Skip to main content

AI assistant

Sign in to chat with this filing

The assistant answers questions, extracts KPIs, and summarises risk factors directly from the filing text.

DEVELOP GLOBAL LIMITED Regulatory Filings 2022

Sep 5, 2022

64801_rns_2022-09-05_0aee0458-e27f-4f5f-a7da-b608ad36d963.pdf

Regulatory Filings

Open in viewer

Opens in your device viewer

ASX Announcement September 6, 2022

Sulphur Springs Zinc-Copper Project, WA

Total Resource increases 15% to 1.3Mt of contained zinc-equivalent[1]

Indicated Resource up 32% to 1.16Mt contained ZnEq[1] , paving way for completion of DFS in early CY2023

Highlights

  • Update Mineral Resource Estimate completed for Sulphur Springs Deposit

  • 13.8Mt @ 5.7% Zn, 1.1% Cu, 0.3% Pb, 22.5g/t Ag & 0.2g/t Au (9.3% ZnEq[1] Previous estimate was 13.4Mt @ 8.1% ZnEq[1]

  • Contained metal increased to 786Kt Zn, 153Kt Cu & 10.4Moz Ag (~1.3Mt ZnEq[1] )

  • Substantial increase in geological confidence with ~90% of Resource in the Indicated category

  • Grade increases significantly: zinc up +50%, silver up +15%

  • The Resource is conservative because it is calculated on a net smelter return basis, or payable metal, making it the project’s most robust Resource to date

  • Follow-up infill and resource drilling program underway

  • Underground mine and open pit plans will be redesigned ahead of an updated Reserve estimate

  • Metallurgical testwork almost completed; Project costings being updated

  • Majority of project approvals already secured, including Ministerial Environmental Approval

  • Updated Definitive Feasibility Study (DFS) underway, scheduled for completion in early 2023

Develop (ASX: DVP) is pleased to announce that it has taken a pivotal step towards developing its Sulphur Springs zinc-copper project in WA’s Pilbara, with a substantial Resource increase.

The expanded inventory now hosts 1.3Mt of zinc-equivalent metal[1] . Importantly, 90 per cent of the Resource is now in the Indicated category, paving the way for an updated Reserve to be completed in the coming quarters.

This will in turn lead to completion of the feasibility study early next calendar year.

Develop Managing Director Bill Beament said: “This is an outstanding result which demonstrates that Sulphur Springs now has scale and therefore is well on track to becoming a significant producer of the zinc and copper which will be in huge demand as part of the energy transition.

“With 90 per cent of the increased Resource now in the Indicated category, we are highly confident about the outlook for Sulphur Springs and the key role it will play in Develop’s portfolio of producing assets.

“Our focus is now on completing the mine designs, which will include our revised strategy of starting underground in order to access the more favourable primary ore first. This will increase free cashflow generation and reduce development risk.

“At the same time, we will secure the last permit being the works approval, complete the metallurgical testwork and update project cost estimates, all of which will put us on track to publish the feasibility study early next year.”

Resource Details

The Mineral Resource Estimate has been independently prepared by leading mining consultant Entech.

The updated Sulphur Springs MRE of 13.8Mt @ 5.7% Zn, 1.1% Cu, 0.3% Pb, 22.5g/t Ag & 0.2g/t Au is reported on the basis of a $80/t Net Smelter Return (NSR) and represents the most robust resource for the deposit to date including geometallurgical domaining and recoveries and to fully elucidate the potential for economic extraction.

Significantly, 90% of the Mineral Resource is now classified as Indicated, with the remaining resources in the Inferred category. The classification is supported by drilling density, geological continuity and confidence in the geological interpretation.

Background

As previously announced (see ASX releases 8 December 2021, February 2022 and 16 May 2022), a total of 68 drill holes were completed in 2021 as part of the Company’s de-risking and growth strategy at Sulphur Springs. The drilling was designed to infill the Inferred material within the 2018 Sulphur Springs MRE to a sufficient density to allow conversion into the higher confidence Indicated category; additional exploration drilling also completed across several target areas. The updated MRE results are consistent with these objectives and will pave the way for an increased Reserve, optimised mine development plan, revised project costings and finalisation of funding options.

The MRE includes a mix of oxide, transitional and sulphide mineralisation. The robust nature of the Resource is demonstrated by grade-tonnage curve (Figure 1), which highlights the significant quantity of sulphide mineralisation at higher cut-off grades. Note, the grade-tonnage curve for the Resource includes material classified as Inferred, where data is insufficient to allow the geological grade and continuity to be confidently interpreted.

The drilling and resultant remodelled MRE has resulted in Indicated category resources increasing from to ~68% to ~90% of the total. Step-out and exploration drilling has also highlighted to ongoing potential for expansion to the known mineralisation.

The update MRE has also led to a 260Kt increase in contained zinc metal, a 2.4Moz increase in silver metal, with a decrease of 56Kt in contained copper metal.

Resource Category Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Metallurgical
Domain
Tonnes
(kt)
NSR
($A/t)¹
Zn %
Pb %
Cu %
Ag g/t
Au g/t
Fe %
Indicated Oxide 209
$381
0.3
0.1
4.2
18.9
0.1
29.8
Transitional 6,655
$313
5.7
0.3
1.4
21.8
0.1
23.9
Fresh 5,495
$289
5.8
0.3
0.9
22.0
0.1
21.0
Sub-total
12,360
$303
5.6
0.3
1.2
21.9
0.1
22.7
Inferred Fresh
1,401
$249
6.4
0.5
0.2
38.4
0.2
20.8
Sub-total
1,401
$249
6.4
0.5
0.2
38.4
0.2
20.8
GRAND TOTAL 13,760 $298 5.7 0.3 1.1 23.5 0.2 22.5

Table 1: Sulphur Springs MRE by Resource category and metallurgical domain. NSR reported at A$80/t cut-off. Tonnages are dry metric tonnes. Minor discrepancies may occur due to rounding.

==> picture [455 x 245] intentionally omitted <==

----- Start of picture text -----

Grade Tonnage Curve
18,000,000 12
16,000,000
10
14,000,000
12,000,000 8
10,000,000
6
8,000,000
6,000,000 4
4,000,000
2
2,000,000
- 0
NSR Cut-Off (A$/t)
Tonnes (NSR) Grade (Cu%) Grade (Zn%)
Tonnes
Average Base metal grade (%)
10 30 50 70 90 110 130 150 170 190 210 230 250 270 290 310 330 350 370 390 410 430 450 470 490
----- End of picture text -----

Figure 1: Sulphur Springs Grade Tonnage Curve.

==> picture [424 x 357] intentionally omitted <==

Figure 2. Sulphur Springs Resource block model classification.

==> picture [355 x 303] intentionally omitted <==

Figure 3. Sulphur Springs 2018 Resource block model classification and 2018 Underground mining and open pit Shapes..

==> picture [355 x 306] intentionally omitted <==

Figure 4 . Sulphur Springs 2022 Resource block model classification and 2018 Underground mining and open pit Shapes.

==> picture [396 x 304] intentionally omitted <==

Figure 5. Sulphur Springs Resource block model Zn grades.

==> picture [402 x 309] intentionally omitted <==

Figure 6. Sulphur Springs Resource block model Cu grades.

Future Work

Given the potential for the combination of increased metal grades and output to materially improve the economic outcomes of the 2018 DFS, DVP intends to prepare an optimised DFS in early 2023. Develop also believes that Sulphur Spring has significant growth potential, having historically been under-explored and untested at depth. In particular, the Company believes that Sulphur Springs has strong potential for extensions of existing lenses which are open at depth and along strike, and for the discovery of additional lenses, with logical structural positions untested.

Authorised for ASX release by Managing Director Bill Beament.

Investor Enquiries

Bill Beament DEVELOP Global Limited T: +61 8 6389 7400 E: [email protected]

Media Enquiries

Paul Armstrong Read Corporate P: +61 8 9388 1474 E: [email protected]

About Develop

Develop (ASX: DVP) has a twin-pronged strategy for creating value. The first of these centres on the exploration and production of future-facing metals. As part of this, the Company owns the Sulphur Springs copper-zinc-silver project in WA’s Pilbara region. This project is currently the focus of ongoing exploration to grow the inventory and various development studies. Develop also owns the Woodlawn zinc-copper project in NSW. Woodlawn, which is on care and maintenance, comprises an underground mine, a significant JORC Resource and Reserve and a new processing plant. The second plank of Develop’s strategy centres on the provision of underground mining services. As part of this, Develop has an agreement with Bellevue Gold (ASX: BGL) to provide underground mining services at its Bellevue Gold Project in WA.

1.The zinc equivalent grades for Sulphur Springs (Zn Eq) are based on zinc, copper and silver prices of US$3320/t Zinc, US$7650/t Copper and US$17.5/oz Silver with metallurgical metal recoveries of 93.6% Zn, 86.8% Cu and 46% Ag and are supported by metallurgical test work undertaken. The zinc equivalent calculation is as follows: Zn Eq = Zn grade% * Zn recovery + (Cu grade % *Cu recovery % * (Cu price $/t/ Zn price $/t)) + (Ag grade g/t /31.103 * Ag recovery % * (Ag price $/oz/ Zn price $/t)). It is the opinion of Develop Global and the Competent Person that all elements and products included in the metal equivalent formula have a reasonable potential to be recovered and sold.

Competent Person Statement

The information in this announcement that relates to Exploration Results at the Sulphur Springs Project is based on information by Mr Luke Gibson who is an employee of the Company. Mr Gibson is a member of the Australian Institute of Geoscientists and Mr Gibson has sufficient experience with the style of mineralisation and the type of deposit under consideration. Mr Gibson consents to the inclusion in the report of the results reported here and the form and context in which it appears.

The information contained in this announcement relating to the Sulphur Springs Resources is based on information compiled or reviewed by Ms Jillian Irvin of Entech Pty Ltd who is a Member of the Australian Institute of Geoscientists. Ms Irvin consents to the inclusion. Ms Irvin has sufficient experience relevant to the style of mineralisation, type of deposit under consideration and to the activity being undertaking to qualify as Competent Persons as defined in the 2012 – Refer Edition of the “Australasian Code for Reporting of Mineral Resources”.

Cautionary Statement

The information contained in this document (“Announcement”) has been prepared by DEVELOP Global Limited (“Company”). This Announcement is being used with summarised information. See DEVELOP’s other and periodic disclosure announcements lodged with the Australian Securities Exchange, which are available at www.asx.com.au or at www.develop.com.au for more information.

While the information contained in this Announcement has been prepared in good faith, neither the Company nor any of its shareholders, directors, officers, agents, employees or advisers give any representations or warranties (express or implied) as to the accuracy, reliability or completeness of the information in this Announcement, or of any other written or oral information made or to be made available to any interested party or its advisers (all such information being referred to as “Information”) and liability therefore is expressly disclaimed. Accordingly, to the full extent permitted by law, neither the Company nor any of its shareholders, directors, officers, agents, employees or advisers take any responsibility for, or will accept any liability whether direct or indirect, express or implied, contractual, tortious, statutory or otherwise, in respect of, the accuracy or completeness of the Information or for any of the opinions contained in this Announcement or for any errors, omissions or misstatements or for any loss, howsoever arising, from the use of this Announcement.

This Announcement may include certain statements that may be deemed “forward-looking statements”. All statements in this Announcement, other than statements of historical facts, that address future activities and events or developments that the Company expects, are forward-looking statements. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results or developments may differ materially from those in the forward-looking statements. The Company, its shareholders, directors, officers, agents, employees or advisers, do not represent, warrant or guarantee, expressly or impliedly, that the information in this Announcement is complete or accurate. To the maximum extent permitted by law, the Company disclaims any responsibility to inform any recipient of this Announcement of any matter that subsequently comes to its notice which may affect any of the information contained in this Announcement. Factors that could cause actual results to differ materially from those in forward-looking statements include market prices, continued availability of capital and financing, and general economic, market or business conditions. DEVELOP assumes no obligation to update such information.

Investors are cautioned that any forward-looking statements are not guarantees of future performance and that actual results or developments may differ materially from those projected in forward looking statements. Please undertake your own evaluation of the information in this Announcement and consult your professional advisers if you wish to buy or sell DEVELOP shares.

This Announcement has been prepared in compliance with the JORC Code 2012 Edition. The ‘forward-looking information’ is based on the Company’s expectations, estimates and projections as of the date on which the statements were made. The Company disclaims any intent or obligations to update or revise any forward looking statements whether as a result of new information, estimates or options, future events or results or otherwise, unless required to do so by law.

entech .

Engineering | Geology | Geotech

Entech Pty Ltd. ABN 23 143 135 773

8 Cook St, West Perth WA 6005 [email protected]

entechmining.com

5 September 2022

Luke Gibson Geology Manager Develop Global Limited

LETTER OF CONSENT – SULPHUR SPRINGS ZINC - COPPER DEPOSIT

UNDERGROUND MINERAL RESOURCE ESTIMATE

Dear Mr Gibson

The following report summarises material outcomes with respect to the underground Mineral Resource Estimate for the Sulphur Springs Zinc-Copper deposit, prepared by Entech Pty Ltd during August 2022 and reported in accordance with JORC Code (2012) guidelines. The Material Summary, JORC Code Table 1, sign-off and consent form included in this letter enable Develop Global Limited to achieve compliance with the Australian Securities Exchange (ASX) Listing Rules regarding announcements of Mineral Resources to the market.

Should you have any questions relating to this report please contact the undersigned.

Regards

Entech Pty Ltd

==> picture [150 x 61] intentionally omitted <==

Jill Irvin Principal Geology Consultant BSc MAIG

entech .

MATERIAL SUMMARY

SULPHUR SPRINGS UNDERGROUND MINERAL RESOURCE ESTIMATE

Material information summary as required under ASX Listing Rule 5.8 and JORC Code (2012) reporting guidelines.

Mineral Resource Statement

The Mineral Resource Statement for the Sulphur Springs zinc-copper underground Mineral Resource estimate (MRE) was prepared in August 2022 and is reported according to the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (the ‘JORC Code’) 2012 edition.

The MRE includes 58,868 m of drilling from 149 diamond drill holes (DD), including reverse circulation with diamond tails, and 85 reverse circulation (RC) drill holes, completed since 1988. Of the drill metres underpinning the Mineral Resource, 33% (77 drill holes) were completed by Develop Global Ltd (DVP) during 2021–2022. The remaining historical drilling was completed by previous owners between 1988 and 2017. The depth from surface to the current vertical limit of the Mineral Resources is approximately 400 m.

In the opinion of Entech, the Mineral Resource evaluation reported herein is a reasonable representation of the global underground zinc, copper, silver, lead and gold Mineral Resources within the deposit, based on sampling drill data available as at 18 May 2022.

The Indicated and Inferred Mineral Resources comprise oxide, transitional and fresh rock material and use a net smelter return[1] (NSR) cut-off value. The NSR cut-off value chosen to constrain and report Mineral Resource blocks was A$80/t. Entech considered this cut-off to represent the economic value required to obtain metal recovery[2] using mechanised underground mining methods. The Mineral Resource Statement is presented in Table 1.

1 Net smelter return inputs and application to Mineral Resources are provided under ‘Cut-off parameters’ in Section 3 of the attached JORC Code Table 1.

2 Based on review of feasibility studies, DVP’s Life of Mine Plan (LOMP) and benchmarked against peer operations with comparable deposit style and commodities.

2 | P a g e

entech .

Table 1 Sulphur Springs underground zinc-copper Mineral Resource at A$80/t NSR cut-off

Mineral
Resource
Category
Weathering1 Tonnes
(kt)
NSR
(A$/t)2
Zinc
(%)
Copper
(%)
Silver
(ppm)
Lead
(%)
Gold
(ppm)
Iron
(%)
Indicated Oxide 209 381 0.3 4.2 18.9 0.1 0.1 29.8
Transitional 6,655 313 5.7 1.4 21.8 0.3 0.1 23.9
Fresh 5,495 289 5.8 0.9 22.0 0.3 0.1 21.0
Sub-total 12,360 303 5.6 1.2 21.9 0.3 0.1 22.7
Inferred Fresh 1,401 249 6.4 0.2 38.4 0.5 0.2 20.8
Sub-total 1,401 249 6.4 0.2 38.4 0.5 0.2 20.8
Total 13,760 298 5.7 1.1 23.5 0.3 0.2 22.5

1 Weathering profile reflects metallurgical sulphide oxidation state. Supporting information on definition and application within the Mineral Resources is provided under Section 3 of the JORC Code Table 1.

2 The NSR has been calculated using metal pricing, recoveries and other payability assumptions for zinc, copper and silver as detailed in ‘Cut-off parameters’ in Section 3 of the attached JORC Code Table 1.

It is Entech’s opinion that all metals used in the NSR calculation have reasonable potential to be extracted, recovered and sold. Tonnages are dry metric tonnes. Minor discrepancies may occur due to rounding.

Data from a total of 58,868 m of drilling from 149 DD and 85 RC drill holes were available for the MRE. Mineralisation interpretations were informed by 104 DD holes intersecting the resource and 66 RC drill holes intersecting the resource, for a total of 5,954 m of drilling intersecting the resource.

