63 | ABR0020 |
16.00 |
18.00 | 2.00 | S200538 | 0.008 | 0.13 | 30 |
285 | 108 | 0.44 |
| ABR0016 | 20.00 |
22.00 | 2.00 |
S200438 | 0.013 | 0.14 | 30 |
110 | 71 | 0.40 | ABR0020 |
18.00 |
20.00 | 2.00 | S200539 | 0.008 | 0.14 | 40 |
289 | 90 | 0.47 |
| ABR0016 | 22.00 |
24.00 | 2.00 |
S200439 | 0.014 | 0.12 | 30 |
161 | 122 | 0.41 | ABR0020 |
20.00 |
22.00 | 2.00 | S200541 | 0.010 | 0.16 | 30 |
247 | 100 | 0.45 |
| ABR0016 | 24.00 |
26.00 | 2.00 |
S200440 | 0.013 | 0.11 | 30 |
138 | 100 | 0.35 | ABR0020 |
22.00 |
24.00 | 2.00 | S200542 | 0.028 | 0.20 | 30 |
168 | 74 | 0.46 |
| ABR0016 | 26.00 |
28.00 | 2.00 |
S200442 | 0.009 | 0.11 | 30 |
287 | 142 | 0.29 | ABR0020 |
24.00 |
26.00 | 2.00 | S200543 | 0.030 | 0.16 | 30 |
131 | 80 | 0.42 |
| ABR0016 | 28.00 |
30.00 | 2.00 |
S200443 | 0.009 | 0.09 | 30 |
134 | 92 | 0.29 | ABR0020 |
26.00 |
28.00 | 2.00 | S200544 | 0.019 | 0.13 | 40 |
117 | 74 | 0.40 |
| ABR0016 | 30.00 |
32.00 | 2.00 |
S200444 | 0.009 | 0.08 | 30 |
88 | 50 | 0.29 | ABR0020 |
28.00 |
30.00 | 2.00 | S200545 | 0.017 | 0.14 | 40 |
103 | 68 | 0.45 |
| ABR0016 | 32.00 |
34.00 | 2.00 |
S200445 | 0.009 | 0.08 | 30 |
164 | 95 | 0.28 | ABR0020 |
30.00 |
32.00 | 2.00 | S200546 | 0.013 | 0.12 | 40 |
105 | 94 | 0.36 |
| ABR0016 | 34.00 |
36.00 | 2.00 |
S200446 | 0.010 | 0.09 | 40 |
96 | 57 | 0.32 | ABR0020 |
32.00 |
34.00 | 2.00 | S200547 | 0.011 | 0.12 | 30 |
87 | 80 | 0.33 |
| ABR0016 | 36.00 |
38.00 | 2.00 |
S200447 | 0.011 | 0.10 | 20 |
45 | 35 | 0.33 | ABR0020 |
34.00 |
36.00 | 2.00 | S200548 | 0.010 | 0.10 | 20 |
81 | 65 | 0.37 |
| ABR0016 | 38.00 |
40.00 | 2.00 |
S200448 | 0.010 | 0.12 | 30 |
142 | 79 | 0.29 | ABR0020 |
36.00 |
38.00 | 2.00 | S200549 | 0.009 | 0.10 | 20 |
150 | 131 | 0.40 |
| ABR0016 | 40.00 |
42.00 | 2.00 |
S200449 | 0.009 | 0.10 | 30 |
117 | 75 | 0.30 | ABR0020 |
38.00 |
40.00 | 2.00 | S200550 | 0.009 | 0.09 | 30 |
122 | 123 | 0.35 |
| ABR0016 | 42.00 |
44.00 | 2.00 |
S200450 | 0.015 | 0.13 | 20 |
70 | 178 | 0.44 | ABR0020 |
40.00 |
42.00 | 2.00 | S200551 | 0.009 | 0.11 | 20 |
69 | 69 | 0.31 |
| ABR0016 | 44.00 |
46.00 | 2.00 |
S200451 | 0.011 | 0.10 | 20 |
95 | 74 | 0.34 | ABR0020 |
42.00 |
44.00 | 2.00 | S200552 | 0.009 | 0.09 | 40 |
80 | 65 | 0.32 |
| ABR0016 | 46.00 |
48.00 | 2.00 |
S200452 | 0.008 | 0.09 | 30 |
86 | 63 | 0.30 | ABR0020 |
44.00 |
46.00 | 2.00 | S200553 | 0.016 | 0.16 | 20 |
84 | 67 | 0.53 |
| ABR0016 | 48.00 |
50.00 | 2.00 |
S200453 | 0.011 | 0.11 | 20 |
144 | 74 | 0.38 | ABR0020 |
46.00 |
48.00 | 2.00 | S200554 | 0.010 | 0.11 | 30 |
98 | 62 | 0.27 |
| ABR0016 | 50.00 |
52.00 | 2.00 |
S200454 | 0.009 | 0.12 | b.d. | 54 |
56 | 0.38 | ABR0020 |
48.00 |
50.00 | 2.00 | S200555 | 0.009 | 0.09 | 30 |
91 | 65 | 0.29 |
| ABR0016 | 52.00 |
54.00 | 2.00 |
S200455 | 0.012 | 0.12 | 20 |
54 | 49 | 0.41 | ABR0020 |
50.00 |
52.00 | 2.00 | S200556 | 0.007 | 0.07 | 30 |
62 | 80 | 0.29 |
| ABR0016 | 54.00 |
55.00 | 1.00 |
S200456 | 0.012 | 0.13 | 10 |
66 | 68 | 0.42 | ABR0020 |
52.00 |
54.00 | 2.00 | S200557 | 0.009 | 0.11 | 30 |
148 | 101 | 0.32 |
| ABR0020 | 54.00 |
55.00 | 1.00 | S200558 | 0.013 | 0.12 | 30 |
86 | 65 | 0.42 | |||||||||||
| ABR0017 | 0.00 |
2.00 | 2.00 | S200457 | 0.011 | 0.09 | 30 |
180 | 83 | 0.34 | |||||||||||
| ABR0017 | 2.00 |
4.00 | 2.00 | S200458 | 0.008 | 0.09 | 40 |
169 | 102 | 0.50 | ABR0021 |
0.00 |
2.00 | 2.00 | S200559 | 0.006 | 0.03 | 30 |
161 | 65 | 0.69 |
| ABR0017 | 4.00 |
6.00 | 2.00 | S200459 | 0.006 | 0.07 | 30 |
137 | 92 | 0.42 | ABR0021 |
2.00 |
4.00 | 2.00 | S200560 | 0.002 | 0.03 | 20 |
281 | 89 | 0.29 |
| ABR0017 | 6.00 |
8.00 | 2.00 | S200461 | 0.006 | 0.09 | 30 |
128 | 67 | 0.48 | ABR0021 |
4.00 |
6.00 | 2.00 | S200562 | 0.004 | 0.05 | 60 |
521 | 125 | 0.44 |
| ABR0017 | 8.00 |
10.00 | 2.00 |
S200462 | 0.006 | 0.08 | 30 |
137 | 65 | 0.54 | ABR0021 |
6.00 |
8.00 | 2.00 | S200563 | 0.008 | 0.07 | 150 | 461 |
116 | 0.45 |
| ABR0017 | 10.00 |
12.00 | 2.00 |
S200463 | 0.010 | 0.07 | 40 |
116 | 60 | 0.37 | ABR0021 |
8.00 |
10.00 | 2.00 | S200564 | 0.006 | 0.10 | 120 | 364 |
139 | 0.47 |
20
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
Cobalt, Scandium & PGM results from Black Range
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
Hole |
From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ABR0021 | 10.00 |
12.00 | 2.00 |
S200565 | 0.007 | 0.10 | 110 | 373 |
238 | 0.41 | ABR0023 |
58.00 |
60.00 | 2.00 | S200667 | 0.008 | 0.10 | b.d. | 15 |
29 | 0.33 |
| ABR0021 | 12.00 |
14.00 | 2.00 |
S200566 | 0.009 | 0.11 | 80 |
368 | 415 | 0.54 | ABR0023 |
60.00 |
62.00 | 2.00 | S200668 | 0.009 | 0.10 | b.d. | 13 |
35 | 0.36 |
| ABR0021 | 14.00 |
16.00 | 2.00 |
S200567 | 0.005 | 0.12 | 70 |
365 | 455 | 0.54 | ABR0023 |
62.00 |
64.00 | 2.00 | S200669 | 0.010 | 0.10 | 10 |
23 | 34 | 0.37 |
| ABR0021 | 16.00 |
18.00 | 2.00 |
S200568 | 0.007 | 0.26 | 70 |
361 | 396 | 0.65 | ABR0023 |
64.00 |
66.00 | 2.00 | S200670 | 0.007 | 0.08 | b.d. | 12 |
23 | 0.29 |
| ABR0021 | 18.00 |
20.00 | 2.00 |
S200569 | 0.006 | 0.28 | 70 |
303 | 343 | 0.43 | ABR0023 |
66.00 |
68.00 | 2.00 | S200671 | 0.009 | 0.09 | 10 |
14 | 24 | 0.30 |
| ABR0021 | 20.00 |
22.00 | 2.00 |
S200570 | 0.011 | 0.33 | 60 |
274 | 323 | 1.37 | ABR0023 |
68.00 |
70.00 | 2.00 | S200672 | 0.010 | 0.10 | b.d. | 29 |
32 | 0.36 |
| ABR0021 | 22.00 |
24.00 | 2.00 |
S200571 | 0.019 | 0.36 | 50 |
266 | 390 | 1.67 | ABR0023 |
70.00 |
72.00 | 2.00 | S200673 | 0.009 | 0.09 | b.d. | 14 |
24 | 0.33 |
| ABR0021 | 24.00 |
26.00 | 2.00 |
S200572 | 0.014 | 0.38 | 30 |
177 | 307 | 0.98 | ABR0023 |
72.00 |
74.00 | 2.00 | S200674 | 0.014 | 0.13 | 10 |
39 | 109 | 0.46 |
| ABR0021 | 26.00 |
28.00 | 2.00 |
S200573 | 0.015 | 0.39 | 30 |
102 | 157 | 0.88 | ABR0023 |
74.00 |
76.00 | 2.00 | S200675 | 0.012 | 0.12 | 10 |
16 | 27 | 0.43 |
| ABR0021 | 28.00 |
30.00 | 2.00 |
S200574 | 0.021 | 0.43 | 20 |
88 | 137 | 0.79 | ABR0023 |
76.00 |
78.00 | 2.00 | S200676 | 0.015 | 0.13 | 10 |
19 | 27 | 0.46 |
| ABR0021 | 30.00 |
32.00 | 2.00 |
S200575 | 0.034 | 0.38 | 20 |
81 | 121 | 0.68 | ABR0023 |
78.00 |
79.00 | 1.00 | S200677 | 0.013 | 0.13 | b.d. | 21 |
28 | 0.48 |
| ABR0021 | 32.00 |
34.00 | 2.00 |
S200576 | 0.070 | 0.36 | 20 |
117 | 135 | 0.62 | |||||||||||
| ABR0021 | 34.00 |
36.00 | 2.00 |
S200577 | 0.042 | 0.30 | 10 |
77 | 117 | 0.56 | ABR0024 |
0.00 |
2.00 | 2.00 | S200678 | 0.005 | 0.06 | 10 |
109 | 82 | 0.96 |
| ABR0021 | 36.00 |
38.00 | 2.00 |
S200578 | 0.042 | 0.29 | 30 |
99 | 155 | 0.57 | ABR0024 |
2.00 |
4.00 | 2.00 | S200679 | 0.005 | 0.14 | 50 |
57 | 46 | 1.12 |
| ABR0021 | 38.00 |
40.00 | 2.00 |
S200579 | 0.028 | 0.22 | 20 |
115 | 211 | 0.56 | ABR0024 |
4.00 |
6.00 | 2.00 | S200680 | 0.007 | 0.20 | 50 |
37 | 37 | 1.19 |
| ABR0021 | 40.00 |
42.00 | 2.00 |
S200581 | 0.023 | 0.20 | 20 |
113 | 194 | 0.63 | ABR0024 |
6.00 |