The Mineral Resources comprise two key mineralisation styles – massive and disseminated – and three metallurgically defined weathering profiles – oxide, transitional and fresh. A breakdown of Mineral Resources (Table 1) by mineralisation style and weathering profile is presented in Table 2.

3 | P a g e

entech .

Table 2 Sulphur Springs underground zinc-copper Mineral Resource at an A$80/t NSR cut-off by weathering and mineralisation style

Mineral
Resource
Category
Weathering1 Domain Type Tonnes
(kt)
NSR
(A$/t)2
Zinc
(%)
Copper
(%)
Silver
(ppm)
Lead
(%)
Gold
(ppm)
Iron
(%)
Indicated Oxide Massive 202 388 0.2 4.3 19.2 0.1 0.1 30.3
Disseminated 7 156 0.2 2.2 4.1 0.0 0.0 16.5
HW Massive 1 590 15.8 1.4 83.6 0.8 0.4 7.3
Oxide subtotal 209 381 0.3 4.2 18.9 0.1 0.1 29.8
Transitional Massive 5,468 298 5.2 1.4 21.5 0.3 0.1 25.6
Disseminated 505 240 1.9 2.2 7.7 0.2 0.1 15.4
HW Massive 674 495 12.6 0.4 35.6 0.5 0.3 16.5
FW Massive 8 149 4.3 0.4 14.3 0.4 0.0 6.4
Transitional subtotal 6,655 313 5.7 1.4 21.9 0.3 0.2 23.9
Fresh Massive 3,927 293 6.2 0.8 24.2 0.3 0.2 23.5
Disseminated 976 225 3.3 1.4 9.2 0.2 0.1 15.3
HW Massive 366 335 8.4 0.3 31.3 0.6 0.2 13.0
FW Massive 225 411 6.2 1.8 24.2 0.4 0.0 14.9
Fresh subtotal 5,495 289 5.8 0.9 22.0 0.3 0.1 21.0
Indicated Total 12,360 303 5.6 1.2 21.9 0.3 0.2 22.7
Inferred Fresh Massive 1,264 260 6.7 0.2 41.8 0.5 0.3 21.4
Disseminated 136 144 4.1 0.3 6.9 0.2 0.1 15.9
Fresh subtotal 1,401 249 6.4 0.2 38.4 0.5 0.2 20.8
Inferred Total 1,401 249 6.4 0.2 38.4 0.5 0.2 20.8
Total 13,760 298 5.7 1.1 23.5 0.3 0.2 22.5

1 Weathering profile reflects metallurgical sulphide oxidation state. Supporting information on definition and application within the Mineral Resources is provided under Section 3 of the JORC Code Table 1.

2 The NSR has been calculated using metal pricing, recoveries and other payability assumptions for zinc, copper and silver as detailed in ‘Cut-off parameters’ in Section 3 of the attached JORC Code Table 1. It is Entech’s opinion that all metals used in the NSR calculation have reasonable potential to be extracted, recovered and sold.

Tonnages are dry metric tonnes. Minor discrepancies may occur due to rounding.

This MRE includes Inferred Mineral Resources which are unable to have economic considerations applied to them, nor is there certainty that further sampling will enable them to be converted to Measured or Indicated Mineral Resources.

4 | P a g e

entech .

Competent Person’s Statement

The information in the report to which this statement is attached that relates to the Estimation and Reporting of Mineral Resources at the Sulphur Springs zinc-copper deposit is based on information compiled by Ms Jill Irvin, BSc, a Competent Person who is a current Member of the Australian Institute of Geoscientists (MAIG 3035). Ms Irvin, Principal Geologist at Entech Pty Ltd, is an independent consultant to Develop Global Limited (DVP) with sufficient experience relevant to the style of mineralisation and deposit type under consideration and to the activities being 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 . Ms Irvin consents to the inclusion in the report of matters based on her information in the form and context in which it appears.

Entech undertook a site visit to the Sulphur Springs deposit on 21 October 2021 while the RC and DD drilling campaign, to support the 2022 MRE update, was in progress. During the visit, Entech personnel inspected mineralised intersections in drill core (SSD133, hangingwall marker chert, massive and disseminated sulphide mineralisation and footwall dacite) and observed drilling, logging, sampling, QAQC and metadata collection operations.

Drilling Techniques

The first drill program at Sulphur Springs was completed by Miralga Mining in 1986. It consisted of nine RC drill holes that failed to reach target depth and did not intersect significant mineralisation. No assays for these drill holes are included in the database. The first DD hole was completed in 1988.

Drilling between 1990 and 1995 was operated by Sipa Resources Ltd for various joint venture partners. A total of 59 drill holes with RC pre-collars and NQ2-size diamond core tails were completed on approximately 80 m spaced sections. This includes nine drill holes that were re-drilled after the initial drill hole failed to reach the target depth.

Outokumpu managed the drilling for the joint venture partners in 2000 and drilled 19 holes with RC pre-collars and diamond tails to infill the previous drilling and provide material for metallurgical testwork. Most diamond core was HQ size, with some NQ-size core drilled due to drilling difficulties. Some PQ-size core was drilled for metallurgical testwork. A further 22 RC-DD holes were completed by Outokumpu during 2001 to target sulphide mineralisation continuity and for metallurgical and geotechnical testwork. NQ was the preferred size for drill core during this drill program.

CBH Resources Ltd (CBH) drilled 23 RC drill holes in 2005 to test the upper portions of the deposit and potential for open cut mining. During 2007, CBH Sulphur Springs Pty Ltd completed four sterilisation RC drill holes around the mill and stockpile areas and 12 RC drill holes targeting resource infill and extensions to mineralisation.

Venturex Resources Ltd drilled six RC holes in 2012 to target mineralisation in the Inferred Mineral Resource category. Venturex also completed 14 RC-DD holes in 2017, mainly targeting supergene and transitional mineralisation for metallurgical testwork. Most of the drill core is HQ sized; however, PQ

5 | P a g e

entech .

size was used where ground conditions were poor.

The drilling conducted by DVP[3] in 2021 was designed to infill drill Mineral Resources to Indicated status and test for resource extensions. The drilling comprised 33 RC-DD holes and 44 RC drill holes. About 80% of the drill core is HQ size with the remainder being NQ size. This phase of drilling accounts for about 45% of the drill hole samples in the database.

In total, approximately 42% of the drill holes in the database are RC, 7% are diamond and 51% have RC pre-collars with diamond core tails.

An independent resurvey of all pre-2007 drill hole positions was completed by a licensed surveyor for CBH in 2007. After 2007, all hole collar coordinates have been picked up by CBH/Venturex employees using a DGPS. Historical downhole surveys were performed on all holes by either single-shot Eastman camera or REFLEX gyroscope readings. The DVP drilling exclusively used gyroscope readings at 10– 50 m downhole intervals.

The grid system used for the location of all drill holes is MGA_GDA94, Zone 50.

Topographic control is provided by a combination of external survey control, photogrammetry analysis and DGPS readings.

- Sampling and Sub Sampling Techniques

Sipa Resources sampled chips from RC pre-collars on 1 m intervals with a representative portion retained in chip trays. Where the pre-collars drilled through sedimentary rocks in the hangingwall, grab samples from the 1 m samples were composited to 4 m intervals for assay. Core that was mineralised and its immediate footwall and hangingwall was split using a diamond saw and the halfcore was sent for analysis. The core was sampled on approximately 1 m intervals, dependent on mineralisation boundaries. The footwall and poorly mineralised core were selectively sampled every 1–3 m.

Outokumpu sampled mineralised zones in the pre-collars at 1 m intervals using a single-tier riffle splitter and the immediately surrounding material with 2 m composites. Drill core was split into quarters using a diamond saw. Quarter-cores were collected for assay from mineralised zones at approximately 1 m intervals, with sample intervals being based on geological or mineralisation boundaries. Half-cores from selected intervals were sent for metallurgical testwork. A 1–3 m length of less mineralised (or unmineralised) host rock was also sampled with quarter-core for assay.

CBH collected the RC samples from the 2005 drilling at 1 m intervals and used a three-tier riffle splitter to produce samples for assay. A small number of samples were wet, and these were ‘grab’ sampled from the sample bag. The entire samples were weighed, which indicated mostly good sample return. The 2007 RC drilling was sampled in the mineralised zones at 1 m intervals using a spear.

3 ASX. VXR. 7 October 2021. Report: Change of Company Name.

6 | P a g e

entech .

The surrounding host rock was sampled as 10 m composites using a spear.

Venturex sampled the 2012 RC drill holes at 1 m intervals in mineralised domains by an unspecified method. The pre-collars for the 2017 drilling were riffle split into 1 m samples at the cyclone. The 1 m samples were sampled with a scoop to produce 4 m composites, except for the last 10 m of the precollars which were scooped to produce a sample for each metre for assay. The drill core was split into quarter-core using a diamond saw. The quarter-core was sampled at nominally 1 m intervals, with breaks at mineralisation or lithology boundaries.

DVP sampled the 2021 RC drill holes with 1 m splits in the mineralised zones. In the unmineralised areas, 4 m composites were produced by spearing the 1 m samples with a scoop. Composites that returned favourable assays were resampled and assayed from the 1 m RC split samples. The RC sample recovery is visually estimated with approximately 23% of the 1 m splits recorded with recoveries of 10% to 50%. Due to the massive nature of the sulphide mineralisation, Entech considers that sample bias due to loss of fine/coarse material may not have a significant impact on the assay results. A grain size analysis to produce a grade profile would help quantify the impact of the low recoveries. The NQsize diamond core was split in half using a diamond saw. The HQ-size core was split in half using a diamond saw, then one half was split to produce quarter-core. One length of half NQ-size core or one length of quarter HQ-size core were sampled on nominal 1 m intervals, with breaks at mineralisation or rock type boundaries. The core recovery was recorded as good to excellent (92% to 100%).

Sample Analysis Method

Samples from the Sipa Resources drilling up until 1994 were sent to either SGS Australia Pty Ltd (SGS) or Analabs Pty Ltd (Analabs) in Perth. Samples analysed in 1995 were sent to Australian Assay Laboratories (AAL) in Perth. A representative selection of pulps of highly mineralised core was routinely sent to other laboratories for check analysis. Analabs analysed a selection of quarter-core samples that replicated previously sampled half-core and were originally analysed by SGS.

The drill core and RC pre-collar samples from the Outokumpu 2000 drilling were analysed by Genalysis in Perth, with samples assaying greater than 10% zinc and 10% copper also being carried out at ALS Chemex and Analabs. A selection of pulps was sent from Genalysis to Analabs and ALS Chemex, with results comparing well. Duplicates of 43 coarse sample splits from Genalysis were analysed at the three laboratories, and showed good correlation. The drill core and RC pre-collar samples from the 2001 drilling were analysed by Genalysis in Perth. Titration analysis for every sample assaying greater than 10% zinc or 10% copper was carried out by Analabs. A selection of pulps was sent from Genalysis to Analabs, with results comparing well. Duplicates of 67 coarse sample splits were reassayed by Genalysis, with good correlation shown. A selection of pulp samples was re-assayed by Genalysis, with excellent correlation with the original results shown. Due to a lack of available standards, synthetic standards at various grade ranges were created by Gannet Holdings Pty Ltd. A round-robin of 25 samples was sent to four different laboratories to determine the expected values for each standard.

CBH sent the RC samples collected in 2005 to ALS Chemex in Perth for analysis. Field duplicates of

7 | P a g e

entech .

mostly mineralised material were generated from the original field rejects. A series of laboratory resplits from the first sample crush were also analysed. ALS Chemex analysed many laboratory repeats of the original pulverised samples. The standards produced in 2001 were also used during this drill program. ALS inserted many internal standards. The analysis method for the 2007 drilling is not included in the available documents and is assumed to be the same as that used by CBH in 2005.

The sample analysis method used by Venturex for the 2012 drilling is not included in the available documents. Samples from the 2017 drilling were analysed by ALS Laboratories in Perth.

DVP sent the 2021 drill samples to ALS Laboratories in Perth for analysis. Samples with greater than 30% zinc were sent to ALS Vancouver for validation. Several different standards and blanks were inserted at a rate of approximately 1:20. Duplicate RC samples were collected at a rate of 1:20 during sampling at the rig.

Based on documentation review, Entech is of the opinion the sample preparation techniques and analyses are appropriate for the style of deposit and commodity under consideration, and reflect standard techniques available at the time.

Geology and Geological Interpretation

The Sulphur Springs deposit has been classified as a volcanogenic massive sulphide (VMS) zinc-copper deposit located within the Sulphur Springs Group in the central east of the Archaean Pilbara Craton. The Sulphur Springs Group lies within a north–northeasterly trending litho-tectonic zone known as the Lalla Rookh-Western Shaw Structural Corridor (LWSC) that is bound by regional-scale faults.

At deposit scale, Sulphur Springs deposit lithologies intersected in drill holes comprise polymictic breccia, chert, massive and stringer sulphide mineralisation, and felsic volcanic rocks of dacitic composition. Massive pyrite and base metal mineralisation occurs over a 550 m strike length and 600 m down dip extent, and consists of an upper zone of massive sulphide overlying a disseminated/stringer (disseminated) zone. The upper contact of the massive sulphide unit is generally sharp, while the lower contact with the footwall disseminated zone is diffuse, with gradational metal tenor over several metres. There are indications of structural thickening in some mineralisation areas, which has obscured primary morphology and metal zonation.

Lithology and structure are considered the predominant controls on base and precious metals, and gangue (iron) mineralisation at the Sulphur Springs deposit.

Entech interpreted major lithological units to assist with the definition of deposit-scale geology and sulphide mineralisation sequencing as follows:

  • Footwall dacite contact

  • Rhyodacite hangingwall

  • Footwall and hangingwall marker chert horizons

  • Hangingwall marker breccia (interpreted to represent a thrust).

8 | P a g e

entech .

Mineralisation domains were interpreted primarily on geological and mineralisation characterisation models defined by downhole geological contacts and were based on lithology, sulphide characterisation (and distribution), grade tenor, structural models and mapped outcrop geology. Four sulphide mineralisation domains (Figure 1 and Figure 2) were defined as follows:

  • Massive sulphide mineralisation (Domain 1) with a sharp hangingwall contact. The footwall contact was defined either by drill hole logging or by iron and sulphur grades greater than 20%.

  • Disseminated mineralisation (Domain 2) underlying the massive sulphide unit.

  • Hangingwall massive sulphide mineralisation (Domain 3) with two discrete shoots 40–60 m in width of high-tenor zinc mineralisation.

  • Footwall massive sulphide mineralisation (Domain 4).

Zinc and copper distribution within the sulphide domains have consistent geospatial relationships, further outlined below:

  • Zinc-rich mineralisation is most prominent towards the hangingwall of the massive sulphide (Domain 1). Discrete zones of zinc occur towards the footwall of the massive sulphide and are interpreted to be structurally emplaced. Lower-tenor zinc-rich mineralisation is also defined within the footwall disseminated horizon (Domain 2).

  • Copper-rich mineralisation occurs as a semi-continuous lobate lens that straddles the footwall contact between the massive sulphide and underlying disseminated zone, with the majority of the copper mineralisation falling within the massive sulphide horizon.

  • Hangingwall zinc mineralisation (Domain 3) that lies 10–40 m above the massive sulphide is interpreted to be structural repetition of the massive sulphides. There is lower marker breccia below the hangingwall mineralisation that is interpreted as localised thrust faulting. Within the hangingwall mineralisation, massive sulphide mineralisation intercepts were flagged by a sharp hangingwall contact with unmineralised country rock, logged massive sulphide intervals and where logging information was inconclusive, iron and sulphide grades greater than 20% were used to define the footwall contact of the massive sulphide.

  • A north–south post-mineralisation fault (Main fault) is interpreted to offset all sulphide mineralisation domains into two separate lenses (east and west).

Interpretation of massive and disseminated mineralisation was initially undertaken using all available drill holes in Seequent Leapfrog Geo software. Intercepts correlating to massive sulphide and disseminated mineralisation and underpinned by strike continuity implied from lithology wireframes were independently identified and manually selected in Seequent Leapfrog Geo prior to the creation of an implicit vein model. Interpretation was a collaborative process with DVP’s geologists to ensure Entech’s modelling approach represented observations and the current understanding of geological and mineralisation controls.

Entech interpreted and modelled metallurgical and regolith weathering profiles to assist with delineating sulphide mineralisation relationships and recoveries. The metallurgical weathering profile

9 | P a g e

entech .

comprised four distinctive zones – leached, oxide, transitional and fresh – and were determined from field-based observations by DVP personnel of available core photographs to identify areas of vugging or oxidation of sulphides (qualitative observations) and secondly with sequential copper digestion (quantitative measurements). The leached zone, which overlies the oxide zone, has been depleted of all base and precious metal grades and excluded from Mineral Resource tabulations.

Further definition of the metallurgical weathering profiles is presented below:

  • Oxide is defined when chalcocite and covellite represented >50% of copper species. Welldeveloped vuggy sulphides. Gossanous and/ or cavernous textures were evident.

  • Transitional is defined when chalcocite and covellite represented <50% of copper species. Bornite/covellite may be present along with chalcopyrite. Tarnishing was evident on other sulphides (e.g., pyrite). Vugs related to secondary processes were poorly to moderately well developed in sulphide (other than copper species)

  • Fresh is defined when fresh chalcopyrite was the dominant copper sulphide species. No evidence or trace development of vugs. Any vug development was interpreted to have formed due to the dissolution of non-sulphide minerals (e.g., carbonates). No tarnishing of other sulphide species (e.g., pyrite) or secondary copper species was evident.

Zinc and copper metallurgical recovery algorithms were created for each weathering horizon based on metallurgical testwork and were factored into net smelter return (NSR) calculations to reflect recoverable metal in each metallurgical weathering horizon.

==> picture [466 x 239] intentionally omitted <==

Figure 1 Long section of Sulphur Springs zinc-copper deposit (looking towards 145°) showing drill hole traces, massive sulphide and disseminated domains, and topography extents

Note: Mineralised domains (as interpreted) do not represent Mineral Resource classification extents.

10 | P a g e

entech .

==> picture [466 x 239] intentionally omitted <==

Figure 2 Plan view of Sulphur Springs zinc-copper deposit showing drill hole traces and massive and disseminated sulphide domains

Note: Mineralised domains (as interpreted) do not represent Mineral Resource classification extents.

==> picture [478 x 246] intentionally omitted <==

Figure 3 Long section of Sulphur Springs zinc-copper deposit (looking south) showing geological mapping, drill hole traces, massive sulphide domain, and topography extents

Note: Mineralised domains (as interpreted) do not represent Mineral Resource classification extents.

11 | P a g e

entech .

Estimation Methodology

Compositing approaches were selected to honour the mineralisation style, geometry, expected grade variability and potential mining selectivity. Drilling samples were composited to 1 m lengths honouring lode domain boundaries. Composites with a best-fit approach were compiled, whereby any small residual intervals less than 1 m were divided evenly between the composites to mitigate metal loss.

Exploratory data analysis (EDA) of the declustered (20 mN, 5 mE, 20 mZ) composited (density weighted) zinc, lead, copper, gold and silver variables in the mineralised domain groups was undertaken using Supervisor™ software. Analysis for sample bias, domain homogeneity and top capping was undertaken. Further sub-domaining of composite data by weathering (regolith or metallurgical) or lithology boundaries, for the purposes of interpolation, was not supported by statistical and spatial analysis.

Assessment and application of top-capping was undertaken on the zinc, lead, copper, gold, silver and iron variables within individual (and grouped) domains. Domains were capped to address instances where outliers were defined as both statistical and spatial outliers, presented below:

  • Massive: zinc 30%, lead 3%, copper (no cap), silver 300 g/t, gold 1.5 g/t

  • Disseminated: zinc 10%, lead 2%, copper 10%, silver 50 g/t, gold 0.5 g/t

  • Metal reductions from the above caps were minor in nature averaging <3% across all variables within the massive and disseminated domains. Application of silver top cap in the disseminated domain resulted in an 8.5% metal reduction.

  • Iron was not capped.

Variography was undertaken on the capped, declustered zinc, lead, copper, gold, silver and iron variables grouped by mineralisation style (massive, disseminated). Robust variogram models with a low to moderate nugget for zinc, copper and lead (8–10%), gold and silver (10–11%) and iron (15%) were delineated and used in Kriging Neighbourhood Analysis (KNA) to determine parent cell estimation size and optimise search neighbourhoods. Due to statistical and spatial similarities, the variogram and search parameters for zinc were applied to lead. It should be noted that although the maximum continuity modelled in the variograms ranged from 70 m to 80 m (zinc, lead, copper) and from 120 m to 202 m (silver, gold, iron), approximately 35–55% of spatial variability and subsequent kriging weights were applied within 15–60 m.

Interpolation was undertaken using Ordinary Kriging in GEOVIA Surpac™ within parent cell blocks. Dimensions for the interpolation were Y: 5 mN, X: 10 mE, Z: 5 mRL, with sub-celling of Y: 0.312 mN, X: 0.625 mE, Z: 0.312 mRL. The parent block size was selected to provide suitable volume fill, given the available data spacing and mining selectivity. The drill hole spacing for geological and grade domain interpretations averages 40 m × 40 m over the sulphide mineralisation extents. Considerations relating to appropriate block size include drill hole data spacing, conceptual mining method, variogram continuity ranges and search neighbourhood optimisations (KNA).

12 | P a g e

entech .

A two-pass estimation strategy was used, whereby search ranges reflected variogram maximum modelled continuity and a minimum of 6, maximum of 16 composites for zinc, lead and copper, and a minimum of 6, maximum of 12 for gold, silver and iron. The second search reduced the minimum composite required in the neighbourhood to 4; all other parameters (e.g., range and maximum composites) remained the same. Search neighbourhoods broadly reflected the direction of maximum continuity within the plane of mineralisation, ranges, and anisotropy ratios from the variogram models. All blocks which did not meet the criteria to trigger an estimate were not estimated and were excluded from Mineral Resource classification.

Domain and sub-domain boundaries represented hard boundaries, whereby composite samples within that domain were used to estimate blocks within the domain. Global and local validation of the zinc, lead, copper, gold, silver and iron variables estimated outcomes was undertaken with statistical analysis, swath plots and visual comparison (cross and long sections) against input data.

Global comparison of declustered and capped composite mean against estimated mean (by domain and variable) highlighted less than 10% variation for zinc and silver and within 5% variation for copper.

The 3D block model was coded with geology, regolith and metallurgical weathering, mineralisation style, NSR and Mineral Resource classification prior to evaluation for Mineral Resource reporting. Multivariate regressions were calculated for density and sulphur, by metallurgical weathering horizon, and applied directly into the block model.

Classification Criteria

Mineral Resources were classified as Indicated and Inferred to appropriately represent confidence and risk with respect to data quality, drill hole spacing, geological and grade continuity and mineralisation volumes. In Entech’s opinion, the drilling, surveying and sampling undertaken, and the analytical methods and quality controls used, are appropriate for the style of deposit under consideration.

Mineral Resources were classified based on geological and grade continuity confidence drawn directly from:

  • Drill hole methodology, data quality, spacing and orientation

  • Geological domaining

  • Estimation quality parameters

  • Historical mining strike lengths, widths, stope orientations and remnant mining areas.

Indicated Mineral Resources were defined where a moderate level of geological confidence in geometry, continuity, and grade was demonstrated, and were identified as areas where:

  • Blocks were well supported by drill hole data, with drilling averaging a nominal 40 m × 40 m or less between drill holes, or where drilling was within 50 m of the block estimate.

  • Blocks were interpolated with a neighbourhood informed by a 12–16 composites and slope of regression above 0.5.

13 | P a g e

entech .

Inferred Mineral Resources were defined where a lower level of geological confidence in geometry, continuity and grade was demonstrated, and were identified as areas where:

  • Drill spacing was averaging a nominal 60 m or less, or where drilling was within 70 m of the block estimate

  • Blocks were interpolated with a neighbourhood informed by a minimum of 10 samples and slope of regression above 0.2.

Consideration has been given to all factors material to Mineral Resource outcomes, including but not limited to:

  • Confidence in volume and grade delineation, continuity and preferential orientation of mineralisation tenor

  • Quality of data underpinning Mineral Resources

  • Nominal drill hole spacing and estimation quality (conditional bias slope, number of samples, distance to informing samples).

The reported Mineral Resource was constrained at depth by the available drill hole spacing outlined for Inferred classification, nominally 400 m below surface topography. Mineralisation within the model which did not satisfy the criteria for classification as Mineral Resources remained unclassified.

Mineral Resources that are not Ore Reserves do not have demonstrated economic viability. The MRE does not account for selectivity, mining loss and dilution. This MRE update includes Inferred Mineral Resources which are unable to have economic considerations applied to them, nor is there certainty that further sampling will enable them to be converted to Measured or Indicated Mineral Resources.

The delineation of Indicated and Inferred Mineral Resources appropriately reflects the Competent Person’s view on continuity and risk at the deposit.

Cut-off Grade

The NSR cut-off grade used for reporting of Mineral Resources at Sulphur Springs was A$80/t, which is approximately 80% of the break-even stoping cut-off value underpinning DVP’s current Life of Mine Plan (LOMP). The NSR cut-off reflects costs associated with metal recovery and was selected based on discussions with DVP engineers, and benchmarked against previous detailed studies[4] at the project.

The NSR cut-off considers revenue from saleable base metals – zinc, copper (percent) – and silver (ppm) and offsets site operating and sustaining capital costs, including underground operating development. The base metal and precious metals used in the NSR calculation all have reasonable potential of being saleable.

4 Venturex Resources Ltd, ASX release dated 10 October 2018 : Sulphur Springs Feasibility Study confirms longlife, high-margin Australian copper-zinc mine with outstanding economics

14 | P a g e

entech .

The NSR calculation determines a value for the saleable metals by applying the following modifying factors (presented in Table 3):

  • Metal prices

  • Metallurgical recoveries (by metallurgical weathering profile)

  • Payability factors, inclusive of concentrate treatment charges, metal refining charges, payment terms (concentrate), logistics costs and NSR royalties.

Table 33 Key NSR assumptions

Metal FX rate Metal Price Recovery Payability factors
Zinc A$0.69:US$1 A$5199.28/t Zinc recovery algorithm Concentrate treatment charges,
metal refining charges, payment
terms (concentrate), logistics
costs and NSR royalties
Copper A$11678.70/t Copper recovery algorithm
Silver A$27.54/oz 18%¹
28%²

¹Silver recovery for zinc concentrate which includes deportment from cost model.

²Silver recovery for copper concentrate which includes deportment from cost model.

The NSR has been calculated using metal pricing, recoveries and other payability assumptions for zinc, copper and silver as detailed in Section 3 under ‘Cut-off parameters’ in the JORC Code Table 1. It is Entech’s opinion that all metals used in the NSR calculation have reasonable potential to be extracted, recovered and sold.

The metallurgical recovery algorithms for zinc and copper by metallurgical weathering horizon are given in Table 4.

Table 4 Metallurgical recovery algorithms for copper and zinc by metallurgical weathering horizon

Metallurgical
weathering horizon
Zinc recovery algorithm Copper recovery algorithm
Oxide 0.5 * Zn% + 62 *(1 - exp (-0.85 * Zn%)) 92 (1 - exp (-1.0Cu%))
Transitional 0.2 * Zn% + 91 *(1 - exp (-0.7 * Zn%)) 94 *(1 - exp(-1.5 * Cu%))
Fresh 2.5 + 93 *(1 - exp (-1.4 * Zn%)) 1.5/Cu% + 94.5 *(1 - exp (-1.7 * Cu%))

Bulk Density

This MRE contains dry bulk density data collected on drill core from 212 holes (between 1990 and 2022). Density measurements were collected and measured using the water immersion density determination method for each sample.

The density samples were located between 7659400 mN and 7660200 mN, and 728400 mE and 729500 mE, and nominally from the surface to a depth of 550 m, providing a representative density profile between mineralised domains, weathering profile and depth profile within the Mineral Resource area. Analysis of the bulk density data indicated values between 1.64 and 5.01 g/cm[3] SG

15 | P a g e

entech .

(specific gravity).

The metallurgical weathering profile comprises four key horizons: leached, oxide, transitional and fresh. Multi-element regression indicated varying regression coefficients occur across the weathering horizons. Therefore, a separate regression formula was used for oxide, transitional and fresh materials. Note the leached zone is depleted of mineralisation and therefore did not comprise Mineral Resources. A background density was applied in this horizon with adjustments and depletions applied to represent the vuggy nature of the leached zone.

Validation of the regression concluded a correlation coefficient of 0.93 between measured and regression density. Ideally, sulphur would be included in this regression given the close correlation with iron. However, insufficient sampling of sulphur limited the ability to use all measured densities and derive a robust regression formula. In this instance, sulphur was therefore not used in density regressions. Given below are the density regressions applied within the MRE.

  • Oxide: 1.976418 +Zn%0.02795 +Pb%-0.092028 +Cu%-0.003506 +Fe%0.051415

  • Transitional: 2.472249 +Zn%0.022663 +Pb%0.023376 +Cu%0.000101 +Fe%0.043261

  • Fresh:2.526907 +Zn%0.020732 +Pb%0.052578 +Cu%-0.005445 +Fe%0.043606.

Regression formulas were applied in the block model on a block-by-block basis, using estimated zinc, lead, copper and iron values for the individual blocks and restricted by block model coding of metallurgical weathering horizons.

Project History and Historical Mineral Resources

A report of sulphur precipitating in a creek downstream from a felsic volcanic sequence led to the discovery of a sulphidic gossan in 1984 with the project named Sulphur Springs. Surface rock chip sampling revealed anomalous gold and base metal values.

Ashling Resources NL (Ashling) acquired the Sulphur Springs tenements in 1990 and entered a joint venture with Sipa Resources Ltd (Sipa), Guardian Resources NL (Guardian), and Outokumpu Zinc OY (Outokumpu) in 1993. This joint venture continued through until 2005, during which the Sulphur Springs orebody was explored by extensive RC and DD programs.

Regional alteration and geology mapping campaigns were completed over the whole Panorama Trend, producing a geological framework and model for the mineralisation of the belt. Various external geological and mineralisation studies and thesis have been completed on the Panorama Trend, with Sulphur Springs being the basis for many of these studies.

The Sulphur Springs tenements were wholly bought by CBH Sulphur Springs Pty Ltd (CBHSS) in 2006 from Sipa/Outokumpu. CBHSS completed further resource drilling for mineralogical and metallurgical testwork, including testwork of barren hangingwall, and updated resource/reserve estimations. CBHSS proposed mining through open pit method and completed feasibility studies and relevant heritage, biological and hydrological surveys, in preparation for mining and construction. Continuing

16 | P a g e

entech .

optimisation studies were completed for plant design, mine design and other associated infrastructure.

In 2010, Venturex Resources Limited acquired CBHSS, which was subsequently renamed Venturex Sulphur Springs Pty Ltd. In December 2013, Venturex Resources Ltd published a definitive feasibility study (DFS) of all its Pilbara holdings, including Sulphur Springs, to evaluate all production options.

In February 2021, Venturex Resources Ltd announced a re-capitalisation plan and equity raising. The company subsequently changed its name from Venturex to Develop Global in October 2021.

Mineral resources (not prepared under the guidelines of the JORC Code) were publicly reported in annual reports of various companies in 1994, 1996, 2001 and 2006.

The published Ore Reserves reported in June 2006 for the Sulphur Springs deposit was 10 Mt grading at 3.5% zinc, 1.4% copper and 17 g/t silver.

The last publicly reported MRE was the 2018 Sulphur Springs Resource[5] , prepared by Mil Min Pty Ltd under the guidelines of the JORC Code, reported Indicated and Inferred Mineral Resources of 13.8 Mt grading at 3.8% zinc, 1.5% copper, 0.2% lead, 0.1 g/t gold and 18 g/t silver.

By comparison, approaches to domaining, classification, reasonable prospects for eventual economic extraction (RPEEE) (application of NSR cut-off) undertaken by Entech and the addition of 77 RC and DD drilling completed by DVP in 2021–2022 account for the variations from historical Mineral Resources.

Key differences in approach included:

  • Inclusion of 77 additional resource definition and infill drill holes providing increased volume delineation of discrete lenses and zinc and copper sub-domains. This approach was implemented across all other lenses and varied from the Mil Min Pty Ltd approach, which included internal waste in broader sulphide domains.

  • Change in Mineral Resource classification and reporting criteria from ‘0.4% Cu or Cu less than 0.4 with more than 2% Zn’[5] , in 2018 MRE to the current (2022) NSR-based approach.

Assessment of Reasonable Prospects for Eventual Economic Extraction

Entech assessed the Sulphur Springs MRE, as reported, as meeting the criterion for RPEEE based on the following considerations.

Mining

The Sulphur Springs MRE extends from the topographic surface to approximately 400 m below surface. Entech considers material at this depth, and at the grades estimated, would fall under the

5 MM_505_Sulphur_Springs_Resource_Report_March_2018

17 | P a g e

entech .

definition of RPEEE in an underground mining framework.

The MRE is reported using an NSR cut-off of A$80/t. For the purposes of NSR determination, NSR values were calculated, by metallurgical weathering domains, using estimated zinc, copper (per cent) and silver values (ppm), on a block-by-block basis prior to implementing reporting cut-offs. The metal components of the NSR calculation all have reasonable potential of being saleable. Entech considers the NSR cut-offs appropriately reflect costs associated with metal recovery and would fall within the definition of RPEEE in an underground framework.

Entech understands DVP plans to implement mechanised underground mining methods. No mining dilution or cost factors was applied to the estimate. No factors or assumptions were made within the MRE with respect to environmental considerations.

Variances to the tonnage, grade and metal of the Mineral Resources are expected with further definition drilling. The Mineral Resources may also be affected by subsequent assessment of mining, environmental, processing, permitting, taxation, socio-economic and other factors.

It is the Competent Person’s opinion that the proposed underground mining methods and cut-off grades applied satisfy the requirements for RPEEE.

Metallurgy

Metallurgical recovery factors have been factored into NSR calculations based on inputs supplied by DVP and a review of previous detailed studies[4] at the project.