8.00 | 2.00 | S200682 | 0.010 | 0.22 | 30 |
45 | 57 | 1.14 |
| ABR0021 | 42.00 |
44.00 | 2.00 |
S200582 | 0.015 | 0.15 | 20 |
135 | 254 | 0.53 | ABR0024 |
8.00 |
10.00 | 2.00 | S200683 | 0.017 | 0.30 | 50 |
40 | 60 | 1.25 |
| ABR0021 | 44.00 |
46.00 | 2.00 |
S200583 | 0.012 | 0.11 | 30 |
406 | 476 | 0.44 | ABR0024 |
10.00 |
12.00 | 2.00 | S200684 | 0.014 | 0.29 | 40 |
73 | 112 | 1.38 |
| ABR0021 | 46.00 |
48.00 | 2.00 |
S200584 | 0.016 | 0.16 | 10 |
82 | 127 | 0.65 | ABR0024 |
12.00 |
14.00 | 2.00 | S200685 | 0.017 | 0.39 | 20 |
64 | 146 | 0.78 |
| ABR0021 | 48.00 |
50.00 | 2.00 |
S200585 | 0.016 | 0.16 | 10 |
84 | 121 | 0.59 | ABR0024 |
14.00 |
16.00 | 2.00 | S200686 | 0.016 | 0.44 | 10 |
44 | 82 | 0.64 |
| ABR0021 | 50.00 |
52.00 | 2.00 |
S200586 | 0.015 | 0.15 | 20 |
69 | 164 | 0.63 | ABR0024 |
16.00 |
18.00 | 2.00 | S200687 | 0.025 | 0.49 | 10 |
43 | 42 | 0.60 |
| ABR0021 | 52.00 |
54.00 | 2.00 |
S200587 | 0.016 | 0.16 | 10 |
49 | 124 | 0.59 | ABR0024 |
18.00 |
20.00 | 2.00 | S200688 | 0.095 | 0.59 | 20 |
30 | 39 | 0.55 |
| ABR0021 | 54.00 |
56.00 | 2.00 |
S200588 | 0.018 | 0.16 | 20 |
79 | 143 | 0.61 | ABR0024 |
20.00 |
22.00 | 2.00 | S200689 | 0.059 | 0.50 | 10 |
20 | 27 | 0.48 |
| ABR0021 | 56.00 |
58.00 | 2.00 |
S200589 | 0.018 | 0.16 | 20 |
175 | 192 | 0.65 | ABR0024 |
22.00 |
24.00 | 2.00 | S200690 | 0.024 | 0.35 | b.d. | 16 |
25 | 0.44 |
| ABR0021 | 58.00 |
60.00 | 2.00 |
S200590 | 0.013 | 0.15 | 10 |
72 | 243 | 0.61 | ABR0024 |
24.00 |
26.00 | 2.00 | S200691 | 0.015 | 0.19 | b.d. | 17 |
24 | 0.44 |
| ABR0021 | 60.00 |
62.00 | 2.00 |
S200591 | 0.015 | 0.16 | 20 |
148 | 173 | 0.57 | ABR0024 |
26.00 |
28.00 | 2.00 | S200692 | 0.015 | 0.16 | 10 |
30 | 37 | 0.52 |
| ABR0021 | 62.00 |
64.00 | 2.00 |
S200592 | 0.019 | 0.15 | 10 |
114 | 96 | 0.60 | ABR0024 |
28.00 |
30.00 | 2.00 | S200693 | 0.016 | 0.17 | 10 |
25 | 33 | 0.54 |
| ABR0021 | 64.00 |
66.00 | 2.00 |
S200593 | 0.016 | 0.15 | 20 |
76 | 81 | 0.49 | ABR0024 |
30.00 |
32.00 | 2.00 | S200694 | 0.016 | 0.17 | 20 |
23 | 40 | 0.52 |
| ABR0021 | 66.00 |
68.00 | 2.00 |
S200594 | 0.013 | 0.13 | 20 |
128 | 142 | 0.42 | ABR0024 |
32.00 |
34.00 | 2.00 | S200695 | 0.014 | 0.17 | b.d. | 26 |
40 | 0.53 |
| ABR0021 | 68.00 |
70.00 | 2.00 |
S200595 | 0.011 | 0.11 | 10 |
36 | 56 | 0.40 | ABR0024 |
34.00 |
36.00 | 2.00 | S200696 | 0.015 | 0.16 | 10 |
36 | 38 | 0.55 |
| ABR0021 | 70.00 |
72.00 | 2.00 |
S200596 | 0.012 | 0.11 | 10 |
32 | 57 | 0.40 | ABR0024 |
36.00 |
38.00 | 2.00 | S200697 | 0.015 | 0.17 | 10 |
19 | 38 | 0.56 |
| ABR0021 | 72.00 |
73.00 | 1.00 |
S200597 | 0.012 | 0.12 | 20 |
53 | 68 | 0.43 | ABR0024 |
38.00 |
40.00 | 2.00 | S200698 | 0.015 | 0.16 | 10 |
21 | 38 | 0.58 |
| ABR0024 | 40.00 |
42.00 | 2.00 | S200699 | 0.015 | 0.15 | 10 |
120 | 44 | 0.56 | |||||||||||
| ABR0022 | 0.00 |
2.00 | 2.00 | S200598 | 0.005 | 0.13 | 80 |
209 | 236 | 1.02 | ABR0024 |
42.00 |
44.00 | 2.00 | S200701 | 0.015 | 0.15 | 10 |
25 | 37 | 0.55 |
| ABR0022 | 2.00 |
4.00 | 2.00 | S200599 | 0.005 | 0.19 | 80 |
264 | 282 | 0.95 | ABR0024 |
44.00 |
46.00 | 2.00 | S200702 | 0.016 | 0.16 | 20 |
23 | 27 | 0.56 |
| ABR0022 | 4.00 |
6.00 | 2.00 | S200601 | 0.055 | 0.22 | 70 |
343 | 451 | 0.89 | ABR0024 |
46.00 |
48.00 | 2.00 | S200703 | 0.016 | 0.16 | 10 |
24 | 33 | 0.54 |
| ABR0022 | 6.00 |
8.00 | 2.00 | S200602 | 0.043 | 0.28 | 70 |
213 | 378 | 1.16 | ABR0024 |
48.00 |
50.00 | 2.00 | S200704 | 0.014 | 0.15 | 10 |
22 | 31 | 0.57 |
| ABR0022 | 8.00 |
10.00 | 2.00 |
S200603 | 0.027 | 0.31 | 70 |
220 | 469 | 0.97 | ABR0024 |
50.00 |
52.00 | 2.00 | S200705 | 0.014 | 0.15 | 10 |
21 | 34 | 0.55 |
| ABR0022 | 10.00 |
12.00 | 2.00 |
S200604 | 0.024 | 0.53 | 60 |
126 | 249 | 1.13 | ABR0024 |
52.00 |
54.00 | 2.00 | S200706 | 0.016 | 0.16 | 30 |
25 | 35 | 0.63 |
| ABR0022 | 12.00 |
14.00 | 2.00 |
S200605 | 0.024 | 0.61 | 60 |
126 | 336 | 1.02 | ABR0024 |
54.00 |
56.00 | 2.00 | S200707 | 0.015 | 0.14 | 20 |
35 | 45 | 0.55 |
| ABR0022 | 14.00 |
16.00 | 2.00 |
S200606 | 0.117 | 0.60 | 60 |
165 | 338 | 1.00 | ABR0024 |
56.00 |
58.00 | 2.00 | S200708 | 0.014 | 0.14 | 10 |
32 | 41 | 0.46 |
| ABR0022 | 16.00 |
18.00 | 2.00 |
S200607 | 0.369 | 0.82 | 60 |
228 | 297 | 1.08 | ABR0024 |
58.00 |
60.00 | 2.00 | S200709 | 0.016 | 0.13 | 10 |
40 | 39 | 0.48 |
| ABR0022 | 18.00 |
20.00 | 2.00 |
S200608 | 0.308 | 1.12 | 70 |
224 | 181 | 1.37 | ABR0024 |
60.00 |
62.00 | 2.00 | S200710 | 0.015 | 0.16 | b.d. | 18 |
28 | 0.45 |
| ABR0022 | 20.00 |
22.00 | 2.00 |
S200609 | 0.386 | 1.14 | 50 |
135 | 285 | 1.08 | ABR0024 |
62.00 |
64.00 | 2.00 | S200711 | 0.008 | 0.11 | 10 |
12 | 20 | 0.36 |
| ABR0022 | 22.00 |
24.00 | 2.00 |
S200610 | 0.144 | 0.86 | 60 |
89 | 219 | 1.04 | ABR0024 |
64.00 |
66.00 | 2.00 | S200712 | 0.009 | 0.09 | b.d. | 10 |
16 | 0.30 |
| ABR0022 | 24.00 |
26.00 | 2.00 |
S200611 | 0.088 | 0.69 | 60 |
75 | 124 | 1.69 | ABR0024 |
66.00 |
68.00 | 2.00 | S200713 | 0.007 | 0.10 | b.d. | 19 |
22 | 0.34 |
| ABR0022 | 26.00 |
28.00 | 2.00 |
S200612 | 0.028 | 0.70 | 50 |
131 | 104 | 2.95 | ABR0024 |
68.00 |
70.00 | 2.00 | S200714 | 0.009 | 0.11 | 10 |
13 | 26 | 0.38 |
| ABR0022 | 28.00 |
30.00 | 2.00 |
S200613 | 0.045 | 0.62 | 30 |
64 | 123 | 1.70 | ABR0024 |
70.00 |
72.00 | 2.00 | S200715 | 0.013 | 0.12 | 10 |
15 | 23 | 0.44 |
| ABR0022 | 30.00 |
32.00 | 2.00 |
S200614 | 0.028 | 0.50 | 10 |
87 | 112 | 0.77 | ABR0024 |
72.00 |
74.00 | 2.00 | S200716 | 0.011 | 0.11 | b.d. | 16 |
21 | 0.41 |
| ABR0022 | 32.00 |
34.00 | 2.00 |
S200615 | 0.049 | 0.60 | 10 |
39 | 111 | 0.63 | |||||||||||
| ABR0022 | 34.00 |
36.00 | 2.00 |
S200616 | 0.039 | 0.54 | 10 |
40 | 94 | 0.62 | ABR0025 |
0.00 |
2.00 | 2.00 | S200717 | 0.002 | 0.05 | b.d. | 51 |
38 | 0.32 |
| ABR0022 | 36.00 |
38.00 | 2.00 |
S200617 | 0.022 | 0.42 | 20 |
31 | 85 | 0.53 | ABR0025 |
2.00 |
4.00 | 2.00 | S200718 | 0.001 | 0.28 | b.d. | 127 |
41 | 0.66 |
| ABR0022 | 38.00 |
40.00 | 2.00 |
S200618 | 0.019 | 0.35 | 20 |
44 | 105 | 0.68 | ABR0025 |
4.00 |
6.00 | 2.00 | S200719 | b.d. | 0.02 | b.d. | 83 |
29 | 0.59 |
| ABR0022 | 40.00 |
42.00 | 2.00 |
S200619 | 0.021 | 0.25 | 10 |
50 | 145 | 0.65 | ABR0025 |
6.00 |
8.00 | 2.00 | S200721 | 0.002 | 0.03 | 20 |
58 | 37 | 0.40 |
| ABR0022 | 42.00 |
44.00 | 2.00 |
S200620 | 0.019 | 0.22 | 10 |
60 | 94 | 0.62 | ABR0025 |
8.00 |
10.00 | 2.00 | S200722 | 0.002 | 0.04 | 20 |
57 | 45 | 0.76 |
| ABR0022 | 44.00 |
46.00 | 2.00 |
S200622 | 0.019 | 0.17 | 10 |
34 | 96 | 0.71 | ABR0025 |
10.00 |
12.00 | 2.00 | S200723 | 0.004 | 0.09 | b.d. | 17 |
19 | 1.34 |
| ABR0022 | 46.00 |
48.00 | 2.00 |
S200623 | 0.018 | 0.19 | 10 |
56 | 71 | 0.62 | ABR0025 |
12.00 |
14.00 | 2.00 | S200724 | 0.005 | 0.16 | 40 |
21 | 25 | 1.35 |
| ABR0022 | 48.00 |
50.00 | 2.00 |
S200624 | 0.019 | 0.19 | 10 |
50 | 112 | 0.60 | ABR0025 |
14.00 |
16.00 | 2.00 | S200725 | 0.006 | 0.15 | 40 |
37 | 41 | 1.49 |
| ABR0022 | 50.00 |
52.00 | 2.00 |
S200625 | 0.016 | 0.17 | 10 |
43 | 108 | 0.57 | ABR0025 |
16.00 |
18.00 | 2.00 | S200726 | 0.008 | 0.16 | 40 |
62 | 87 | 1.34 |
| ABR0022 | 52.00 |
54.00 | 2.00 |
S200626 | 0.016 | 0.16 | 10 |
52 | 155 | 0.52 | ABR0025 |
18.00 |
20.00 | 2.00 | S200727 | 0.014 | 0.23 | 60 |
80 | 162 | 1.16 |
| ABR0022 | 54.00 |
56.00 | 2.00 |
S200627 | 0.016 | 0.16 | 10 |
39 | 102 | 0.54 | ABR0025 |
20.00 |
22.00 | 2.00 | S200728 | 0.009 | 0.24 | 50 |
100 | 242 | 1.19 |
| ABR0022 | 56.00 |
58.00 | 2.00 |
S200628 | 0.016 | 0.17 | 10 |
36 | 66 | 0.60 | ABR0025 |
22.00 |
24.00 | 2.00 | S200729 | 0.010 | 0.26 | 60 |
136 | 196 | 1.90 |
| ABR0022 | 58.00 |
60.00 | 2.00 |
S200629 | 0.012 | 0.14 | 20 |
27 | 44 | 0.41 | ABR0025 |
24.00 |
26.00 | 2.00 | S200730 | 0.011 | 0.30 | 20 |
73 | 119 | 1.89 |
| ABR0022 | 60.00 |
62.00 | 2.00 |
S200630 | 0.008 | 0.10 | b.d. | 24 |
33 | 0.32 | ABR0025 |
26.00 |
28.00 | 2.00 | S200731 | 0.040 | 0.62 | b.d. | 75 |
74 | 1.44 |
| ABR0022 | 62.00 |
64.00 | 2.00 |
S200631 | 0.009 | 0.10 | 10 |
32 | 42 | 0.34 | ABR0025 |
28.00 |
30.00 | 2.00 | S200732 | 0.202 | 1.04 | b.d. | 37 |
37 | 0.59 |
| ABR0022 | 64.00 |
66.00 | 2.00 |
S200632 | 0.006 | 0.07 | b.d. | 43 |
35 | 0.20 | ABR0025 |
30.00 |
32.00 | 2.00 | S200733 | 0.017 | 0.80 | b.d. | 20 |
31 | 0.53 |
| ABR0022 | 66.00 |
68.00 | 2.00 |
S200633 | 0.007 | 0.08 | b.d. | 19 |
30 | 0.25 | ABR0025 |
32.00 |
34.00 | 2.00 | S200734 | 0.027 | 0.74 | b.d. | 30 |
33 | 0.57 |
| ABR0022 | 68.00 |
70.00 | 2.00 |
S200634 | 0.007 | 0.08 | b.d. | 12 |
26 | 0.25 | ABR0025 |
34.00 |
36.00 | 2.00 | S200735 | 0.032 | 0.51 | b.d. | 35 |
42 | 0.64 |
| ABR0022 | 70.00 |
72.00 | 2.00 |
S200635 | 0.013 | 0.12 | 10 |
16 | 34 | 0.43 | ABR0025 |
36.00 |
38.00 | 2.00 | S200736 | 0.067 | 0.44 | b.d. | 27 |
35 | 0.60 |
| ABR0022 | 72.00 |
73.00 | 1.00 |
S200636 | 0.012 | 0.12 | 20 |
25 | 27 | 0.42 | ABR0025 |
38.00 |
40.00 | 2.00 | S200737 | 0.100 | 0.47 | b.d. | 29 |
38 | 0.65 |
| ABR0025 | 40.00 |
42.00 | 2.00 | S200738 | 0.084 | 0.43 | b.d. | 27 |
33 | 0.62 | |||||||||||
| ABR0023 | 0.00 |
2.00 | 2.00 | S200637 | 0.006 | 0.11 | 50 |
146 | 171 | 0.72 | ABR0025 |
42.00 |
44.00 | 2.00 | S200739 | 0.058 | 0.37 | b.d. | 28 |
32 | 0.62 |
| ABR0023 | 2.00 |
4.00 | 2.00 | S200638 | 0.008 | 0.15 | 60 |
167 | 150 | 1.14 | ABR0025 |
44.00 |
46.00 | 2.00 | S200740 | 0.009 | 0.22 | b.d. | 13 |
30 | 0.75 |
| ABR0023 | 4.00 |
6.00 | 2.00 | S200639 | 0.015 | 0.15 | 50 |
200 | 252 | 0.85 | ABR0025 |
46.00 |
48.00 | 2.00 | S200742 | 0.018 | 0.26 | b.d. | 26 |
43 | 0.76 |
| ABR0023 | 6.00 |
8.00 | 2.00 | S200641 | 0.027 | 0.21 | 80 |
250 | 315 | 0.74 | ABR0025 |
48.00 |
50.00 | 2.00 | S200743 | 0.027 | 0.18 | b.d. | 34 |
43 | 0.67 |
| ABR0023 | 8.00 |
10.00 | 2.00 |
S200642 | 0.036 | 0.28 | 50 |
162 | 209 | 0.61 | ABR0025 |
50.00 |
52.00 | 2.00 | S200744 | 0.017 | 0.17 | b.d. | 28 |
42 | 0.66 |
| ABR0023 | 10.00 |
12.00 | 2.00 |
S200643 | 0.018 | 0.39 | 40 |
95 | 189 | 1.03 | ABR0025 |
52.00 |
54.00 | 2.00 | S200745 | 0.016 | 0.17 | b.d. | 26 |
36 | 0.58 |
| ABR0023 | 12.00 |
14.00 | 2.00 |
S200644 | 0.015 | 0.44 | 40 |
94 | 180 | 1.57 | ABR0025 |
54.00 |
56.00 | 2.00 | S200746 | 0.015 | 0.16 | b.d. | 20 |
34 | 0.57 |
| ABR0023 | 14.00 |
16.00 | 2.00 |
S200645 | 0.015 | 0.25 | 30 |
86 | 138 | 1.16 | ABR0025 |
56.00 |
58.00 | 2.00 | S200747 | 0.014 | 0.16 | b.d. | 90 |
113 | 0.58 |
| ABR0023 | 16.00 |
18.00 | 2.00 |
S200646 | 0.017 | 0.30 | 20 |
57 | 98 | 0.93 | ABR0025 |
58.00 |
60.00 | 2.00 | S200748 | 0.014 | 0.15 | b.d. | 26 |
31 | 0.59 |
| ABR0023 | 18.00 |
20.00 | 2.00 |
S200647 | 0.052 | 0.49 | 30 |
40 | 71 | 0.97 | ABR0025 |
60.00 |
62.00 | 2.00 | S200749 | 0.011 | 0.14 | b.d. | 28 |
28 | 0.57 |
| ABR0023 | 20.00 |
22.00 | 2.00 |
S200648 | 0.313 | 0.78 | 10 |
47 | 69 | 0.89 | ABR0025 |
62.00 |
64.00 | 2.00 | S200750 | 0.013 | 0.14 | b.d. | 33 |
31 | 0.51 |
| ABR0023 | 22.00 |
24.00 | 2.00 |
S200649 | 0.061 | 0.88 | 20 |
29 | 58 | 0.69 | ABR0025 |
64.00 |
66.00 | 2.00 | S200751 | 0.013 | 0.15 | b.d. | 17 |
22 | 0.46 |
| ABR0023 | 24.00 |
26.00 | 2.00 |
S200650 | 0.019 | 0.27 | 10 |
35 | 60 | 0.62 | ABR0025 |
66.00 |
68.00 | 2.00 | S200752 | 0.013 | 0.13 | b.d. | 14 |
20 | 0.44 |
| ABR0023 | 26.00 |
28.00 | 2.00 |
S200650A | 0.032 | 0.34 | b.d. | 22 |
51 | 0.46 | ABR0025 |
68.00 |
70.00 | 2.00 | S200753 | 0.008 | 0.09 | b.d. | 20 |
26 | 0.34 |
| ABR0023 | 28.00 |
30.00 | 2.00 |
S200651 | 0.018 | 0.25 | b.d. | 34 |
71 | 0.66 | ABR0025 |
70.00 |
72.00 | 2.00 | S200754 | 0.009 | 0.11 | b.d. | 14 |
19 | 0.39 |
| ABR0023 | 30.00 |
32.00 | 2.00 |
S200652 | 0.020 | 0.24 | 20 |
33 | 70 | 0.68 | ABR0025 |
72.00 |
73.00 | 1.00 | S200755 | 0.009 | 0.10 | b.d. | 13 |
16 | 0.39 |
| ABR0023 | 32.00 |
34.00 | 2.00 |
S200653 | 0.020 | 0.23 | 10 |
43 | 80 | 0.66 | |||||||||||
| ABR0023 | 34.00 |
36.00 | 2.00 |
S200654 | 0.020 | 0.22 | 10 |
43 | 95 | 0.69 | ABR0026 |
0.00 |
2.00 | 2.00 | S200756 | 0.004 | 0.08 | 10 |
114 | 30 | 0.69 |
| ABR0023 | 36.00 |
38.00 | 2.00 |
S200655 | 0.020 | 0.22 | b.d. | 33 |
64 | 0.68 | ABR0026 |
2.00 |
4.00 | 2.00 | S200757 | b.d. | 0.02 | b.d. | 42 |
22 | 0.21 |
| ABR0023 | 38.00 |
40.00 | 2.00 |
S200656 | 0.019 | 0.21 | 10 |
28 | 58 | 0.67 | ABR0026 |
4.00 |
6.00 | 2.00 | S200758 | b.d. | 0.02 | b.d. | 105 |
28 | 0.68 |
| ABR0023 | 40.00 |
42.00 | 2.00 |
S200657 | 0.018 | 0.20 | b.d. | 32 |
49 | 0.68 | ABR0026 |
6.00 |
8.00 | 2.00 | S200759 | 0.001 | 0.02 | b.d. | 51 |
19 | 0.38 |
| ABR0023 | 42.00 |
44.00 | 2.00 |
S200658 | 0.022 | 0.21 | 10 |
33 | 60 | 0.69 | ABR0026 |
8.00 |
10.00 | 2.00 | S200761 | b.d. | 0.02 | b.d. | 36 |
23 | 0.34 |
| ABR0023 | 44.00 |
46.00 | 2.00 |
S200659 | 0.016 | 0.20 | b.d. | 21 |
68 | 0.68 | ABR0026 |
10.00 |
12.00 | 2.00 | S200762 | b.d. | 0.03 | b.d. | 37 |
41 | 0.28 |
| ABR0023 | 46.00 |
48.00 | 2.00 |
S200661 | 0.014 | 0.17 | b.d. | 19 |
62 | 0.56 | ABR0026 |
12.00 |
14.00 | 2.00 | S200763 | 0.002 | 0.04 | 20 |
49 | 45 | 0.29 |
| ABR0023 | 48.00 |
50.00 | 2.00 |
S200662 | 0.017 | 0.19 | b.d. | 28 |
56 | 0.66 | ABR0026 |
14.00 |
16.00 | 2.00 | S200764 | 0.001 | 0.03 | 20 |
54 | 41 | 0.43 |
| ABR0023 | 50.00 |
52.00 | 2.00 |
S200663 | 0.017 | 0.18 | 10 |
35 | 66 | 0.56 | ABR0026 |
16.00 |
18.00 | 2.00 | S200765 | 0.014 | 0.14 | 20 |
11 | 11 | 1.63 |
| ABR0023 | 52.00 |
54.00 | 2.00 |
S200664 | 0.013 | 0.14 | 10 |
11 | 23 | 0.40 | ABR0026 |
18.00 |
20.00 | 2.00 | S200766 | 0.019 | 0.19 | 20 |
29 | 64 | 1.63 |
| ABR0023 | 54.00 |
56.00 | 2.00 |
S200665 | 0.011 | 0.11 | b.d. | 18 |
33 | 0.39 | ABR0026 |
20.00 |
22.00 | 2.00 | S200767 | 0.023 | 0.21 | 10 |
50 | 106 | 1.29 |
| ABR0023 | 56.00 |
58.00 | 2.00 |
S200666 | 0.007 | 0.09 | b.d. | 11 |
23 | 0.28 | ABR0026 |
22.00 |
24.00 | 2.00 | S200768 | 0.013 | 0.24 | 50 |