Entech understands that metallurgical amenability and recovery factors for oxide (supergene), transitional and fresh material were addressed by a number of testwork programs based on historical metallurgical testwork for fresh material and during the 2018 DFS, with holes SSD089 to SSD102 sampled for testing of oxide and transitional material.

Historical metallurgical testwork focused on fresh material, resulting in a recommendation to use selective sequential flotation to produce separate copper- and zinc-rich concentrates with high mineral recoveries at target grades.

Recovery algorithms for copper and zinc have been determined for each metallurgical weathering horizon based on historical testwork and feasibility studies, and have been factored into NSR calculations.

A global silver recovery, including deportment from cost model of 18% and 28% for zinc and copper concentrates, respectively, was factored into NSR calculations.

Entech understands from discussions (with DVP personnel), documentation reviews (supplied by DVP) and project site inspections that no other deleterious variables, which would materially affect eventual economic extraction of Mineral Resources, have been identified at the project. No factors or assumptions were made within the MRE with respect to deleterious elements or by-products.

18 | P a g e

entech .

END.

19 | P a g e

entech .

COMPETENT PERSON’S CONSENT FORM

Pursuant to the requirements of ASX Listing Rules 5.6, 5.22 and 5.24 and clause 9 of the 2012 JORC Code (Written Consent Statement)

Report Description

Report: Sulphur Springs Zinc-Copper Project, WA. Total Resource increases 15% to 1.3 Mt of contained ZnEq[1]

Releasing Company: Develop Global Limited

Deposit Name: Sulphur Springs Zinc-Copper Deposit

Date: 5 September 2022

Statement

I, Jillian Irvin, confirm that I am the Competent Person (Estimation and Reporting of Mineral Resources) for the Report, and:

  • I have read and understood the requirements of the 2012 edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code, 2012 edition).

  • I am a Competent Person as defined by the JORC Code, 2012 edition, having five years’ experience that is relevant to the style of mineralisation and type of deposit described in the Report, and to the activity for which I am accepting responsibility.

  • I am a Member of the Australian Institute of Geoscientists (MAIG 3035).

  • I have reviewed the Report to which this Consent Statement applies.

  • I am a consultant working for Entech Pty Ltd and have been engaged by Develop Global Limited to prepare the documentation for the Sulphur Springs Underground Mineral Resource Estimate on which the Report is based, for the period ending 31[st] December 2022.

I have disclosed to the reporting company the full nature of the relationship between myself and the company, including any issue that could be perceived by investors as a conflict of interest.

I verify that the Report is based on and fairly and accurately reflects in the form and context in which it appears, the information in my supporting documentation relating to Mineral Resources.

20 | P a g e

entech .

CONSENT

I consent to the release of the Report and this Consent Statement by the directors of:

Develop Global Limited.

==> picture [151 x 60] intentionally omitted <==

5 September 2022

Signature of Competent Person

Date

Professional Membership: Membership Number:

Australian Institute of Geoscientists MAIG (3035)

==> picture [90 x 51] intentionally omitted <==

Ruth Jupp (MAIG 7377)

Signature of Witness

West Perth, Western Australia

21 | P a g e

entech .

Additional Deposits covered by the Report for which the Competent Person signing this form is accepting responsibility:

NONE........................................................................................................................................................ .................................................................................................................................................................. .................................................................................................................................................................. ..................................................................................................................................................................

Additional Reports related to the deposit for which the Competent Person signing this form is accepting responsibility:

NONE........................................................................................................................................................ .................................................................................................................................................................. .................................................................................................................................................................. ..................................................................................................................................................................

==> picture [151 x 60] intentionally omitted <==

5 September 2022

Signature of Competent Person

Date

Professional Membership: Australian Institute of Geoscientists Membership Number: MAIG (3035)

==> picture [90 x 51] intentionally omitted <==

Ruth Jupp (MAIG 7377)

Signature of Witness

West Perth, Western Australia

22 | P a g e

SECTION 1 SAMPLING TECHNIQUES AND DATA

(Criteria in this section apply to all succeeding sections.)

Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. 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.

The deposit was sampled with a combination of reverse circulation (RC) and diamond drill (DD) holes completed on a
variable spacing across the deposit to a maximum vertical depth of approximately 800 m. The RC drill holes were
sampled via an industry-standard cyclone and riffle splitter system from the recovered sample. Diamond drill core
was sampled using standard cut half-core, or where metallurgical samples were taken, quarter-core was used.

Diamond core was oriented, aligned and cut on geologically determined intervals in the range from 0.15 m to 2.1 m.

Include reference to measures taken to
ensure sample representivity and the
appropriate calibration of any
measurement tools or systems used.

Industry-standard RC drilling produced whole metre RC drill samples that were split at the rig using a cone splitter to
produce samples weighing approximately 3 kg. Diamond drilling was completed to industry standard using
predominantly NQ size core prior to 2017, with HQ being the most common size used during 2017 and 2021 drilling.

The whole samples from the drilling were individually weighed, dried, stage crushed and pulverised to nominally
minus 75 μm or 200 mesh (total preparation) to produce a pulp which was sub-sampled for analysis.

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 (e.g. ‘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
(e.g. submarine nodules) may warrant
disclosure of detailed information.

RC and DD drilling was used to obtain a 1 m sample (on average) from which samples were crushed and then
pulverised in a ring pulveriser (LM5) to a nominal 90% passing 75 μm. For each interval, a 250 g pulp sub-sample was
taken; these were then split to a 50 g charge weight for fire assaying, with checks routinely undertaken.
Drilling techniques
Drill type (e.g. core, reverse circulation,
open-hole hammer, rotary air blast,
auger, Bangka, sonic, etc) and details
(e.g. core diameter, triple or standard

A total of 58,868 m of drilling from 149 diamond and diamond tails, and 85 RC drill holes were available for the
Mineral Resource estimate (MRE).

RC drilling prior to 2007 concentrated on shallow, near-surface exploration targets. More recent drilling targeted
deep massive mineralisation with hole depths averaging ~380 m.

1

Criteria JORC Code explanation Commentary
tube, depth of diamond tails, face-
sampling bit or other type, whether
core is oriented and if so, by what
method, etc).

DD procedures, core sizes and recoveries have varied over the years. Most historical surface drill holes were cored at
NQ size; more recent drilling has been predominantly HQ, with some PQ in poor ground conditions or in holes drilled
for metallurgical testwork.

Drill core orientation has been performed on DD holes completed since 2000. The orientation line is preserved on the
portion of core remaining in the core tray after sampling.
Drill sample recovery
Method of recording and assessing core
and chip sample recoveries and results
assessed.

During DD campaigns, cores were laid out in standard core trays, marked and oriented, and recoveries calculated.

Core recoveries are generally fair to good, with an average recovery of about 98%. Some holes that started coring
closer to surface encountered more cavernous zones with poor recovery.

Historical documentation does not record RC recoveries. For the 2021 RC drilling, the recovery is recorded on the
sampling sheet, based on visual inspection. About 23% of the 1 m splits reported recoveries of 10% to 50%.

Measures taken to maximise sample
recovery and ensure representative
nature of the samples.

Powerful RC rigs were used during the 2021 drilling to improve the recovery of chip samples from the deep drill
holes.

Triple tube was used for some recent HQ and PQ core drilling to improve drill core recoveries in areas of poor ground.

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.

No relationship between sample recovery and grade tenor was identified or observed. However, a grain size analysis
should be conducted to generate a grade profile for the massive sulphide mineralisation due to the low recoveries for
some RC samples in this zone.
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.

DD holes were geologically logged in their entirety and photographed. Representative areas of diamond drilling were
logged for geotechnical purposes. RC drill holes were all qualitatively logged and representative sieved and washed
chips collected and stored in chip trays.

Logging by all operators was at an appropriate detailed quantitative standard to support future geological, Mineral
Resource and Ore Reserve estimations and technical/economic studies.

All holes were logged in full.

Whether logging is qualitative or
quantitative in nature. Core (or costean,
channel, etc) photography.

Entech’s review of available drill hole data in the database shows the level of detail of geological logging varies year
to year – from capture of base lithology through to more comprehensive detail, including lithology, structure,
mineralogy, alteration and weathering (oxidation state) for both RC samples and DD core.

Logging is both qualitative and quantitative. Visual percentage estimates for lithology, mineralogy, mineralisation,
structure (where possible in core only), weathering and features were routinely recorded, with summary comments
provided.

All DD core has been photographed.

The total length and percentage of the
relevant intersections logged.

No drill logs are available for the RC drill holes completed in 1986.

Less than 1% of all other drill holes in the database were not logged.
Sub-sampling
techniques and sample
preparation

If core, whether cut or sawn and
whether quarter, half or all core taken.

DD core was sawn with a diamond saw. Half-core samples (quarter-core in some metallurgical holes) were taken for
assay.

If non-core, whether riffled, tube

1 m RC samples were collected and split off the drill rigusinga splitter. Approximately90% of the samples were dry.

2

Criteria JORC Code explanation Commentary
sampled, rotary split, etc and whether
sampled wet or dry.
In areas of no mineralisation, these 1 m samples were composited to 4 m samples. Zones of mineralisation were
sampled or re-split at 1 m intervals.

For all sample types, the nature, quality
and appropriateness of the sample
preparation technique.

Based on the documentation review, Entech is of the opinion the sample preparation techniques are appropriate for
the style of deposit and commodity under consideration, and reflect standard techniques available at the time.

Quality control procedures adopted for
all sub-sampling stages to maximise
representivity of samples.

Prior to 2005, it appears the company did not include QAQC samples in the sample submissions; however, the
laboratory inserted its own internal QAQC checks.

From 2005 to 2012, company QAQC samples were included with the drill samples. Since 2017, the blanks and
certified reference materials (CRMs) were included at a rate of about 1:20 samples. Duplicate samples were also
collected at a rate of 1:20 samples.

The procedures implemented since 2017 meet current industry standards.

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.

Approximately 200 field duplicate samples have been collected from chips and 20 from quarter drill core at Sulphur
Springs. The duplicate samples correlate reasonably well, with some spread in results as expected. Some individual
assays do not correlate well.

Whether sample sizes are appropriate
to the grain size of the material being
sampled.

In Entech’s opinion, the sample sizes are industry standard and appropriate to represent mineralisation at the
Sulphur Springs deposit based on the style of mineralisation, thickness and consistency of mineralised intersections,
the sampling methodology and the observed assay ranges.
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.

Over the project life, four different assaying facilities in Perth have been used. Analytical techniques involve either a
three-acid or a four-acid digest with a multi-element suite ICP-MS finish (30 g fire assay (FA) with AAS for precious
metals). Samples were split into high sulphide and low sulphide types on submission to ensure appropriate digestion
and quality analysis. Sulphur was determined by LECO methods. All methods of analysis are considered to provide
‘total’ assay values.

QAQC using re-submitted pulps and external check assays, blind blanks and reference standards has been applied to
samples assayed. Depending on the operator, between 5% and 10% of the assays relate to QAQC procedures. An
independent analysis of intra- and inter-laboratory bias and precision was undertaken in 2007 by then-owner, CBH
Resources. The results of this and subsequent QAQC work indicate there is no material bias to assay results used for
this MRE.

Based on documentation review, Entech is of the opinion the assaying and laboratory procedures are appropriate for
the style of deposit and commodity under consideration, and reflect standard techniques available at the time.
The described analytical methods are considered to be total assaying techniques:
o
Multi-element analyses by acid digestion and determination by AAS, ICP, ICP-AES with the assumption that
digestion is a total dissolution.
o
Multi-element analyses of a pulverised and pressed aliquot by XRD and XRF.
o
Gold determination by FA with an AAS finish.

For geophysical tools, spectrometers,
handheld XRF instruments, etc, the

No geophysical tools were used to determine any element concentrations reported.

3

Criteria JORC Code explanation Commentary
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 (ie lack of bias) and precision
have been established.

Entech completed a review of QAQC procedures. Key points and findings are summarised as follows:
o
Prior to 2005, it appears the company did not include QAQC samples in the sample submissions; however, the
laboratory inserted its own internal QAQC checks. From 2005 to 2012, company QAQC samples were included
with the drill samples.
o Since 2017, blanks and CRMs were included at a rate of about 1:20 samples. Duplicate samples were also
collected at a rate of 1:20 samples.
o The procedures implemented since 2017 meet current industry standards.
o No gold CRMs have been used in the most recent drill programs; however, several different commercially
available gold CRMs were used with the earlier drilling programs.
o There is a small bias shown for some gold CRMs; however, the bias is not consistently positive or negative.
o Numerous different commercially available base metal CRMs have been used with the Sulphur Springs drilling.
The most recently used CRMs are commercially available and have been prepared by Ore Research and
Exploration P/L (OREAS).
o There is a bias shown for some base metal CRMs; however, the bias is not consistently positive or negative.
Several CRMs have been labelled incorrectly.
o The base metal CRMs used for the 2017–2019 drilling are commercially available and were prepared by Geostats
Pty Ltd. These CRMs had similar issues with samples being labelled incorrectly.
o Other CRMs were used for pre-2017 drilling but, based on the data provided, Entech was not able to determine
when they were used and which drill programs they were associated with. These older CRMs are generally
within acceptable limits, with a small bias and the occasional result outside acceptable limits.
o The number of base metal CRMs submitted represents about 5% of the total samples assayed since 2005.
o A certified blank (OREAS c27e) prepared by OREAS was used during the 2021 drilling program. Three other
blanks of unknown origin were used for the earlier drilling.
o The number of blanks submitted represents about 3% of the total samples assayed.
o Most blank assays are below acceptable limits; however, there is evidence of contamination between some
samples. Incorrect labelling of blanks has also occurred. Entech is unable to determine if follow-up and
re-assaying of drill samples due to contaminated blanks was completed. The data provided to Entech are not in a
form that allows these contaminated samples to be correlated to specific drill holes or intervals.
o Approximately 200 field duplicate samples have been collected from chips and 20 from quarter drill core. The
duplicate samples correlate reasonably well, with some spread in results as expected.
o Laboratory checks have been conducted on approximately 2,600 samples of different sample types, including
chips, high-sulphur drill core, half-core and quarter-core. The correlation is better than the field duplicates.
o No umpire checks at alternative laboratories have been conducted.

4

Criteria JORC Code explanation Commentary
Verification of sampling
and assaying

The verification of significant
intersections by either independent or
alternative company personnel.

Prior to 2011, verification procedures are not documented. However, inspection of retained core indicates that
recorded locations of mineralisation are correct. After 2011, significant intersections were checked by senior
company personnel. Significant intersections are also verified by portable XRF data collected in the field and cross-
checked against the final assays when received.

A range of primary data collection methods were employed since 1989. Since 2007, data recording used a set of
standard MS Excel templates on a data logger and uploaded to a Notebook computer. The data are sent to Perth
head office for verification and compilation into an SQL database by the in-house database administrator. Full copies
are stored off site. Full database verification of all historical information was completed in 2007 by CBH Resources. All
data are loaded and stored in a DataShed database.
~~•~~
The historical data (pre-2007) have been adjusted – all negative assays, representing below detection assays, were
converted to positive assays of half the stated assay detection limit.

The use of twinned holes.

No twinned holes have been drilled.

Documentation of primary data, data
entry procedures, data verification,
data storage (physical and electronic)
protocols.

A range of primary data collection methods have been employed since 1989. Since 2007, data recording used a set of
standard MS Excel templates on a data logger and uploaded to a Notebook computer. The data are sent to Perth
office for verification and compilation into an SQL database by the in-house database administrator. Full copies are
stored off site. Full database verification of all historical information was completed in 2007 by CBH Resources. All
data are loaded and stored in a DataShed database.

The historical data (pre-2007) have been adjusted – all negative assays, representing below detection assays, were
converted to positive assays of half the stated assay detection limit.

Discuss any adjustment to assay data.

No assay data have been adjusted for this MRE.
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.

MGA_GDA94, Zone 50 (MGA94_50) is the grid system covering the region.

Drill hole collar locations:
o
A full independent re-survey of all pre-2007 hole positions was completed by a licensed surveyor for CBH
Resources in 2007. After 2007, all hole collar coordinates have been picked up by CBH/DVP employees using a
DGPS with all coordinates and elevation (RL) data considered reliable.

Downhole surveying and accuracy:
o
Downhole surveys were performed on all holes by either single-shot Eastman camera or REFLEX gyroscope
readings at 10–50 m downhole intervals.

Adjustments to the collar elevations of 36 drill holes for instances where GPS elevations did not correlate with
adjacent DGPS drill holes on the same drill pad.

Downhole survey azimuths for drill holes SSD001 to SSD088 were re-converted from local mine grid to MGA94_50
using a correction of +22°.

Specification of the grid system used.

All MRE coordinates are in MGA94_50 grid coordinate system.

Quality and adequacy of topographic
control.

A digital terrain model (DTM) dated 2016 correlates with DGPS collar elevations; however, the source data origins
and accuracy of the DTM are unknown.

Topographic control is provided by combination of external survey control, photogrammetry analysis and DGPS
readings.

5

Criteria JORC Code explanation Commentary
Data spacing and
distribution

Data spacing for reporting of
Exploration Results.