44 | 101 | 1.51 |
21
Cobalt, Scandium & PGM results from Black Range
==> picture [35 x 842] intentionally omitted <==
==> picture [184 x 26] intentionally omitted <==
| Hole | From (m) |
To (m) |
Width (m) |
Sample number |
Co (%) |
Ni (%) |
Sc (g/t) |
Pt (ppb) |
Pd (ppb) |
Cr (%) |
|---|---|---|---|---|---|---|---|---|---|---|
| ABR0026 | 24.00 |
26.00 | 2.00 |
S200769 | 0.034 | 0.42 | 30 |
54 | 133 | 1.28 |
| ABR0026 | 26.00 |
28.00 | 2.00 |
S200770 | 0.029 | 0.52 | b.d. | 37 |
46 | 1.19 |
| ABR0026 | 28.00 |
30.00 | 2.00 |
S200771 | 0.016 | 0.50 | b.d. | 30 |
44 | 1.07 |
| ABR0026 | 30.00 |
32.00 | 2.00 |
S200772 | 0.020 | 0.61 | b.d. | 33 |
47 | 1.03 |
| ABR0026 | 32.00 |
34.00 | 2.00 |
S200773 | 0.061 | 0.58 | b.d. | 43 |
44 | 0.83 |
| ABR0026 | 34.00 |
36.00 | 2.00 |
S200774 | 0.049 | 0.47 | b.d. | 39 |
37 | 1.09 |
| ABR0026 | 36.00 |
38.00 | 2.00 |
S200775 | 0.026 | 0.38 | b.d. | 29 |
31 | 0.69 |
| ABR0026 | 38.00 |
40.00 | 2.00 |
S200776 | 0.015 | 0.25 | b.d. | 32 |
50 | 0.64 |
| ABR0026 | 40.00 |
42.00 | 2.00 |
S200777 | 0.015 | 0.21 | b.d. | 22 |
34 | 0.63 |
| ABR0026 | 42.00 |
44.00 | 2.00 |
S200778 | 0.015 | 0.20 | b.d. | 25 |
35 | 0.59 |
| ABR0026 | 44.00 |
46.00 | 2.00 |
S200779 | 0.013 | 0.18 | b.d. | 22 |
36 | 0.58 |
| ABR0026 | 46.00 |
48.00 | 2.00 |
S200781 | 0.015 | 0.17 | b.d. | 29 |
34 | 0.58 |
| ABR0026 | 48.00 |
50.00 | 2.00 |
S200782 | 0.014 | 0.16 | b.d. | 29 |
35 | 0.59 |
| ABR0026 | 50.00 |
52.00 | 2.00 |
S200783 | 0.015 | 0.16 | b.d. | 24 |
36 | 0.60 |
| ABR0026 | 52.00 |
54.00 | 2.00 |
S200784 | 0.015 | 0.15 | b.d. | 27 |
32 | 0.60 |
| ABR0026 | 54.00 |
56.00 | 2.00 |
S200785 | 0.013 | 0.15 | b.d. | 30 |
43 | 0.55 |
| ABR0026 | 56.00 |
58.00 | 2.00 |
S200786 | 0.013 | 0.15 | b.d. | 29 |
26 | 0.64 |
| ABR0026 | 58.00 |
60.00 | 2.00 |
S200787 | 0.013 | 0.16 | b.d. | 19 |
25 | 0.56 |
| ABR0026 | 60.00 |
62.00 | 2.00 |
S200788 | 0.012 | 0.15 | b.d. | 18 |
25 | 0.56 |
| ABR0026 | 62.00 |
64.00 | 2.00 |
S200789 | 0.013 | 0.14 | b.d. | 18 |
27 | 0.50 |
| ABR0026 | 64.00 |
66.00 | 2.00 |
S200790 | 0.007 | 0.10 | b.d. | 12 |
20 | 0.35 |
| ABR0026 | 66.00 |
68.00 | 2.00 |
S200791 | 0.006 | 0.09 | b.d. | 14 |
36 | 0.33 |
| ABR0026 | 68.00 |
70.00 | 2.00 |
S200792 | 0.013 | 0.12 | b.d. | 19 |
29 | 0.43 |
| ABR0026 | 70.00 |
72.00 | 2.00 |
S200793 | 0.013 | 0.13 | b.d. | 16 |
30 | 0.45 |
| ABR0026 | 72.00 |
73.00 | 1.00 |
S200794 | 0.014 | 0.13 | 10 |
26 | 54 | 0.45 |
| ABR0027 | 0.00 |
2.00 | 2.00 | S200795 | 0.002 | 0.03 | 10 |
89 | 33 | 0.40 |
| ABR0027 | 2.00 |
4.00 | 2.00 | S200796 | b.d. | 0.01 | 10 |
37 | 20 | 0.18 |
| ABR0027 | 4.00 |
6.00 | 2.00 | S200797 | 0.002 | 0.03 | 40 |
30 | 14 | 0.22 |
| ABR0027 | 6.00 |
8.00 | 2.00 | S200798 | 0.001 | 0.02 | 20 |
70 | 20 | 0.44 |
| ABR0027 | 8.00 |
10.00 | 2.00 |
S200799 | b.d. | 0.02 | 20 |
49 | 24 | 0.32 |
| ABR0027 | 10.00 |
12.00 | 2.00 |
S200800 | 0.002 | 0.02 | 50 |
61 | 22 | 0.67 |
| ABR0027 | 12.00 |
14.00 | 2.00 |
S200802 | 0.002 | 0.03 | 10 |
41 | 40 | 0.20 |
| ABR0027 | 14.00 |
16.00 | 2.00 |
S200803 | 0.002 | 0.03 | 20 |
48 | 52 | 0.22 |
| ABR0027 | 16.00 |
18.00 | 2.00 |
S200804 | 0.002 | 0.04 | 70 |
29 | 36 | 0.26 |
| ABR0027 | 18.00 |
20.00 | 2.00 |
S200805 | 0.002 | 0.04 | 40 |
47 | 41 | 0.38 |
| ABR0027 | 20.00 |
22.00 | 2.00 |
S200806 | 0.004 | 0.10 | 40 |
11 | 10 | 1.28 |
| ABR0027 | 22.00 |
24.00 | 2.00 |
S200807 | 0.007 | 0.20 | 60 |
34 | 54 | 1.40 |
| ABR0027 | 24.00 |
26.00 | 2.00 |
S200808 | 0.007 | 0.18 | 80 |
32 | 62 | 1.96 |
| ABR0027 | 26.00 |
28.00 | 2.00 |
S200809 | 0.016 | 0.33 | 60 |
78 | 94 | 0.92 |
| ABR0027 | 28.00 |
30.00 | 2.00 |
S200810 | 0.085 | 1.07 | 30 |
62 | 44 | 0.72 |
| ABR0027 | 30.00 |
32.00 | 2.00 |
S200811 | 0.199 | 0.98 | 10 |
62 | 53 | 0.63 |
| ABR0027 | 32.00 |
34.00 | 2.00 |
S200812 | 0.075 | 0.85 | 20 |
40 | 55 | 0.61 |
| ABR0027 | 34.00 |
36.00 | 2.00 |
S200813 | 0.052 | 0.94 | 10 |
32 | 48 | 0.65 |
| ABR0027 | 36.00 |
38.00 | 2.00 |
S200814 | 0.032 | 0.71 | 10 |
18 | 43 | 0.68 |
| ABR0027 | 38.00 |
40.00 | 2.00 |
S200815 | 0.024 | 0.35 | 20 |
19 | 34 | 0.61 |
| ABR0027 | 40.00 |
42.00 | 2.00 |
S200816 | 0.016 | 0.25 | 20 |
20 | 45 | 0.60 |
| ABR0027 | 42.00 |
44.00 | 2.00 |
S200817 | 0.017 | 0.21 | 30 |
16 | 33 | 0.59 |
| ABR0027 | 44.00 |
46.00 | 2.00 |
S200818 | 0.015 | 0.18 | 10 |
21 | 34 | 0.61 |
| ABR0027 | 46.00 |
48.00 | 2.00 |
S200819 | 0.013 | 0.16 | 20 |
17 | 40 | 0.58 |
| ABR0027 | 48.00 |
50.00 | 2.00 |
S200821 | 0.011 | 0.15 | b.d. | 39 |
47 | 0.53 |
| ABR0027 | 50.00 |
52.00 | 2.00 |
S200822 | 0.014 | 0.15 | 30 |
16 | 35 | 0.57 |
| ABR0027 | 52.00 |
54.00 | 2.00 |
S200823 | 0.013 | 0.15 | 10 |
15 | 31 | 0.55 |
| ABR0027 | 54.00 |
56.00 | 2.00 |
S200824 | 0.014 | 0.16 | 10 |
14 | 33 | 0.52 |
| ABR0027 | 56.00 |
58.00 | 2.00 |
S200825 | 0.013 | 0.15 | 10 |
17 | 29 | 0.53 |
| ABR0027 | 58.00 |
60.00 | 2.00 |
S200826 | 0.014 | 0.14 | 30 |
19 | 40 | 0.53 |
| ABR0027 | 60.00 |
62.00 | 2.00 |
S200827 | 0.013 | 0.14 | 10 |
13 | 25 | 0.53 |
| ABR0027 | 62.00 |
64.00 | 2.00 |
S200828 | 0.013 | 0.13 | 20 |
11 | 23 | 0.52 |
| ABR0027 | 64.00 |
66.00 | 2.00 |
S200829 | 0.012 | 0.14 | 20 |
13 | 29 | 0.48 |
| ABR0027 | 66.00 |
68.00 | 2.00 |
S200830 | 0.018 | 0.15 | 10 |
27 | 91 | 0.46 |
| ABR0027 | 68.00 |
70.00 | 2.00 |
S200831 | 0.012 | 0.14 | 10 |
12 | 28 | 0.49 |
| ABR0027 | 70.00 |
72.00 | 2.00 |
S200832 | 0.016 | 0.14 | 30 |
27 | 39 | 0.47 |
| ABR0027 | 72.00 |
74.00 | 2.00 |
S200833 | 0.011 | 0.13 | b.d. | b.d. |
1 | 0.45 |
| ABR0027 | 74.00 |
76.00 | 2.00 |
S200834 | 0.012 | 0.13 | 30 |
17 | 55 | 0.53 |
| ABR0027 | 76.00 |
78.00 | 2.00 |
S200835 | 0.012 | 0.11 | 10 |
14 | 31 | 0.41 |
| ABR0027 | 78.00 |
80.00 | 2.00 |
S200836 | 0.013 | 0.12 | 20 |
14 | 33 | 0.42 |
| ABR0027 | 80.00 |
82.00 | 2.00 |
S200837 | 0.012 | 0.12 | 20 |
10 | 21 | 0.42 |
| ABR0027 | 82.00 |
84.00 | 2.00 |
S200838 | 0.013 | 0.12 | 10 |
9 | 21 | 0.42 |
| ABR0027 | 84.00 |
85.00 | 1.00 |
S200839 | 0.012 | 0.12 | b.d. | 9 |
15 | 0.42 |
22
Cobalt, Scandium & PGM results from Black Range
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Appendix 3 – Collated intercepts, Black Range
Parameters used to define cobalt, PGE, and scandium intercepts at Black Range
| Parameter | Cobalt-nickel | Platinum+Palladium (PGE) | Scandium |
|---|---|---|---|
| Minimum cutoff | 0.10 % Co | 0.5 g/t Pt+Pd | 50 g/t Sc |
| Minimum intercept thickness | 2 m | 2 m | 2 m |
| Maximum internal waste thickness | 4 m | 3 m | 3 m |
Cobalt, PGE, and scandium intercepts from new drilling at Black Range
| Drillhole | Cobalt-Nickel intercepts | PGE intercepts | Scandium intercepts |
|---|---|---|---|
| ABR0001 | 2 m at 0.11 % Co and 0.38 % Ni from 18.0 m | 18 m at 0.83 g/t Pt+Pd from surface |
18 m at 97.8 g/t Sc from surface |
| 2 m at 0.51 g/t Pt+Pd from 40.0 m | |||