No Exploration Results are being reported as part of this MRE

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.

The resource definition drilling is variably spaced, nominally 40 m × 40 m centres.

Entech considers the data spacing to be sufficient to demonstrate the continuity of both the geology and the
mineralisation. The spacing is sufficient to define a Mineral Resource for the Sulphur Springs zinc-copper deposit.

Most lengths range between 0.1 m and 1.1 m, with longer sample lengths limited to composited samples.

Whether sample compositing has been
applied.

For MRE purposes, a 1 m composite (base and other metals) was generated.
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.

Sulphur Springs comprises massive pyrite and base metal mineralisation bound within a 550 m × 550 m area and
600 m depth extent, and consists of an upper zone of massive sulphide overlying a disseminated/stringer zone.
A subparallel hangingwall horizon lies 10–40 m above the massive sulphide. Across-strike widths vary from 1 m to
<40 m.

Mineralisation is offset by a steeply dipping north–south oriented fault (Main fault) which divides the mineralisation
into the east and west lenses.

The average orientation of the sulphide mineralisation is east–west, dipping on average 50° to the north, plunging
slightly (003) to the northeast.

All holes have been collared from surface. The RC and DD holes were drilled in a fan array from a limited number of
drill pad locations constrained by topography.

Drill hole coverage for geological and grade domain interpretations averages 40 m × 40 m over the sulphide
mineralisation extents.

Both RC and DD holes were drilled from locations in the hangingwall, with some hole orientations at a low angle to
mineralisation due to fan drill angles and spatial constraints associated with topography.

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.

Entech considers the predominant drilling orientation is suitable for mineralisation volume delineation at the Sulphur
Springs deposit and does not introduce bias or pose a material risk to the MRE.
Sample security
The measures taken to ensure sample
security.

Independent audits of the data in 2002 and 2006 concluded that the sampling protocols were adequate.

After 2011, the chain of custody was managed by Venturex. The samples were transported by Venturex personnel to
Whim Creek, stored in a secure facility and collected from site by Toll IPEC and delivered to the assay laboratory in
Perth. Online tracking was used to track the progress of batches of samples.
Audits or reviews
The results of any audits or reviews of
sampling techniques and data.

Independent audits of the sampling techniques and data were completed as part of previous and current feasibility
studies in 2002 (McDonald Spiejers Pty Ltd), 2006 (Golder Associates), 2008 (Zilloc Pty Ltd) and 2011 (Snowden).

The studies were comprehensive and cover all industrystandard issues. There does not appear to be anysignificant

6

Criteria JORC Code explanation Commentary
risk in accepting the data as valid.

Entech conducted a site visit in 2021 and did not identify any material issues or risks pertaining to the MRE

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 Sulphur Springs deposit is located within M45/454. The registered owner of the tenement is Venturex Sulphur
Springs Pty Ltd, a wholly owned subsidiary of Develop Global Ltd. The prospects are held by Venturex Sulphur Springs
Pty Ltd.

The following is extracted from the annual report on exploration activities during 2011, prepared by GEOS Mineral
Consultants:
o
A licence covering 952 ha was granted to Ashling Resources NL (Ashling) on 22 October 1990 for a period of 21
years, expiring on 21 October 2011.
o
On 7 May 1991, a joint venture agreement was registered between Burmine Exploration and Development and
Ashling. At the same time, a 10% share in M45/494 was registered in favour of Guardian Resources NL (the name
was subsequently changed to Guardian Resources Limited, and the company was later acquired by Compass
Resources NL).
o
On 10 March 1993, a farm-in and joint venture and Heads of Agreement was registered between Sipa Resources
Limited (Sipa), Guardian Resources NL, Sipa Resources International NL, Outokumpu Zinc OY (Outokumpu) and
Ashling. On 23 June 1993, Guardian’s 10% share was transferred to Sipa and later that year (1 October 1993)
Guardian’s interest was assigned to Sipa and Outokumpu’s interest was assigned to Outokumpu Zinc Australia Pty
Ltd (Outokumpu Aus).
o
On 5 July 1994, Outokumpu Aus was registered as having a 60% ownership while Ashling retained 15.6% and Sipa
retained 24.4%. Sipa later (30 April 2004) transferred its interest to a wholly owned subsidiary, Sipa Resources
(1987) Limited (Sipa 1987).
o
On 7 June 2005, the 60% interest of Outokumpu Aus was transferred back to Sipa 1987.
o
On 24 May 2006, 100% title was transferred to CBH Sulphur Springs Pty Ltd, under the terms of the Agreement
for Sale of Sulphur Springs tenements dated 11 May 2005 between Outokumpu Aus, Outokumpu, Sipa 1987,
Ashling, Sipa, CBHSS and CBH Resources. As part of this agreement, a mortgage was lodged on 29 November
2006 in favour of Outokumpu Aus in respect of the 100% ownership by CBHSS. The mortgage was discharged on
25 January 2008.
o
In 2010, Venturex Resources Limited acquired CBHSS, which was subsequently renamed to Venturex Sulphur
Springs Pty Ltd.

The tenement is within Njamal Native Title Claim (WC99/8) where native title has been determined. The traditional
owners of the land are the Njamal People. Thegrant of the tenementpredates native title and the tenement is not

7

Criteria JORC Code explanation Commentary
subject to native title claim.

The security of the tenure held at the
time of reporting along with any known
impediments to obtaining a license to
operate in the area.

The tenement is subject to two third-party royalties on any production from the tenement.

The tenement is in good standing and no known impediments exist.
Exploration done by
other parties

Acknowledgment and appraisal of
exploration by other parties.

Previous exploration has been undertaken by several parties going back over 30 years. Modern exploration has been
undertaken by Sipa Resources, CBH Resources, Homestake Mining and Venturex Resources.

The following are excerpts taken from various company annual reports:
o
Ashling Resources NL (Ashling) acquired the Sulphur Springs tenements in 1990 and entered a joint venture with
Sipa Resources Ltd (Sipa), Guardian Resources NL (Guardian), and Outokumpu Zinc OY (Outokumpu) in 1993. This
joint venture continued through until 2005, during which the Sulphur Springs orebody was explored by extensive
RC and DD programs.
o
Regional alteration and geology mapping campaigns were completed over the whole Panorama Trend district,
producing a geological framework and model for the mineralisation of the belt. Various external geological and
mineralisation studies and theses have been completed on the Panorama Trend, with Sulphur Springs being the
basis for many of these studies.
o
The Sulphur Springs tenements were wholly bought by CBH Sulphur Springs Pty Ltd (CBHSS) in 2006 from
Sipa/Outokumpu. CBHSS completed further resource drilling for mineralogical and metallurgical testwork,
including testwork of barren hangingwall material, and updated the resource/reserve estimations. CBHSS
proposed mining through open pit method and completed feasibility studies and relevant heritage, biological and
hydrological surveys in preparation for mining and construction. Continuing optimisation studies were completed
for plant design, mine design and other associated infrastructure.
o
In 2010, Venturex Resources Limited acquired CBHSS, which was subsequently renamed Venturex Sulphur
Springs Pty Ltd. In late 2013, Venturex purchased the mining lease containing the Kangaroo Caves deposit and
several prospecting licences to the southwest from Sipa Resources Ltd.
o
In December 2013, Venturex Resources Ltd published a definitive feasibility study (DFS) on all its Pilbara holdings,
including Sulphur Springs, to evaluate all production options.
o
In February 2021, Venturex Resources Ltd announced a re-capitalisation plan and equity raising. Subsequent to
this, the company changed its name from Venturex to Develop Global in October 2021.

The following is an executive summary of the exploration history of the Sulphur Springs project:
o
A report of sulphur precipitating in a creek downstream from a felsic volcanic sequence led to the discovery of a
sulphidic gossan in 1984. Surface rock chip sampling revealed anomalous gold and base metal values.
o
1987 to 1989 - Drilling and mapping carried out on behalf of Miralga Mining was centred on an 8 km2area around
the gossan outcrop. Nine shallow RC holes were centred over the gossan, but target depths were not achieved
because of cavernous ground conditions within the gossan.
o
1989 - Homestake withdrew from the joint venture during the March quarter. Miralga Mining entered a joint
venture with Sipa/Ashling in June 1989 on tenements 845/419 and E45/581.
o
1989 to 1992 - Discoveryof volcanogenic massive sulphide(VMS)at Sulphur Springs bySipa Resources and

8

Criteria JORC Code explanation Commentary
Ashling Resources NL.
o
1993 to 2000 - Continued exploration and discovery of other VMS potential areas by Sipa Resources and Ashling
Resources NL in joint venture with Outokumpu Zinc Australia Pty Ltd.
o
1993 - A total of 18 drill holes for 7,869 m were completed geophysical surveying including SIROTEM (fixed loop,
in loop, FREM and DHTEM), ground magnetics, gravity and Crone DHTEM.
o
1994 - A total of 16 DD holes for 6,458 m were drilled and a maiden MRE (Indicated and Inferred) of 3.3 Mt
grading at 11% zinc and 2.9 Mt grading at 4% copper and 1% zinc, was declared.
o
1995 - Three DD holes and two extensions for 2,423 m were completed, and 171 geochemical samples were
collected.
o
1996 - Indicated and Inferred MRE of 2.8 Mt grading at 10.7% zinc and 0.6% copper
o
1999 - Pre-feasibility study (PFS), including geological review, preliminary mine plan, review of surface
infrastructure, water resource assessment, process modelling, CAPEX/OPEX estimates.
o
2000 to 2002 - Outokumpu Zinc Australia Pty Ltd completed a total of 19 RC-DD holes to infill the drill pattern.
A revised MRE was produced, and other studies relating to mining, metallurgy, mineralogy, environment, and
native title commenced. Completion of Stage 1 of the feasibility study and commencement of Stage 2. Other
studies relating to mining, metallurgy, mineralogy, environment, and native title commenced.
o
2002 to 2004 - RC drilling (23 holes for 1,941 m) and collection of 14 metallurgical samples by Sipa Resources.
o
2004 - Project was taken over by CBH Resources
o
2004 to 2012 - Water bore drilling (14 holes for 1,287 m). Mineralogical characterisation, metallurgical testwork,
flora and fauna studies, and native title survey were carried out.
o
2012 - Venturex Resources acquired the Sulphur Springs project from CBH Resources.
o
2012 to 2020 - Various resource definition and exploration drilling campaigns completed. Re-optimisation study
and reprocessing of existing DHTEM data from seven holes drilled into the Sulphur Springs deposit.
o
2020 - Primary approval for the Sulphur Springs project was granted by the Western Australian Minister for
Environment.
o
2021 - Venturex Resources Ltd announced a re-capitalisation plan and name change to Develop Global (DVP).
o
2021 to present - 89 RC and DD holes drilled for a total of 21,148.7 m, including 72 resource infill holes and 17
geotechnical DD holes.
Geology
Deposit type, geological setting and
style of mineralisation.

Project is located approximately 144 km southeast of Port Hedland and 57 km west of Marble Bar along the 27 km
Panorama Trend within the Sulphur Springs Group and has been classified as a VMS zinc-copper deposit located in the
central east of the Archaean Pilbara Craton.

The Sulphur Springs Group lies within a north–northeasterly trending litho-tectonic zone known as the Lalla Rookh-
Western Shaw Structural Corridor (LWSC) that is bound by regional-scale faults.

Deposit lithologies in the upper part of the Kangaroo Caves Formation which are intersected in drill holes comprise
polymict breccia, chert, massive and stringer sulphide mineralisation, and felsic volcanic rocks of dacitic composition.

Base metal mineralisation lies within the upper part of the Kangaroo Caves Formation.

The massive pyrite and base metal mineralisation occurs over a 550 m strike length and 600 m down dip extent, and
consists of an upper zone of massive sulphide overlyinga disseminated/stringer zone. The upper contact of the

9

Criteria JORC Code explanation Commentary
massive sulphide unit is generally sharp, while the lower contact with the underlying disseminated/stringer
mineralisation is diffuse/gradational. Sulphide mineralisation appears to have been structurally thickened, which has
obscured primary morphology and metal zonation, resulting in distinctive geospatial distribution of base metals.

Massive sulphide horizon widths vary from less than 2 m at the periphery up to 40 m in the central part of the east
and west lenses, while the lower disseminated stringer zone has more variable widths – between 2 m and 20 m.

The following major mineralisation styles and relationships are recognised:
o
Zinc-rich mineralisation is most prominent towards the hangingwall of the massive sulphide. Discrete zones of
zinc occur towards the footwall of the massive sulphide and are interpreted to be structural emplacement. Lower
tenor zinc-rich mineralisation is also defined within the footwall.
o
Copper-rich mineralisation is most prominent towards the footwall of the massive and upper disseminated area
of sulphide mineralisation.
o
Hangingwall zinc mineralisation that lies 10–40 m above the massive sulphide is interpreted to be structural
repletion of the massive sulphides. There is low marker breccia below the hangingwall mineralisation that is
interpreted as localised thrust faulting.

The principal zinc mineral is a pale brown–coloured, iron-poor sphalerite occurring as fine-grained disseminations
throughout the sulphide mineralisation, but is preferentially concentrated with pyrite in massive sulphide lenses
towards the hangingwall of the massive sulphides. Fine-grained galena occurs as discrete, localised mineralisation.

The principal copper mineral is chalcopyrite, occurring as pervasive coarse disseminations, veins and fracture infill
concentrated towards the footwall of the massive sulphide and hangingwall of the disseminated sulphide. Minor
amounts of bornite and tennantite–tetrahedrite have been noted. Chalcocite has been noted in some of the shallower
weathered intersections. Malachite is prominent in the gossan.

Sulphide mineralisation is offset by a steeply dipping north–south oriented fault (Main fault) which divides the
mineralisation into the east and west lenses.

Drill holes intersecting the Main fault area show significant intersections of breccia, which is interpreted to be growth
fault breccia that is not mineralised.
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:
o easting and northing of the drill
hole collar
o elevation or RL (Reduced Level –
elevation above sea level in metres)
of the drill hole collar
o dip and azimuth of the hole
o down hole length and interception
depth

No Exploration Results are being reported as part of this MRE.

All relevant drill holes used for the modelling and estimation of the Sulphur Springs Mineral Resources are reported in
the Appendices of this Report.

10

Criteria JORC Code explanation Commentary
o hole length.

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.

Refer to previous statement.
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.

No Exploration Results are being reported as part of this MRE.

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.

No Exploration Results or aggregated intercepts are being reported.

The assumptions used for any reporting
of metal equivalent values should be
clearly stated.

A metal equivalent in the form of net smelter return (NSR) has been applied to Mineral Resources for reporting
purposes and is further detailed in Section 3 Estimation and Reporting of Mineral Resources.
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 (e.g.
‘down hole length, true width not
_known’). _

The geometry of mineralisation is well known and tested at this deposit by way of DD and RC drilling and detailed
prospect-scale mapping. Across the drill hole dataset, angles to mineralisation are considered to represent a drill
intercept perpendicular to lens strike orientation.
Diagrams
Appropriate maps and sections (with
scales) and tabulations of intercepts
should be included for any significant
discovery being reported These should

No significant discovery is being reported. Plan and long section maps, and sections relevant to the Mineral Resources
are included in the body of this Report.

11

Criteria JORC Code explanation Commentary
include, but not be limited to a plan
view of drill hole collar locations and
appropriate sectional views.
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.

No Exploration Results are being reported as part of this MRE.
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.

A substantive drilling campaign was completed during Q3 and Q4 2021 and was designed to infill and test Inferred
Mineral Resource material at depth and support conversion to Indicated status within an MRE update.

Geotechnical, metallurgical, bulk density, rock mass characterisation testwork was completed to feasibility study level
of detail in 2018 by Venturex Resources Ltd.

Entech does not consider there are any outstanding meaningful or material exploration data relevant or material to
this MRE.
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).

Entech understands DVP plans to drill test lens extensional opportunities both along strike and down dip.

Diagrams clearly highlighting the areas
of possible extensions, including the
main geological interpretations and
future drilling areas, provided this
information is not commercially
sensitive.

Refer to previous statement.

12

SECTION 3 ESTIMATION AND REPORTING OF MINERAL RESOURCES

(Criteria listed in section 1, and where relevant in section 2, also apply to this section.)

Criteria JORC Code explanation Commentary
Database integrity
Measures taken to ensure that data
has not been corrupted by, for
example, transcription or keying errors,
between its initial collection and its use
for Mineral Resource estimation
purposes.

The database has been audited by Entech for validation errors and physical comparison of drill hole core photography
against geological and assay data undertaken for 170 holes underpinning the Mineral Resource.

DVP’s database to April 2022 comprised 301 Collar records, 4,310 Survey records, 19,911 Assay records and 10,087
Lithology records.

Data from a total of 58,868 m of drilling from 149 DD and 85 RC drill holes were available for the MRE. Mineralisation
interpretations were informed by 104 DD holes intersecting the resource and 66 RC drill holes intersecting the
resource, for a total of 5954 m of drilling intersecting the resource.

Adjustments to the collar elevations of 36 drill holes for instances where GPS elevations did not correlate with
adjacent DGPS drill holes on the same drill pad.

Downhole survey azimuths for drill holes SSD001 to SSD088 were re-converted from local mine grid to MGA94_50
using a correction of +22°.