| ABR0002 | 2 m at 0.13 % Co and 0.68 % Ni from 10.0 m | 4 m at 55 g/t Sc from surface | |
| ABR0003 | 8 m at 0.17 % Co and 0.69 % Ni from 8.0 m | 12 m at 0.67 g/t Pt+Pd from surface |
12 m at 68.3 g/t Sc from surface |
| ABR0004 | 12 m at 0.92 g/t Pt+Pd from 4.0 m | 18 m at 70 g/t Sc from surface |
|
| ABR0005 | 2 m at 0.11 % Co and 0.86 % Ni from 14.0 m | 6 m at 0.8 g/t Pt+Pd from 4.0 m |
6 m at 56.7 g/t Sc from surface |
| 2 m at 50 g/t Sc from 12.0 m | |||
| ABR0006 | 10 m at 0.12 % Co and 0.74 % Ni from 16.0 m | 2 m at 0.86 g/t Pt+Pd from 10.0 m |
10 m at 94 g/t Sc from surface |
| 10 m at 62 g/t Sc from 16.0 m | |||
| ABR0007 | 6 m at 0.14 % Co and 1.02 % Ni from 40.0 m | 2 m at 0.59 g/t Pt+Pd from 2.0 m |
4 m at 65 g/t Sc from surface |
| 16 m at 50 g/t Sc from 14.0 m | |||
| 2 m at 50 g/t Sc from 34.0 m | |||
| ABR0008 | 16 m at 0.14 % Co and 0.74 % Ni from 60.0 m | 10 m at 60 g/t Sc from 32.0 m | |
| 2 m at 0.12 % Co and 0.97 % Ni from 88.0 m | 26 m at 47.7 g/t Sc from 52.0 m | ||
| 6 m at 0.17 % Co and 0.46 % Ni from 98.0 m | 2 m at 50 g/t Sc from 82.0 m | ||
| ABR0009 | 10 m at 0.12 % Co and 0.81 % Ni from 34.0 m | 2 m at 60 g/t Sc from 16.0 m | |
| 4 m at 55 g/t Sc from 24.0 m | |||
| ABR0010 | 4 m at 0.62 g/t Pt+Pd from 10.0 m | 2 m at 50 g/t Sc from 6.0 m |
|
| ABR0011 | 8 m at 67.5 g/t Sc from surface | ||
| ABR0012 | 4 m at 0.17 % Co and 0.73 % Ni from 2.0 m | ||
| ABR0013 | 10 m at 0.21 % Co and 0.75 % Ni from 4.0 m | 8 m at 57.5 g/t Sc from 2.0 m | |
| ABR0014 | 8 m at 0.2 % Co and 0.87 % Ni from 2.0 m | 10 m at 58 g/t Sc from 2.0 m | |
| ABR0015 | 2 m at 0.18 % Co and 0.35 % Ni from 30.0 m | 16 m at 0.64 g/t Pt+Pd from surface |
32 m at 83.1 g/t Sc from surface |
| 2 m at 0.6 g/t Pt+Pd from 22.0 m | |||
| 4 m at 0.56 g/t Pt+Pd from 28.0 m | |||
| ABR0016 | 4 m at 0.11 % Co and 0.48 % Ni from 10.0 m | 6 m at 0.75 g/t Pt+Pd from surface |
18 m at 54.4 g/t Sc from surface |
| ABR0017 | |||
| ABR0018 | |||
| ABR0019 | 2 m at 0.51 g/t Pt+Pd from 26.0 m | ||
| ABR0020 | 6 m at 0.85 g/t Pt+Pd from surface | 8 m at 90 g/t Sc from surface |
|
| 4 m at 0.66 g/t Pt+Pd from 10.0 m | |||
| ABR0021 | 20 m at 0.66 g/t Pt+Pd from 4.0 m | 20 m at 84 g/t Sc from 4.0 m |
|
| 2 m at 0.88 g/t Pt+Pd from 44.0 m | |||
| ABR0022 | 10 m at 0.27 % Co and 0.91 % Ni from 14.0 m | 8 m at 0.66 g/t Pt+Pd from 2.0 m |
28 m at 64.3 g/t Sc from surface |
| 4 m at 0.51 g/t Pt+Pd from 14.0 m | |||
| ABR0023 | 2 m at 0.31 % Co and 0.78 % Ni from 20.0 m | 2 m at 0.57 g/t Pt+Pd from 6.0 m |
10 m at 58 g/t Sc from surface |
| ABR0024 | 8 m at 45 g/t Sc from 2.0 m |
23
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Cobalt, Scandium & PGM results from Black Range
| Drillhole | Cobalt-Nickel intercepts | PGE intercepts | Scandium intercepts | ||
|---|---|---|---|---|---|
| ABR0025 | 2 | m at | 0.2 % Co and 1.04 % Ni from 28.0 m | 6 m at 56.7 g/t Sc from 18.0 m | |
| 2 | m at | 0.1 % Co and 0.47 % Ni from 38.0 m | |||
| ABR0026 | 2 m at 50 g/t Sc from 22.0 m | ||||
| ABR0027 | 2 | m at | 0.2 % Co and 0.98 % Ni from 30.0 m | 2 m at 50 g/t Sc from 10.0 m | |
| 2 m at 70 g/t Sc from 16.0 m | |||||
| 6 m at 66.7 g/t Sc from 22.0 m |
Cobalt, PGE, and scandium intercepts from historic drilling at Black Range
| Drillhole | Cobalt-Nickel intercepts | PGE intercepts | Scandium intercepts |
|---|---|---|---|
| BKRC0120 | 6 m at 0.17 % Co and 1 % Ni from 28.0 m | No data |
No data |
| BKRC0121 | 6 m at 0.21 % Co and 1.74 % Ni from 8.0 m | No data |
No data |
| BKRC0129 | 2 m at 0.16 % Co and 0.98 % Ni from 20.0 m | No data |
No data |
| BKRC0132 | 2 m at 0.17 % Co and 0.83 % Ni from 2.0 m | No data |
No data |
| BKRC0133 | 4 m at 0.14 % Co and 0.82 % Ni from 2.0 m | No data |
No data |
| BKRC0134 | 8 m at 0.14 % Co and 0.86 % Ni from 20.0 m | No data |
No data |
| BKRC0135 | 6 m at 0.32 % Co and 0.87 % Ni from 24.0 m 6mat 0.22% Co and 0.72%Ni from38.0m |
No data |
No data |
| BKRC0136 | 12 m at 0.14 % Co and 1.2 % Ni from 36.0 m | No data |
No data |
| BKRC0144 | 4 m at 0.11 % Co and 1.05 % Ni from 34.0 m | No data |
No data |
| BKRC0145 | 4 m at 0.13 % Co and 0.31 % Ni from 68.0 m | No data |
No data |
| BKRC0147 | 6 m at 0.15 % Co and 0.62 % Ni from 60.0 m | No data |
No data |
| BRR0069 | 4 m at 0.16 % Co and 0.61 % Ni from 16.0 m | No data |
No data |
| BRR0070 | 4 m at 0.14 % Co and 0.49 % Ni from 16.0 m | No data |
No data |
| BRR0071 | 20 m at 0.25 % Co and 0.55 % Ni from 28.0 m | No data |
No data |
| BRR0072 | 4 m at 0.11 % Co and 0.73 % Ni from 28.0 m | No data |
No data |
| BRR0073 | 8 m at 0.24 % Co and 1.86 % Ni from 16.0 m | No data |
No data |
| BRR0074 | 8 m at 0.32 % Co and 1.15 % Ni from 24.0 m | No data |
No data |
| BRR0075 | 4 m at 0.15 % Co and 1.3 % Ni from 24.0 m | No data |
No data |
| BRR0076 | 4 m at 0.14 % Co and 1.18 % Ni from 24.0 m | No data |
No data |
| BRR0078 | 4 m at 0.1 % Co and 0.71 % Ni from 24.0 m | No data |
No data |
| BRR0079 | 16 m at 0.15 % Co and 0.86 % Ni from 16.0 m | No data |
No data |
| BRR0080 | 20 m at 0.15 % Co and 0.56 % Ni from 20.0 m | No data |
No data |
| BRR0081 | 4 m at 0.16 % Co and 0.29 % Ni from 20.0 m 16mat 0.15 % Co and 0.36 %Ni from32.0m |
No data |
No data |
| BRR0096 | 12 m at 0.23 % Co and 0.76 % Ni from 40.0 m | No data |
No data |
| BRRB008 | 4 m at 0.5 g/t Pt+Pd from 0.0 m | No data |
|
| BRRB009 | 8 m at 0.54 g/t Pt+Pd from 12.0 m | No data |
|
| BRRB014 | 4 m at 0.53 g/t Pt+Pd from 0.0 m | No data |
|
| BRRB022 | 4 m at 0.65 g/t Pt+Pd from 16.0 m | No data |
|
| BRRB052 | 4 m at 0.67 g/t Pt+Pd from 0.0 m | No data |
|
| BRRB059 | 4 m at 0.9 g/t Pt+Pd from 0.0 m | No data |
|
| BRRB060 | 4 m at 0.19 % Co and 0.48 % Ni from 32.0 m | 4 m at 0.57 g/t Pt+Pd from 4.0 m |
No data |
| BRRB061 | 16 m at 0.74 g/t Pt+Pd from 8.0 m | No data |
24
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Cobalt, Scandium & PGM results from Black Range
Appendix 4 – JORC Code, 2012 Edition, Table 1 report
Section 1 Sampling Techniques and Data
(Criteria in this section applies to all succeeding sections)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling techniques Note: Due to the similarity of the deposit styles, procedures and estimations used this table represents the combined methods for all Ardea Resources (ARL) Cobalt and Nickel Laterite Resources. Where data not collected by ARL has been used in the resource calculations, variances in techniques are noted. |
• Nature and quality of sampling (eg cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. • Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. • Aspects of the determination of mineralisation that are Material to the Public Report. • In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine nodules) may warrant disclosure of detailed information. |
• In this most recent program, Ardea sampled the Black Range deposit by drilling using Reverse Circulation (RC) on a grid spacing of 400mE x 40mN. Holes were vertical (-90 degree dip), designed to optimally intersect the sub- horizontal mineralisation. All holes were sampled on 2 metre, or rarely 1 metre, down hole intervals. • The drill spacing was designed to augment and infill between historic drilling, leading to an overall drill density of 40x200m. |
25
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Cobalt, Scandium & PGM results from Black Range
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Drilling techniques | • Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc). |
• RC drilling was performed with a face sampling hammer (bit diameter between 4½ and 5 ¼ inches) and samples were collected by either a cone (majority) or riffle splitter using 2 metre composites. Sample condition, sample recovery and sample size were recorded for all drill samples collected by ARL. |
| Drill sample recovery | • Method of recording and assessing core and chip sample recoveries and results assessed. • Measures taken to maximise sample recovery and ensure representative nature of the samples. • Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. |
• RC chip sample recovery was recorded by visual estimation of the reject sample, expressed as a percentage recovery. Overall estimated recovery was approximately 80%, which is considered to be acceptable for nickel-cobalt laterite deposits. RC Chip sample condition recorded using a three code system, D=Dry, M=Moist, W=Wet. A small proportion of samples were moist or wet (11.5%), with the majority of these being associated with soft goethite clays, where water injection has been used to improve drill recovery. • Measures taken to ensure maximum RC sample recoveries included maintaining a clean cyclone and drilling equipment, using water injection at times of reduced air circulation, as well as regular communication with the drillers and slowing drill advance rates when variable to poor ground conditions are encountered. |
| Logging | • Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. • Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. • The total length and percentage of the relevant intersections logged. |
• Visual geological logging was completed for all RC drilling on 1 metre intervals. The logging system was developed by Heron Resources Limited specifically for the KNP and was designed to facilitate future geo- metallurgical studies. Logging was performed at the time of drilling, and planned drill hole target lengths adjusted by the geologist during drilling. The geologist also oversaw all sampling and drilling practices. A mixture of ARL employees and contract geologists supervised all drilling. A small selection of representative chips were also collected for every 1 metre interval and stored in chip-trays for future reference. Only drilling contractors with previous nickel laterite experience and suitable rigs were used. • The geological legend used by ARL is a qualitative legend designed to capture the key physical and metallurgical features of the nickel-cobalt laterite mineralisation. Logging captured the colour, regolith unit and mineralisation style, often accompanied by the logging of protolith, estimated percentage of free silica, texture, grain size and alteration. Logging correlated well with the geochemical algorithm developed by Heron Resources Limited for the Yerilla Nickel Project for material type prediction from multi-element assay data. |
| Sub-sampling techniques and sample preparation |
• If core, whether cut or sawn and whether quarter, half or all core taken. • If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. • For all sample types, the nature, quality and appropriateness of the sample preparation technique. • Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. • Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. • Whether sample sizes are appropriate to the grain size of the material being sampled. |
• 2 metre (and rarely 1 metre) composite samples were recovered using a 15:1 rig mounted cone splitter or trailer mounted riffle splitter during drilling into a calico sample bag. Sample target weight was between 2 and 3kg. In the case of wet clay samples, grab samples taken from sample return pile, initially into a calico sample bag. Wet samples stored separately from other samples in plastic bags and riffle split once dry. • QAQC was employed. A standard, blank or duplicate sample was inserted into the sample stream 10 metres on a rotating basis. Standards were either quantified industry standards, or standards made from homogenised bulk samples of the mineralisation being drilled (in the case of the Yerilla project). Every 30th sample a duplicate sample was taken using the same sample sub sample technique as the original sub sample. Sample sizes are appropriate for the nature of mineralisation. |
| Quality of assay data and laboratory tests |
• The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. |
• All Ardea samples were submitted to Kalgoorlie ALS laboratories and transported to ALS Perth, where they were pulverised. Analysis at ALS Perth was by ICP utilising a 50g charge (lab method PGM-ICP24) for PGM suite elements (Au, Pt, Pd). Additional analysis was undertaken by sending subsamples to ALS |
26
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Cobalt, Scandium & PGM results from Black Range
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| • For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. • Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. |
Brisbane where analysis by silicate fusion / XRF analysis (lab method ME-XRF12n) for multiple grade attributes for laterite ores (Al2O3, As, BaO, CaO, Cl, Co, Cr2O3, Cu, Fe2O3, Ga, K2O, MgO, MnO, Na2O, Ni, P2O5, Pb, Sc, SiO2, SO3, SrO, TiO2, V2O5, Zn, ZrO2). Fusion / XRF analysis is an industry standard method used to analyse nickel laterite ores and ALS is a reputable commercial laboratory with extensive experience in assaying nickel laterite samples from numerous Western Australian nickel laterite deposits. • ALS routinely inserts analytical blanks, standards and duplicates into the client sample batches for laboratory QAQC performance monitoring. • Ardea also inserted QAQC samples into the sample stream at a 1 in 20 frequency, alternating between duplicates splits, blanks (industrial sands) and standard reference materials. • Additionally, a review was conducted for geochemical consistency between historically expected data, recent data, and geochemical values that would be expected in a nickel laterite profile. • All of the QAQC data has been statistically assessed. There were some inconsistencies in the returning results from standards submitted, relating to the XRF analysis suite. This has been thoroughly investigated with the conclusion that either some standards were not correctly identified and recorded on submission, or time/external influence has had an impact on some of the quality of the values standards, as figures reported for the relevant errant standards were significantly different to the normal recognisable standard values. Ardea has undertaken its own further in-house review of QAQC results of the ALS routine standards, 100% of which returned within acceptable QAQC limits. This fact combined with the fact that the data is demonstrably consistent and repeated for expected Ni/Co values within the lateritic ore profiles of both reported areas and is also consistent with nearby abundant historic drilling data, has meant that the results are considered to be acceptable and suitable for reporting. |