During the site visit in October 2021, the Competent Person conducted an additional check of the database against
known drill holes being drilled, logged and sampled. It was determined that the drill holes being processed at the time
(e.g. stage of drilling or assayed) matched the compiled dataset detailed above and that these data fairly represented
the most recent drilling information available at the project at the time of project cessation.

Data validation procedures used.

Entech completed various validation checks using built-in validation tools in GEOVIA Surpac™ and data queries in MS
Access such as overlapping samples, duplicate entries, missing data, sample length exceeding hole length, unusual
assay values and a review of below detection limit samples. A visual examination of the data was also completed to
check for erroneous downhole surveys.

The data validation process identified no major drill hole data issues that would materially affect the MRE outcomes.

Entech’s database checks included the following:
o
Checking for duplicate drill hole names and duplicate coordinates in the collar table.
o
Checking for missing drill holes in the collar, survey, assay and geology tables based on drill hole names.
o
Checking for survey inconsistencies including dips and azimuths <0°, dips >90°, azimuths >360° and negative
depth values.
o
Checking for inconsistencies in the ‘From’ and ‘To’ fields of the assay and geology tables. The inconsistency
checks included the identification of negative values, overlapping intervals, duplicate intervals, gaps and intervals
where the ‘From’ value is greater than the ‘To’ value.
Site visits
Comment on any site visits undertaken
by the Competent Person and the
outcome of those visits.

Entech undertook a site visit to the Sulphur Springs deposit on 21 October 2021 while an RC and DD drilling campaign
to support the 2022 MRE update was in progress. During the visit, Entech personnel inspected mineralised
intersections in drill core (SSD133, hangingwall chert, massive and disseminated sulphide mineralisation, footwall
dacite) and observed drilling, logging, sampling, QAQC and metadata collection operations.

If no site visits have been undertaken

Refer to previous statement.

13

Criteria JORC Code explanation Commentary
indicate why this is the case.
Geological
interpretation

Confidence in (or conversely, the
uncertainty of) the geological
interpretation of the mineral deposit.

Lithology and structure are considered the predominant controls on both the base metals (zinc, lead, copper),
precious metal (silver, gold) and gangue (iron) mineralisation at the Sulphur Springs deposit.

Entech relied on historical geological documentation, database-derived geological and assay data, outcrop geological
and structural mapping and site-based observations to evaluate geological, structural and mineralisation continuity.

Entech interpreted major lithological units to assist with the definition of deposit-scale geology and sulphide
mineralisation sequencing as follows:
o
Footwall dacite contact
o
Rhyodacite hangingwall
o
Footwall and hangingwall marker chert horizons
o
Hangingwall marker breccia (interpreted to be represent a thrust).

Sulphide and regolith weathering profiles were interpreted and modelled by Entech to assist with understanding
sulphide mineralisation relationships and recoveries.

The metallurgical weathering profile comprised four distinctive zones – leached, oxide, transitional and fresh – based
on field-based observations with re-logging by DVP personnel of available core photographs to identify area areas of
vugging and/or oxidation of sulphides, with sequential copper digestion used to further differentiate the boundary
between transitional and fresh. The weather zones are summarised as follows:
o
Leached zone: gossan, cavernous ground conditions; depleted in zinc, lead and copper.
o
Oxide zone: chalcocite and covellite represented >50% of copper species; well-developed vuggy sulphides;
gossanous and/or cavernous textures evident.
o
Transitional zone: chalcocite and covellite represented <50% of copper species; bornite/covellite may be present
along with chalcopyrite; tarnishing evident on other sulphides (e.g. pyrite); vugs related to secondary processes
were poorly to moderately well developed in sulphide (other than copper species).
o
Fresh zone: ‘fresh' chalcopyrite was the dominant copper sulphide species; no evidence or trace development of
vugs; any vug development was interpreted to have formed due to the dissolution of non-sulphide minerals
(e.g. carbonates), no tarnishing of other sulphide species (e.g. pyrite) or secondary copper species was evident.

Based on observations from downhole logging data, the regolith profile comprises three zones: oxide (BOPO),
transitional (BOCO) and fresh.

Mineralisation domains were interpreted primarily on geological logging and downhole geological contacts, based on
lithology, sulphide distribution, grade distribution, major faults and geometry. This combination provided a
mineralisation characterisation which effectively domained the mineralisation style and sub-domained the higher-
tenor zinc and copper mineralisation.

Confidence in the mineralisation continuity was based on geological, mineralogical and assay data that were cross-
referenced with available core photography and mapped outcrop geology and structural features.

The massive pyrite and base metal mineralisation occurs over a 550 m strike length and 600 m down dip extent, and
consists of an upper zone of massive sulphide overlying a disseminated/stringer zone. The upper contact of the
massive sulphide unit is generally sharp, while the lower contact with the underlying disseminated/stringer
mineralisation is diffuse/gradational.

14

Criteria JORC Code explanation Commentary

Sulphide mineralisation strikes east–west with an average dip of 50° to the north.

A north–south striking late-stage fault has split and offset sulphide mineralisation into two separate lenses.

Where logging information was inconclusive, iron and sulphide grades of less than 20% were used to define the
footwall contact of the massive sulphide.

The following base metal mineralisation types previously identified by DVP are recognised:
o
Zinc-rich mineralisation is most prominent towards the hangingwall of the massive sulphide. Discrete zones of
zinc occur towards the footwall of the massive sulphide and are interpreted to be structurally emplaced. Lower-
tenor zinc-rich mineralisation is also defined within the footwall disseminated/stringer horizon.
o
Copper-rich mineralisation occurs as a lobate, semi-continuous zone of mineralisation towards the footwall of the
massive sulphide and hangingwall of disseminated/stringer sulphide mineralisation.
o
Hangingwall zinc mineralisation that lies 10–40 m above the massive sulphide is interpreted to be structural
repletion of the massive sulphides. There is lower marker breccia below the hangingwall mineralisation that is
interpreted as localised thrust faulting. Within the hangingwall mineralisation horizon, there are two distinctive
high-grade shoots (40–60 m in strike width) with very high zinc tenor.

Data from a total of 58,868 m of drilling from 149 DD and 85 RC drill holes were available for the MRE. Mineralisation
interpretations were informed by 104 DD holes intersecting the resource and 66 RC drill holes intersecting the
resource, for a total of 5954 m of drilling intersecting the resource.

Interpretation of the two mineralisation types was initially undertaken using all available drill holes in Seequent
Leapfrog GEO™ software. Intercepts correlating to massive sulphide and copper-rich mineralisation and underpinned
by strike continuity implied from lithology wireframes were independently identified and manually selected in
Seequent Leapfrog GEO™prior to creating an implicit vein model.
Massive sulphide mineralisation

Entech considers confidence is moderate to high in the geological interpretation and continuity of mineralisation
domains within the massive sulphides.

Massive sulphide mineralisation intercepts were flagged by sharp a hangingwall contact with unmineralised country
rock, logged massive sulphide intervals and where logging information was inconclusive, iron and sulphide
grades >20% were used to define the footwall contact of the massive sulphide.

Within the massive sulphide lode domains, correlation and statistical analysis and visual review of the mineralisation
tenor, orientation and continuity underpinned base metal (zinc, lead, copper), precious metal (silver, gold) and gangue
(iron) sub-domain approaches.

Statistical distributions highlighted a bimodal distribution for copper and zinc in the massive sulphide lens.

Copper and zinc in these horizons have a distinctive geospatial relationship, with zinc primarily towards the
hangingwall and copper towards the footwall of the massive sulphide. Copper mineralisation occurs as a semi-
continuous lobate lens that straddles the footwall contact between the massive sulphide and underlying
disseminated/stringer zone, with most of the copper mineralisation falling in the massive sulphide horizon.

Based on these conclusions, indicator numerical modelling was used to capture spatially continuous sub-domains of
zinc (including lead) and copper. These sub-domains were exclusive of each other and used as hard boundaries in the
massive sulphidegeological envelopes,wherebyzinc and lead were composited and estimated within the zinc sub-

15

Criteria JORC Code explanation Commentary
domain, and copper was composited and estimated within the copper sub-domain.

Correlation analysis indicated gold, silver and iron were similarly distributed across massive sulphide domains and thus
were composited and estimated inside this boundary with no sub-domaining undertaken.

To maintain continuity, some material below 1% zinc and 1% copper has been included in the lodes.

Weathering and oxidation horizons have been modelled from downhole logged geology and assay data and have been
used for sub-domaining purposes.
Copper-rich mineralisation

Copper occurs as a lobate, semi-continuous zone of mineralisation towards the footwall of the massive and
hangingwall of disseminated sulphide mineralisation and straddles the boundary between the massive and lower
disseminated sulphides.

The copper mineralisation may contribute to the softer lower boundary definition of the massive sulphide.

Entech considers confidence is moderate to high in the geological interpretation and continuity of the copper
mineralisation. Entech considers that any alternate interpretations would be unlikely to result in significant differences
to lodes spatially and/or volumetrically.

Nature of the data used and of any
assumptions made.

Assumptions with respect to mineralisation continuity (plunge, strike and dip) within the underground Mineral
Resource were drawn directly from:
o
Drill hole lithological logging
o
Drill hole core photography (where available)
o
Mapped and interpreted north–south trending major fault
o
Mapped and interpreted outcrop geology (Archibald, 1993)
o
Variably spaced resource definition drilling, nominally 40 m × 40 m centres
o
Historical resource and open file documentation/records/files.

The effect, if any, of alternative
interpretations on Mineral Resource
estimation.

Entech is of the opinion that alternate interpretations and additional drill hole information would be unlikely to result
in significant spatial or volume variations. This conclusion was based on undertaking grade-based probabilistic volume
modelling (numerical modelling).

The use of geology in guiding and
controlling Mineral Resource
estimation.

The geological sequence, sulphide mineralisation styles and major structural faults defined the geospatial framework
for numerical modelling.

The factors affecting continuity both of
grade and geology.

The topography has restricted the location and position of drill holes; however, drill hole coverage for geological and
grade domain interpretations averages 40 m × 40 m over the sulphide mineralisation.
Dimensions
The extent and variability of the
Mineral Resource expressed as length
(along strike or otherwise), plan width,
and depth below surface to the upper
and lower limits of the Mineral
Resource.

The Sulphur Springs deposit comprises massive pyrite and base metal mineralisation is bound within a 550 m × 550 m
area and 600 m depth extent. Across-strike widths vary from 1 m to <40 m.

The MRE for zinc, lead, copper, silver and gold on which this Table 1 is based has the following extents:
o
Above 750 mRL
o
From 728400 mE to 729500 mE
o
From 7659400 mN to 7660200 mN.

16

Criteria JORC Code explanation Commentary
Estimation and
modelling techniques

The nature and appropriateness of the
estimation technique(s) applied and
key assumptions, including treatment
of extreme grade values, domaining,
interpolation parameters and
maximum distance of extrapolation
from data points. If a computer
assisted estimation method was chosen
include a description of computer
software and parameters used.

Domain intercepts were flagged and implicitly modelled in Seequent Leapfrog GEO™ software.

Interpretation was a collaborative process with DVP geologists to ensure Entech’s modelling represented observations
and understanding of geological and mineralisation controls.

Domain interpretations used all available RC and DD drill hole data. All interpreted intervals were snapped to sample
intervals prior to the construction of implicitly modelled 3D lode solids.

All drill hole samples and block model blocks were coded for lens and oxidation domain.

Compositing approaches were selected to honour the mineralisation style, geometry, expected grade variability and
potential mining selectivity.

Drilling samples were composited to 1 m lengths honouring lode domain boundaries using a best-fit approach
whereby any small uncomposited intervals (residuals) were divided evenly between the composites.

Composites were declustered and reviewed for statistical outliers and top-caps were applied by domain and variable.
Top-caps were applied where outliers were determined to be both statistical and spatial in nature.

Exploratory data analysis (EDA), variogram modelling and estimation validation was completed in GeoAccess,
Supervisor V8.8 and Isatis™.

Linear estimation techniques were considered suitable due to the style, and commodity, of deposit, available data
density and geological knowledge.

Variography analyses for zinc, copper, lead, gold, silver and iron were completed on declustered and capped
downhole composites grouped by mineralisation style (massive, disseminated, stringer). Robust variogram models
with a low to moderate nugget for zinc, copper and lead (8–10%), gold and silver (10–11%) and iron (15%) were
delineated and used in Kriging Neighbourhood Analysis (KNA) to determine parent cell estimation size and optimise
search neighbourhoods. Variogram and search parameters for zinc were applied to lead due to statistical and spatial
similarities. It should be noted that although the maximum continuity modelled in the variograms ranged from 70 m
to 80 m (zinc, lead, copper) and from 120 m to 202 m (silver, gold, iron), approximately 35–55% of spatial variability
and subsequent kriging weights were applied within 15–60 m.

Search neighbourhoods broadly reflected the direction of maximum continuity within the plane of mineralisation,
ranges, and anisotropy ratios from the variogram models. Neighbourhood parameters were optimised through KNA
and validation of interpolation outcomes.

All estimation was completed within respective mineralisation domains as outlined in previous sections:
o Silver ppm, gold ppm and iron per cent. Massive sulphide domain.
o Zinc per cent and lead per cent. Zinc sub-domain inside massive sulphide domain.
o Copper per cent. Copper sub-domain inside massive sulphide domain and also as footwall stringer domain.

Statistical analysis was undertaken to confirm correlated variables and tenor relationships with weathering (regolith
and metallurgical domains), mineralisation style and decisions pertaining to sub-domain delineation. As a result of this
analysis, no other hard boundaries were applied (i.e., weathering profile).

The maximum distance of extrapolation from data points was approximately half the drill hole data spacing. Using this
approach, the maximum distance of classified blocks estimated from known data points was ~40 m.

The availability of check estimates,
previous estimates and/or mine

A check estimate was undertaken for zinc and copper on a selection of domains using Inverse Distance Weighting
Squared (IDW2) with <2% grade variance for zinc and an average of 15% increase in copper for the IDW outcome.

17

Criteria JORC Code explanation Commentary
production records and whether the
Mineral Resource estimate takes
appropriate account of such data.

The last publicly reported MRE was the 2018 Sulphur Springs Resource1, prepared by Mil Min Pty Ltd under the
guidelines of the JORC Code, reported Indicated and Inferred Mineral Resources of 13.8 Mt at 3.8% zinc, 1.5% copper,
0.2% lead, 0.1 g/t gold and 18 g/t silver.

By comparison, approaches to domaining, classification, reasonable prospects for eventual economic extraction
(RPPEEE) (application of net smelter return (NSR) cut-off) undertaken by Entech and the inclusion of data from
additional RC and DD drill holes completed by DVP in 2021–2022 account for the variations to historical Mineral
Resources. Key differences in approach included:
o
Inclusion of 77 resource definition and infill drill holes providing increased volume delineation of discrete lenses
and zinc and copper sub-domains. This approach was implemented across all other lenses and varied from the
Mil Min Pty Ltd approach, which included internal waste in broader sulphide domains.
o
Change in Mineral Resource classification and reporting criteria from ‘0.4% Cu or Cu less than 0.4 with more than
2% Zn’, in 2018 MRE to the current (2022) NSR-based approach.

The project has not been mined historically or via artisanal methods and therefore no historical production records
exist for comparison purposes.

The assumptions made regarding
recovery of by-products.

No assumptions were made with respect to by-product recovery.

Estimation of deleterious elements or
other non-grade variables of economic
significance (e.g. sulfur for acid mine
drainage characterisation).

Entech understands that both iron and sulphur require monitoring for mine planning and metallurgical amenability
purposes.

Iron was composited, estimated and validated using the same domains as for silver and gold.

Sulphur was selectively assayed and there were insufficient data for sulphur to support estimation. A regression was
calculated for sulphur and applied in the final block model using estimated block grades for zinc, copper and iron as
input values.

No assumptions were made within the MRE with respect to other deleterious variables or by-products.

In the case of block model
interpolation, the block size in relation
to the average sample spacing and the
search employed.

Block sizes used were Y: 5 mN, X: 10 mE, Z: 5 mRL, with sub-celling of Y: 0.312 mN, X: 0.625 mE, Z: 0.312 mRL. The
parent block size was selected to provide suitable volume fill, given the available data spacing and mining selectivity.

The drill data spacing was 40 m × 40 m. Holes were drilled from pads on a fan basis to cover the sulphide
mineralisation at depth.

A two-pass estimation strategy was used, whereby search ranges reflected variogram maximum modelled continuity
and a minimum of 6, maximum of 16 composites for zinc, lead and copper, and a minimum of 6, maximum of 12 for
gold, silver and iron. The second search reduced the minimum composite required in the neighbourhood to 4; all
other parameters (e.g., range and maximum composites) remained the same. All blocks which did not meet the
criteria to trigger an estimate were not estimated and were excluded from Mineral Resource classification.

Any assumptions behind modelling of
selective mining units.

No selective mining units were assumed for this MRE.

Any assumptions about correlation

Correlation analyses were completed for all variables within sulphide domains(Domains 1 to 4),which contributed to

1 MM_505_Sulphur_Springs_Resource_Report_March_2018

18

Criteria JORC Code explanation Commentary
between variables. the grouping of elements for compositing and estimation within domains and sub-domains.