|
| Verification of sampling and assaying |
• The verification of significant intersections by either independent or alternative company personnel. • The use of twinned holes. • Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. • Discuss any adjustment to assay data. |
• No independent verification has been undertaken. • No twinned holes were drilled. • A review of logged geology and geochemical domains within drill holes reconciles consistently with values that would be expected within the lateritic profiles of both areas. Data values are within the numerical ranges that are consistent with 200 m proximal drill hole values for the respective orebodies (i.e. values are not considered outliers or skewed). Scandium has not been historically evaluated and is unusually high in drill hole AKR0015, however historic drill holes were not assayed for scandium so no comparison is available. • No adjustments have been made to the assay data. |
| Location of data points | • Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. • Specification of the grid system used. • Quality and adequacy of topographic control. |
• All drill holes surveyed using an RTK DGPS system with either a 3 or 7 digit accuracy. The coordinates are stored in the exploration database referenced to the MGA Zone 51 Datum GDA94. • All holes drilled as part of the Black Range program were vertical. No holes were down-hole surveyed. The sub-horizontal orientation of the mineralisation, combined with the soft nature of host material results in minimal deviation of vertical RC drill holes. For example, a small number of vertical open RC holes were check surveyed at Jump Up Dam, and found to have deviation over 60m of less than 1 metre, which is considered sufficiently accurate for this style of mineralisation. • The grid system for all models is GDA94. Where historic data or mine grid data has been used it has been transformed into GDA94 from its original source grid via the appropriate transformation. Both original and transformed data is stored in the digital database. • A DTM was constructed from picked up drill collar locations. The use of collar data is considered |
27
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Cobalt, Scandium & PGM results from Black Range
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| sufficiently accurate for reporting of resources, but is not suitable for mine planning and reserves. | ||
| Data spacing and distribution |
• Data spacing for reporting of Exploration Results. • Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. • Whether sample compositing has been applied. |
• This drill program at Black Range was drilled at a grid spacing of 400mE x 40mN. Black Range has historically been drilled on a series of uniform grids ranging from a maximum of 400mE x 100mN to 200mE x 40mN. • Sample compositing has not been applied to the newly collected data. |
| Orientation of data in relation to geological structure |
• Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. • If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. |
• All drill holes in this program were vertical and give a true width of the regolith layers and mineralisation. • On a local scale there is some variability due to sub-vertical to vertical structures which may not be picked up with the relatively broad spaced vertical drill pattern employed. This local variability is not considered to be significant for the project overall, but will have local effects on mining and scheduling later in the project life. |
| Sample security | • The measures taken to ensure sample security. |
• All samples were collected and accounted for by ARL employees during drilling. All samples were bagged into plastic bags and closed with cable ties. Samples were transported to Kalgoorlie from site by ARL employees/contractors in sealed bulka bags. • Consignments were transported to ALS Laboratories in Perth by Coastal Midwest Transport. All samples were transported with a manifest of sample numbers and a sample submission form containing laboratory instructions. Any discrepancies between sample submissions and samples received were routinely followed up and accounted for. |
| Audits or reviews | • The results of any audits or reviews of sampling techniques and data. |
• ARL has periodically conducted internal reviews of sampling techniques relating to resultant exploration datasets, and larger scale reviews capturing the data from multiple drilling programmes within the KNP. • Internal reviews of the exploration data included the following: • Unsurveyed drill hole collars (less than 1% of collars). • Drill Holes with overlapping intervals (0%). • Drill Holes with no logging data (less than 2% of holes). • Sample logging intervals beyond end of hole depths (0%). • Samples with no assay data (from 0 to <5% for any given project, usually • related to issues with sample recovery from difficult ground conditions, • mechanical issues with drill rig, damage to sample in transport or sample preparation). • Assay grade ranges. • Collar coordinate ranges • Valid hole orientation data. • The ALS Laboratory was visited by ARL staff in 2016, and the laboratory processes and procedures were reviewed at this time and determined to be robust. |
28
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Cobalt, Scandium & PGM results from Black Range
Section 2 - Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Mineral tenement and land tenure status |
• Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures,partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. • The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
• The tenement on which the Black Range drilling was undertaken is M24/757. • The tenement and land tenure status for the KNP prospect areas containing continuous cobalt rich laterite mineralisation is summarised in Table 3 following and in the Ardea Prospectus, section 9 “Solicitor’s Report on Tenements”. |
| Exploration done by other parties |
• Acknowledgment and appraisal of exploration by other parties. |
• The Black Range deposit was initially discovered and drilled by Anaconda Nickel Limited. Much historic drilling and assessment of the Black Range Project was undertaken by Heron Resources Limited. |
| Geology | • Deposit type, geological setting and style of mineralisation. |
• The KNP nickel-cobalt laterite mineralisation developed during the weathering and near surface enrichment of Archaean-aged olivine-cumulate ultramafic units. The mineralisation is usually within 60 metres of surface and can be further subdivided on mineralogical and metallurgical characteristics into upper iron-rich material and lower magnesium-rich material based on the ratios of iron to magnesium. The deposits are analogous to many weathered ultramafic-hosted nickel-cobalt deposits both within Australia and world-wide. • Cobalt-rich mineralisation is typically best developed in iron-rich material in regions of deep weathering in close proximity to major shear zones or transfer shear structures and to a lesser extent as thin zones along the interface of ferruginous and saprolite boundaries at shallower depths proximal to shear structures. • The Cobalt Zone is associated with a distinctive geo-metallurgical type defined as “Clay Upper Pyrolusitic”. Mineralogy is goethite, gibbsite and pyrolusite (strictly “asbolite” or “cobaltian wad”). The Cobalt Zones typically occur as sub-horizontal bodies at a palaeo-water table within the KNP (late stage supergene enrichment). This material is particularly well developed at Goongarrie South. |
| Drill hole Information |
• A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: • easting and northing of the drill hole collar • elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar • dip and azimuth of the hole • down hole length and interception depth • hole length. |
• All holes drilled in this most recent program are listed in“Appendix 1 – Collar location data, Black Range”. Also listed are all historic drill holes from programs for which ARL holds at least some assay data. |
| Drill hole Information |
• If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. |
• All assay data relating to the metals of interest at Black Range, namely cobalt, nickel, scandium, platinum, palladium, and chromium, are listed in “Appendix 2 – Assay results from Black Range”. Other elements were assayed but have not been reported here. They are of use and of interest from a scientific and metallurgical perspective, but are not considered material and their exclusion does not detract from the |
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Cobalt, Scandium & PGM results from Black Range
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| understanding of this report. | ||
| Data aggregation methods |
• In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated. • Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. • The assumptions used for any reporting of metal equivalent values should be clearly stated. |
• Most drill hole samples have been collected over 2m down hole intervals. • All newly defined cobalt intercepts at Black Range (calculated both from new data and historic data) were calculated using the following parameters: • 0.10 % cobalt minimum cutoff; • 2 m minimum intercept; and • 4 m internal waste. • Platinum and palladium are closely associated metals in nature in general and at Black Range in particular. Platinum and palladium are two of a group of metals that are typically referred to as Platinum Group Elements (PGEs) or Platinum Group Metals (PGMs). All newly defined platinum and palladium intercepts at Black Range (calculated both from new data and historic data) were calculated using the following parameters: • 0.50 g/t platinum+palladium minimum cutoff; • 2 m minimum intercept; and • 3 m internal waste. • All newly defined scandium intercepts at Black Range were calculated using the following parameters: • 50 g/t scandium minimum cutoff; • 2 m minimum intercept; and • 3 m internal waste. • Assay compositing techniques were not used in this assessment. • No metal equivalent calculations have been used in this assessment. |
| Relationship between mineralisation widths and intercept lengths |
• These relationships are particularly important in the reporting of Exploration Results. • If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. • If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’). |
• The nickel-cobalt laterite mineralisation at Black Range has a strong global sub-horizontal orientation. This is also true of the Pt+Pd and Sc mineralisation. • All drill holes are vertical. • All drill holes intersect the mineralisation at approximately 90° to its orientation. All down hole widths approximate true widths. |
| Diagrams | • Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. |
• Maps and sections of the cobalt, nickel, platinum, palladium, and scandium mineralisation are shown within the report. Every drillhole on every section drilled is shown. |
| Balanced reporting |
• Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. |
• Not applicable to this report. All results are report either in the text or in the associated appendices. Examples of high-grade mineralisation are labelled as such. |
| Other substantive exploration data |
• Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
• No other data are, at this stage, known to be either beneficial or deleterious to recovery of the metals reported. Uncertainties surrounding the possibility of recovery of the metals of interest are noted prominently in the report. |
| Further work | • The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling). • Diagrams clearly highlighting the areas of possible extensions, including the main |
• Further drilling is likely to be undertaken at Black Range but has not yet been defined. Further drilling could include infill drilling as well as extension of lines to the north and south as appropriate. • Metallurgicalassessment ofall metals of interest atBlack Rangewillbe undertakenduring thePre- |
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Cobalt, Scandium & PGM results from Black Range
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
Feasibility Study (PFS) about to commence on the KNP Cobalt Zone. Features such as the host minerals to the platinum, palladium, scandium, and chromium, and their recoverability will be assessed in detail. |
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