Correlation trends are consistent across massive and disseminated/stringer sulphide mineralisation

Grouping of elements for compositing and estimation was based on the following positive correlations:
o
Zinc + lead (and associated high tenor sub-domain)
o
Copper and copper sub-domain
o
Gold, silver and iron are moderately correlated
o
Iron and sulphur are strongly correlated with greater than 90% correlation
o
Iron, sulphur and density are strongly correlated with greater than 85% correlation.

Description of how the geological
interpretation was used to control the
resource estimates.

Four sulphide domains were defined as follows:
o
Domain 1: Massive sulphide mineralisation with a sharp hangingwall contact. The footwall contact was defined
either by drill hole logging or by iron and sulphur grades greater than 20%.
o
Domain 2: Disseminated/stringer mineralisation underlying the massive sulphide.
o
Domain 3: Hangingwall massive sulphide mineralisation with two discrete shoots 40–60 m in width of high-tenor
zinc mineralisation.
o
Domain 4: Footwall massive sulphide mineralisation.

All estimation was completed within either a geologically defined massive sulphide domain (silver, gold, iron) or within
higher-tenor zinc or copper sub-domains inside the massive domains. Hard boundaries for estimation were:
o
Silver ppm, gold ppm and iron per cent: Massive sulphide domain
o
Zinc per cent and lead per cent: Zinc sub-domain inside massive sulphide domain
o
Copper per cent: Copper sub-domain, a semi-continuous lobate lens that straddles the footwall contact between
the massive sulphide (Domain 1) and underlying disseminated/stringer zone (Domain 2) with most of the copper
mineralisation falling within the massive sulphide horizon.

Each sub-domain used for estimation hard boundaries was delineated with probability-based numerical modelling and
reflected findings of geospatial, statistical and correlation analysis.

Interpretation of lens strike extents included modelling of a key north–south post-mineralisation fault (Main fault)
that offsets the sulphide mineralisation between 10 m and 35m.

Metallurgical domaining: Metallurgical weathering horizons were defined by re-logging of sulphide oxidation state
from core photography of 65 DD holes and interpreted to comprise three horizons: oxide, transitional and fresh. DVP
personnel outlined the following criteria for classification of the metallurgical weathering zones:
o
Oxide is defined when chalcocite and covellite represented >50% of copper species. Well-developed vuggy
sulphides. Gossanous and/or cavernous textures were evident.
o
Transitional is defined when chalcocite and covellite represented <50% of copper species. Bornite/covellite may
be present along with chalcopyrite. Tarnishing was evident on other sulphides (e.g., pyrite). Vugs related to
secondary processes were poorly to moderately well developed in sulphide (other than copper species).
o
Fresh is defined when fresh chalcopyrite was the dominant copper sulphide species. No evidence or trace
development of vugs. Any vug development was interpreted to have formed due to the dissolution of non-
sulphide minerals(e.g.,carbonates). No tarnishingof other sulphide species(e.g., pyrite)or secondarycopper

19

Criteria JORC Code explanation Commentary
species was evident.

These metallurgical horizons were used in an NSR calculation to reflect recoverable metal in each metallurgical
weathering horizon.

Discussion of basis for using or not
using grade cutting or capping.

Assessment and application of top-capping was undertaken on the zinc, lead, copper, gold, silver and iron variables by
mineralisation style (massive or disseminated). Domains were capped to address instances where outliers were
defined as both statistical and spatial in nature, presented below:
o
Massive: zinc 30%, lead 3%, copper (no cap), silver 300 g/t, gold 1.5 g/t.
o
Disseminated: zinc 10%, lead 2%, copper 10%, silver 50 g/t, gold 0.5 g/t.
o
Metal reductions from the above caps were minor in nature averaging <3% across all variables in the massive and
disseminated domains. Capping of the silver variable in the disseminated domain resulted in an 8.5% metal
reduction.
o
Iron was not capped.

The process of validation, the checking
process used, the comparison of model
data to drill hole data, and use of
reconciliation data if available.

Global and local validation of the zinc, lead, copper, gold, silver and iron estimated outcomes was undertaken with
statistical analysis, swath plots and visual comparison (cross and long sections) against input data.

Global comparison of declustered and capped composite mean against estimated mean (by domain and variable)
highlighted less than 10% variation for zinc and silver and within 5% variation for copper.
Moisture
Whether the tonnages are estimated
on a dry basis or with natural moisture,
and the method of determination of
the moisture content.

The tonnages were estimated on a dry basis.
Cut-off parameters
The basis of the adopted cut-off
grade(s) or quality parameters applied.

The NSR cut-off grade used for reporting of Mineral Resources at Sulphur Springs was A$80/t, which is approximately
80% of the break-even stoping cut-off value underpinning DVP’s current Life of Mine Plan (LOMP). The NSR cut-off
reflects costs associated with metal recovery and was selected based on discussions with DVP engineers, and
benchmarked against previous detailed studies at the project.

The NSR cut-off considers revenue from saleable base metals – zinc, copper (per cent) – and silver (ppm) and offsets
site operating and sustaining capital costs, including underground operating development. The base metal and
precious metals used in the NSR calculation all have reasonable potential of being saleable.

The NSR calculation determines a value for the saleable metals by applying the following modifying factors, presented
in Table 1:
o
Metal prices
o Metallurgical recoveries (by metallurgical weathering profile)
o
Payability factors, inclusive of concentrate treatment charges, metal refining charges, payment terms
(concentrate), logistics costs and NSR royalties.

Silver metal price is A$25.54/oz.

Silver recovery average of 18% for zinc concentrate and includes deportment from cost model.

Silver recovery average of 28% for copper concentrate and includes deportment from cost model.

20

Criteria JORC Code explanation Commentary
Table 1: Key NSR assumptions

For the purposes of NSR determination, NSR values were calculated, by metallurgical domain, on a block-by-block
basis prior to implementing reporting cut-offs.

It is the Competent Person’s opinion that these methods and cut-off grades satisfy the requirements to test, assess
and define the Sulphur Springs Mineral Resources within the context of RPEEE.
Mining factors or
assumptions

Assumptions made regarding possible
mining methods, minimum mining
dimensions and internal (or, if
applicable, external) mining dilution. It
is always necessary as part of the
process of determining reasonable
prospects for eventual economic
extraction to consider potential mining
methods, but the assumptions made
regarding mining methods and
parameters when estimating Mineral
Resources may not always be rigorous.
Where this is the case, this should be
reported with an explanation of the
basis of the mining assumptions made.

Outcomes from the 2018 DFS study demonstrated recoverable material both open pit and underground development.

The MRE extends nominally 400 m below the topographic surface. Entech considers material at this depth, and at the
grades estimated, would fall under the definition of RPEEE in an underground mining framework.

Entech considers the NSR cut-offs used for MRE reporting reflect costs associated with metal recovery from remnant
mining areas and would fall within the definition of RPEEE in an underground framework.

No mining dilution or cost factors were applied to the MRE.
Metallurgical factors or
assumptions

The basis for assumptions or
predictions regarding metallurgical
amenability. It is always necessary as
part of the process of determining
reasonable prospects for eventual
economic extraction to consider
potential metallurgical methods, but
the assumptions regarding
metallurgical treatment processes and
parameters made when reporting
Mineral Resources may not always be

Metallurgical recovery factors have been applied within the NSR based on inputs supplied by DVP and a review of
previous feasibility-level studies2(2018).

Entech understands from the 2018 feasibility report that metallurgical viability and recovery factors for oxide
(supergene), transitional and fresh were addressed by a number of testwork programs based on historical
metallurgical testwork for fresh material and during the 2018 DFS, with holes SSD089 to SSD102 sampled for testing of
oxide and transitional material.

Previous work focused on the fresh ore, resulting in a recommendation to use selective sequential flotation to
produce separate copper- and zinc-rich concentrates with high mineral recoveries at target grades.

Estimated metallurgical recoveries for copper and zinc have been determined for oxide, transitional and fresh material
based on metallurgical testwork.

2 Venturex Resources Ltd, ASX release dated 10 October 2018: Sulphur Springs Feasibility Study confirms long-life, high-margin Australian copper-zinc mine with outstanding economics

21

Criteria JORC Code explanation Commentary
rigorous. Where this is the case, this
should be reported with an explanation
of the basis of the metallurgical
assumptions made.

A global silver recovery, including deportment from cost model of 18% and 28% for zinc and copper concentrates,
respectively.

Total recoveries calculated in the NSR, inclusive of all concentrate products for each material type, were based on the
following recovery algorithms for copper and zinc:

Entech understands from discussions (with DVP personnel), documentation reviews (supplied by DVP) and project site
inspections that no other deleterious variables, which would materially affect eventual economic extraction of Mineral
Resources, have been identified at the project.

No factors or assumptions were made within the MRE with respect to other deleterious variables or by-products.
Environmental factors
or assumptions

Assumptions made regarding possible
waste and process residue disposal
options. It is always necessary as part
of the process of determining
reasonable prospects for eventual
economic extraction to consider the
potential environmental impacts of the
mining and processing operation. While
at this stage the determination of
potential environmental impacts,
particularly for a greenfields project,
may not always be well advanced, the
status of early consideration of these
potential environmental impacts should
be reported. Where these aspects have
not been considered this should be
reported with an explanation of the
environmental assumptions made.

No environmental factors were applied to the Mineral Resources or resource tabulations.
Bulk density
Whether assumed or determined. If
assumed, the basis for the
assumptions. If determined, the
method used, whether wet or dry, the
frequency of the measurements, the
nature, size and representativeness of
the samples.

This MRE contains dry bulk density data which was collected on drill core from 212 holes (between 1990 and 2022).

The density samples were located between 7659400 mN and 7660200 mN, 728400 mE and 729500 mE and nominally
from the surface to a depth of 550 m, providing a representative density profile between mineralised domains,
sulphide and regolith weathering profiles and depth profile within the MRE.

22

Criteria JORC Code explanation Commentary

The bulk density for bulk material must
have been measured by methods that
adequately account for void spaces
(vugs, porosity, etc), moisture and
differences between rock and
alteration zones within the deposit.

Density measurements were collected and measured using an industry-accepted water immersion density
determination method for each sample.

It should be noted that cavities and core loss experienced in the ‘leached zone’, a depleted and weathered sub-surface
zone, were taken into account during compilation of the MRE. Minor cavities (documented as core loss) from
millimetres to 1 m were modelled as voids for stamping into the block model. Additionally, density was reduced within
this weathered zone by 20% to account for the known vuggy nature of leached material. It should be noted Entech
considers this a conservative approach to assist in future mine planning and no mineralised or resource material is
located within this weathered horizon.

Discuss assumptions for bulk density
estimates used in the evaluation
process of the different materials.

Entech applied a multivariate regression equation (zinc %, lead %, copper % and iron %), by metallurgical weathering
profile, to the block model and derived density values on a block-by-block basis.

Within the mineralised domains, 3,090 of 5,855 samples have a measured density value. Of these samples, 2,975
samples have complete analyses for zinc %, lead %, copper % and iron %.

The metallurgical weathering profile comprises four key horizons – leached, oxide, transitional and fresh. Multi-
element regression indicated varying regression co-efficients occur across the weathering horizons. Therefore, a
separate regression formula was used for oxide, transitional and fresh material.

The leached zone is depleted of mineralisation and therefore did not comprise Mineral Resources. A background
density was applied in this horizon with adjustments and depletions applied to represent the vuggy nature of this zone
(as previously discussed).

Within the fresh weathering horizon, evaluation of the copper high-tenor sub-domain mineralisation was undertaken
with no definitive variation in regression outcomes from zinc-dominant sub-domains. Thus, one regression formula for
fresh material was applied across all mineralisation domains.

Validation of the regression concluded a correlation co-efficient of 0.93 between measured and regression density.
Ideally sulphur would be included in this regression given the close correlation with iron. However insufficient
sampling of this element limited the ability to use all measured densities and derive a robust a regression formula, so
in this instance sulphur was not used within density regressions.

Calculated density regression was applied on a block-by-block basis on estimated grade values:
o
Oxide: Density=1.976418+Zn Pct0.02795+Pb Pct-0.092028+Cu Pct-0.003506+Fe Pct0.051415
o
Transitional: Density=2.472249+Zn Pct0.022663+Pb Pct0.023376+Cu Pct0.000101+Fe Pct0.043261
o
Fresh: Density=2.526907+Zn Pct0.020732+Pb Pct0.052578+Cu Pct-0.005445+Fe Pct0.043606.

23

Criteria JORC Code explanation Commentary
Classification
The basis for the classification of the
Mineral Resources into varying
confidence categories.

The underground zinc-copper deposit contains Indicated and Inferred Mineral Resources.

Mineral Resources were classified based on geological and grade continuity confidence drawn directly from:
o
Drill hole methodology, data quality, spacing and orientation
o
Geological domaining
o
Estimation quality parameters

IndicatedMineral Resources were defined where a moderate level of geological confidence in geometry, continuity,
and grade was demonstrated, and were identified as areas where:
o
Blocks were well supported by drill hole data, with drilling averaging a nominal 40 m × 40 m or less between drill
holes
o
Blocks were interpolated with a neighbourhood informed by a minimum 12–16 composites
o
Estimation quality, slope of regression above 0.5.

InferredMineral Resources were defined where a lower level of geological confidence in geometry, continuity and
grade was demonstrated, and were identified as areas where:
o
Drill spacing was averaging a nominal 60 m or less, or where drilling was within 70 m of the block estimate
o
Blocks were interpolated with a neighbourhood informed by a minimum of 10 composite
o
Estimation quality, slope of regression above 0.2.

Mineralisation within the model which did not satisfy the criteria for classification as Mineral Resources remained
unclassified.

Whether appropriate account has been
taken of all relevant factors (ie relative
confidence in tonnage/grade
estimations, reliability of input data,
confidence in continuity of geology and
metal values, quality, quantity and
distribution of the data).

Consideration has been given to all factors material to Mineral Resource outcomes, including but not limited to
confidence in volume and grade delineation, continuity and preferential orientation mineralisation; quality of data
underpinning Mineral Resources, nominal drill hole spacing and estimation quality (conditional bias slope, number of
samples, distance to informing samples).

Whether the result appropriately
reflects the Competent Person’s view of
the deposit.

The delineation of Indicated and Inferred Mineral Resources appropriately reflects the Competent Person’s view on
continuity and risk at the deposit.
Audits or reviews
The results of any audits or reviews of
Mineral Resource estimates.

Internal audits and peer review were undertaken by Entech with a focus on independent resource tabulation, block
model validation, verification of technical inputs, and approaches to domaining, interpolation and classification.
Discussion of relative
accuracy/confidence

Where appropriate a statement of the
relative accuracy and confidence level
in the Mineral Resource estimate using
an approach or procedure deemed
appropriate by the Competent Person.
For example, the application of
statistical orgeostatisticalprocedures

Local variances to the tonnage, grade and metal distribution are expected with further definition drilling. It is the
opinion of the Competent Person that these variances will not significantly affect the economic extraction of the
deposit and the application of the Indicated and Inferred classification extents appropriately convey this risk.

The MRE is considered fit for the purpose of feasibility level studies, life of mine planning and economic evaluation.

24

Criteria JORC Code explanation Commentary
to quantify the relative accuracy of the
resource within stated confidence
limits, or, if such an approach is not
deemed appropriate, a qualitative
discussion of the factors that could
affect the relative accuracy and
confidence of the estimate.

The statement should specify whether
it relates to global or local estimates,
and, if local, state the relevant
tonnages, which should be relevant to
technical and economic evaluation.
Documentation should include
assumptions made and the procedures
used.

The Mineral Resource Statement relates to global tonnage and grade estimates.

No formal confidence intervals nor recoverable resources were undertaken or derived.

These statements of relative accuracy
and confidence of the estimate should
be compared with production data,
where available.

The project has not undergone historical, recent or artisanal mining and therefore no historical production records are
available for comparison.

25

==> picture [494 x 722] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
SSD001 728813.741 7659666.372 1345.032 114.7 167.4 -50 75.65 114.7 Massive
75.65 114.7 Massive
SSD001A 728813.741 7659666.372 1345.032 154 167.4 -50
114.7 114.707 Disseminated/ Stringer
78 113.5 Massive
SSD002 728813.137 7659668.671 1344.932 197 0 -90
113.5 148 Disseminated/ Stringer
168.5 172.96 Massive
SSD003 728857.776 7659920.928 1245.9 266 192.4 -50 215.8 216.7 Massive
216.7 221 Disseminated/ Stringer
81.45 94.6 Massive
SSD004A 729021.635 7659688.785 1255.34 181 212.4 -60
94.6 116.8 Disseminated/ Stringer
96 100.23 Massive
SSD005 728955.175 7659807.528 1250.33 208 202.4 -50 130.3 150 Massive
150 161 Disseminated/ Stringer
196 199 Massive
SSD006 728858.046 7659922.488 1246.31 295.3 192.4 -75 227.1 231.1 Massive
231.1 266 Disseminated/ Stringer
140.63 148.7 Massive
SSD007 728955.145 7659807.791 1249.83 289 0 -90 201.1 254.8 Massive
254.8 271.6 Disseminated/ Stringer
SSD008 728777.529 7659874.721 1254.738 280.5 205.4 -50 153.7 156.4 Disseminated/ Stringer
SSD009B 729034.374 7659712.478 1254.8 153.3 0 -90 61.5 63.8 Massive
31.5 49.2 Massive
SSD010 729061.074 7659666.757 1258.75 124.2 207 -60
49.2 66 Disseminated/ Stringer
250.75 252.25 Massive
316.6 317.6 Massive
SSD012 728860.096 7659919.868 1246.32 378 111.4 -73.5
317.6 318.65 Disseminated/ Stringer
326.6 327.13 Disseminated/ Stringer
255.5 262 Massive
SSD013 728862.596 7659920.978 1246.32 505 106 -60 334.5 344 Massive
344 355 Disseminated/ Stringer
251 273 Massive
SSD014 729183.231 7660025.171 1280.89 354 196.4 -50 273 277 Disseminated/ Stringer
277 285 Massive
318.8 327.8 Massive
SSD015 729183.396 7660027.627 1281.48 390 194.4 -80
327.8 360.9 Disseminated/ Stringer
288.3 319.35 Massive
SSD016 729253.256 7659982.117 1289.96 375.3 194.4 -65
319.35 323.2 Disseminated/ Stringer
356.2 379.25 Massive
SSD017 729253.506 7659983.147 1289.97 422 182 -80
379.25 385.8 Disseminated/ Stringer
257 267.2 Massive
SSD018 729252.686 7659980.177 1290.06 349 194 -50 267.2 268.2 Disseminated/ Stringer
281 290.7 Massive
343.7 355.9 Massive
SSD019 729133.636 7660033.987 1298.26 396.3 200 -80
355.9 361.077 Disseminated/ Stringer
267.3 276.15 Massive
SSD020 729389.726 7659904.048 1320.76 346.9 219 -50
276.15 277.15 Disseminated/ Stringer
353.8 358.15 Massive
SSD022 729133.266 7660032.207 1298.42 397.5 205 -67
358.15 368.45 Disseminated/ Stringer
481.9 487.1 Massive
SSD027 729239.776 7660277.386 1244.68 530 194 -75
487.1 489.5 Disseminated/ Stringer
202 232.15 Massive
SSD030 729229.846 7659866.688 1349.39 285.6 194 -63 232.15 236.1 Disseminated/ Stringer
256.24 260.05 Massive
198.17 215.5 Massive
SSD031 729323.445 7659819.103 1342.53 271.4 219 -61
215.5 216.5 Disseminated/ Stringer
111 141 Massive
SSD034 729149.106 7659816.378 1306.96 270.5 206 -62
141 159 Disseminated/ Stringer
149.2 183.35 Massive
SSD035 729149.576 7659817.318 1306.93 276.5 206 -88
183.35 189.5 Disseminated/ Stringer
215.3 218 Massive
SSD036 729078.766 7659880.828 1327.2 318.5 206 -62 244.8 260 Massive
260 270.5 Disseminated/ Stringer
259.5 261 Massive
SSD038 729078.496 7659877.118 1327.22 358.5 214 -80 302.9 324.2 Massive
324.2 326 Disseminated/ Stringer
186 196 Massive
SSD039 728777.494 7659878.158 1254.588 327 203 -75
196 208 Disseminated/ Stringer
239 254.4 Massive
SSD041 728775.684 7659882.153 1254.607 339.5 0 -90
254.4 256 Disseminated/ Stringer
SSD043 728743.165 7660126.947 1241.347 505.8 206 -60 343.5 348.3 Disseminated/ Stringer
SSD045 728677.778 7659905.305 1266.459 364.65 0 -90
279.5 288.5 Disseminated/ Stringer
SSD046 728677.138 7659903.669 1266.566 301.7 206 -58 184 189 Disseminated/ Stringer
276.9 298 Massive
SSD048 729180.28 7660021.442 1281.11 453.4 194 -64
298 322.5 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 1 of 6

==> picture [494 x 712] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
116 117.1 Massive
SSD052 728921.686 7659850.948 1248.53 203.55 200.79 -54 139.3 166.8 Massive
166.8 188 Disseminated/ Stringer
155 157 Massive
220 250 Massive
SSD053 728922.076 7659852.048 1248.49 297.55 198.94 -85
250 257.4 Disseminated/ Stringer
257.4 261.35 Disseminated/ Stringer
114 116 Massive
SSD054 728957.585 7659806.838 1249.96 219.5 202.4 -75 144.45 180.55 Massive
180.55 201 Disseminated/ Stringer
SSD055 729160.254 7659761.232 1309.33 204.45 292 -82 112.65 166.1 Massive
166.1 173.45 Disseminated/ Stringer
SSD056 728987.075 7659771.578 1252.32 94 202 -60 68 70 Massive
71 73 Massive
SSD057 728986.735 7659770.798 1252.28 168.65 202 -55 103.9 135 Massive
135 141.05 Disseminated/ Stringer
101.5 112.5 Massive
SSD058 729147.842 7659797.688 1306.51 160 193.4 -55
112.5 122.8 Disseminated/ Stringer
90 93 Massive
SSD059 728987.445 7659772.428 1251.86 204.4 202.4 -75 122.55 153.4 Massive
153.4 171.65 Disseminated/ Stringer
197.65 208.2 Massive
SSD060 729231.819 7659859.92 1349.24 249.5 206.9 -50
208.2 216.3 Disseminated/ Stringer
147.6 179 Massive
SSD061 729143.632 7659824.719 1306.59 206.5 219.4 -80
179 185 Disseminated/ Stringer
240.5 265 Massive
SSD062 729283.605 7659888.218 1342.96 306.35 204.63 -65 265 267.6 Disseminated/ Stringer
290.4 294.5 Massive
226.05 249.45 Massive
SSD063 729232.924 7659859.782 1349.23 279.95 235.73 -70
249.45 257.45 Disseminated/ Stringer
158.95 180 Massive
SSD064 728871.574 7659714.757 1328.6 227.9 0 -90
180 200.7 Disseminated/ Stringer
208.2 247.8 Massive
SSD065 729283.378 7659887.737 1342.93 277.2 205.86 -50.5 247.8 252.4 Disseminated/ Stringer
275.45 277.2 Massive
197.3 199.15 Massive
SSD066A 729080.028 7659876.914 1326.96 312.5 173.4 -60
199.15 210 Disseminated/ Stringer
123.35 159.2 Massive
SSD067 728871.767 7659714.108 1328.58 213.15 151.4 -64
159.2 173.05 Disseminated/ Stringer
183.2 222.9 Massive
SSD068 729235.106 7659860.822 1349.28 255.6 190.4 -50
222.9 224.2 Disseminated/ Stringer
SSD069 729023.944 7659705.288 1254.75 135.5 117 -60 51.9 54.1 Massive
166.85 196.3 Massive
SSD070A 729137.056 7659828.018 1307.26 221.35 0 -90 196.3 208.15 Disseminated/ Stringer
208.15 220.3 Massive
117 119 Massive
SSD071 728987.475 7659780.778 1250.85 225.5 0 -90 159.3 192.15 Massive
192.15 213.9 Disseminated/ Stringer
65.9 67.1 Massive
SSD072 729011.168 7659733.513 1253.21 159.5 202 -80 103 132.4 Massive
132.4 142.3 Disseminated/ Stringer
126 127.85 Massive
SSD073 728921.176 7659851.978 1248.57 219.5 202 -68 141.95 183.5 Massive
183.5 195.5 Disseminated/ Stringer
104.15 105.5 Massive
SSD074 729235.297 7659697.031 1294.21 174.5 0 -90
105.5 106.45 Disseminated/ Stringer
226.2 247.8 Massive
SSD076 729226.875 7659865.086 1349.06 291.5 209 -72 247.8 249 Disseminated/ Stringer
256.4 267.5 Massive
121.3 154.75 Massive
SSD077 729138.595 7659824.147 1306.85 180.3 202 -72
154.75 167 Disseminated/ Stringer
203.3 226.33 Massive
SSD078 729230.348 7659861.691 1349.23 270.5 209 -62 226.33 246.35 Disseminated/ Stringer
246.35 249.2 Massive
78 81 Massive
SSD079 728984.575 7659773.678 1252.17 173.4 202 -23 119.7 156.7 Massive
156.7 165.1 Disseminated/ Stringer
73.75 78.4 Massive
SSD080 728984.575 7659773.978 1252.04 170.2 202 -37 113.5 154 Massive
154 164.05 Disseminated/ Stringer
89.6 91.6 Massive
SSD081 728953.896 7659804.187 1250.49 181 202 -38 136 161.9 Massive
161.9 172 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 2 of 6

==> picture [494 x 722] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
98 106 Massive
SSD082 728873.807 7659713.363 1328.42 179.6 202.4 -75 128.35 153.3 Massive
153.3 160 Disseminated/ Stringer
272.3 275.8 Massive
SSD084 729178.618 7660018.512 1281.32 306.5 207 -45
275.8 285.8 Disseminated/ Stringer
25.75 43.6 Massive
43.6 50.6 Massive
SSD085 729189.854 7659700.681 1285.44 127.1 183 -85
50.6 51.6 Disseminated/ Stringer
83.7 85.7 Massive
99.6 121 Massive
SSD086 729202.276 7659766.178 1307.73 161.4 208 -65
121 122.5 Disseminated/ Stringer
117.8 141.45 Massive
SSD087A 729202.227 7659766.33 1307.93 188.5 213 -80 141.45 143.2 Disseminated/ Stringer
168.15 169.3 Massive
69 77.6 Massive
SSD089 728840 7659663 1344 153.7 0 -90 97.8 141 Massive
141 153.7 Disseminated/ Stringer
88.85 128 Massive
SSD090 728840 7659663 1344 134.7 180 -81
128 132 Disseminated/ Stringer
85 118 Massive
SSD091 728820 7659663 1344 141.7 180 -78
118 130 Disseminated/ Stringer
72 76 Massive
SSD092 728820 7659665 1344 159.6 0 -84 78 141.4 Massive
141.4 155 Disseminated/ Stringer
70 120.15 Massive
SSD093 728800 7659670 1344 133.3 0 -90
120.15 128.2 Disseminated/ Stringer
83 103 Massive
SSD094 728800 7659670 1344 174.4 0 -90 114.5 141.2 Massive
141.2 168.4 Disseminated/ Stringer
89 122.9 Massive
SSD095 728780 7659660 1341.971 138.6 0 -90
122.9 130 Disseminated/ Stringer
82 131.8 Massive
SSD096 728780 7659660 1341.971 174.5 0 -70
131.8 164 Disseminated/ Stringer
99 114.1 Massive
134.2 144.5 Massive
SSD097 728780 7659660 1341.971 200.2 14 -64
144.5 150.9 Massive
150.9 200.2 Disseminated/ Stringer
79 95.8 Massive
SSD098 728780 7659660 1341.971 192.3 37 -68 103.5 157.3 Massive
157.3 172 Disseminated/ Stringer
169.1 223.9 Massive
SSD099 728869 7659709 1328.404 249.4 0 -80
223.9 242 Disseminated/ Stringer
89 91 Massive
SSD100 728869 7659709 1328.404 151.7 190 -60 118 139.9 Massive
139.9 149 Disseminated/ Stringer
102 108 Massive
SSD101 728875 7659708 1328 154.5 180 -65 125 143 Massive
143 152.5 Disseminated/ Stringer
117 118 Massive
SSD102 728872.8 7659706.5 1328.479 201.3 285 -77 138 192.5 Massive
192.5 198.25 Disseminated/ Stringer
43.7 75.2 Massive
SSD105 728790 7659650 1341.221 145 210 -70
75.2 85 Disseminated/ Stringer
35 53 Massive
SSD107 729048.37 7659679.14 1256.36 83.4 173 -62
53 69.15 Disseminated/ Stringer
50 59 Massive
SSD109 729044.959 7659678.616 1256.558 122 188 -35
59 94 Disseminated/ Stringer
67 79.8 Massive
SSD110 729039.979 7659678.216 1256.5 121.8 216 -29
79.8 93 Disseminated/ Stringer
44 48 Massive
SSD112 729002.9 7659714.5 1254.5 155.4 189 -67 84.05 111.45 Massive
111.45 125.5 Disseminated/ Stringer
36 38 Massive
SSD113 729005.008 7659714.276 1254.56 179.4 212 -54 77 98.85 Massive
98.85 108 Disseminated/ Stringer
SSD117 729028.26 7659678.121 1257.885 72 236 -15 71 72 Massive
SSD118 729012.495 7659723.079 1253.968 48 210 -35 44 48 Massive
44 48 Massive
SSD121 729004.528 7659725.415 1254.041 173.4 210 -35 83.34 112 Massive
112 133 Disseminated/ Stringer
139.2 166 Massive
SSD122 728852.7 7659909.5 1247.5 240 189 -35 182.24 201.9 Massive
201.9 217.9 Disseminated/ Stringer
195.1 221.5 Massive
SSD126 729322.358 7659821.149 1342.861 226.6 226 -48
221.5 222.6 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 3 of 6

==> picture [494 x 722] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
160.7 162 Massive
SSD128 729133.779 7659823.335 1306.74 237.8 225 -56
162 163 Disseminated/ Stringer
135.5 192 Massive
SSD130 728838.642 7659665.155 1344.531 220 73 -70
192 220 Disseminated/ Stringer
95 103.7 Massive
SSD131 728818.016 7659664.818 1344.648 239.9 25 -76 143.2 196.6 Massive
196.6 202.1 Disseminated/ Stringer
208 212 Massive
SSD132 728785 7659880 1253.57 321.2 95 -88 233 278.65 Massive
278.65 300 Disseminated/ Stringer
235 244 Massive
SSD133 728883.322 7659931.804 1248.81 351 196 -81
314.2 325 Disseminated/ Stringer
211 226 Massive
SSD134 728885.695 7659933.024 1248.824 318 208.49 -76 245 248 Massive
248 272 Disseminated/ Stringer
188 192 Massive
SSD136 728884.816 7659925.68 1249.04 306.1 166 -71
236 265 Massive
265 283 Disseminated/ Stringer
192 199 Massive
SSD137 728886.565 7659925.3 1249.223 324.1 150.49 -70 244 267 Massive
267 269 Disseminated/ Stringer
219 222 Massive
SSD138 728888.118 7659924.338 1249.162 342.3 147 -76 308 310 Massive
310 313 Disseminated/ Stringer
212 216 Massive
SSD139 728889.002 7659925.689 1249.222 333.2 141.75 -72
299.8 302.85 Massive
302.85 307 Disseminated/ Stringer
256 260 Massive
SSD140 728891.884 7659928.824 1249.279 354.2 126 -77 321 322.145 Massive
322.145 336.65 Disseminated/ Stringer
382 403 Massive
SSD142 729294.53 7660050.6 1261 420 177.43 -74
403 420 Disseminated/ Stringer
341 371 Massive
SSD143 729287.5 7660047.38 1261 457 187.67 -70
371 384 Disseminated/ Stringer
236 256 Massive
SSD144 728843.683 7659916.197 1247.094 402 231.59 -86 300 304 Massive
304 308 Disseminated/ Stringer
323 360 Massive
SSD145 729286.85 7660046.9 1261 384 195.25 -66
360 372 Disseminated/ Stringer
313 322 Massive
SSD146 729168 7660030 1282.823 372 205 -68
322 330 Disseminated/ Stringer
327 357 Massive
SSD147 729287 7660049 1262 358 197.84 -74
357 358 Disseminated/ Stringer
347 361 Massive
SSD148 729168 7660031 1282.766 366 199.18 -80
361 366 Disseminated/ Stringer
276 280 Massive
SSD149 729069.317 7659871.06 1327.162 366 234.94 -73
301 344 Massive
344 356 Disseminated/ Stringer
375 409 Massive
SSD150 729174.816 7660025.415 1281.247 438 154 -85
409 415 Disseminated/ Stringer
288 314 Massive
SSD152 729173.996 7660023.42 1281.281 366 171.17 -73
314 338 Disseminated/ Stringer
339 366 Massive
SSD154 729173.44 7660026.486 1281.222 396 170.57 -79
366 372 Disseminated/ Stringer
243 250 Massive
SSD155 729073.469 7659866.959 1327.33 337 215 -73 290 309 Massive
309 321 Disseminated/ Stringer
284 314 Massive
SSD156 729174.596 7660023.854 1281.311 360 167.05 -61
314 335 Disseminated/ Stringer
236 240 Massive
SSD157 729076 7659871 1327.36 318 209.81 -70 251 276 Massive
276 288 Disseminated/ Stringer
271 294 Massive
SSD158 729172.788 7660024.15 1281.33 316 179 -60
294 305 Disseminated/ Stringer
260 264 Massive
SSD159 729075.3 7659867.3 1327 354 225.39 -77 336 353 Massive
353 354 Disseminated/ Stringer
351 387 Massive
SSD160 729172.582 7660024.86 1281.344 399 177.03 -82
387 393 Disseminated/ Stringer
252 256 Massive
SSD161 729070 7659872 1327.109 360 221.56 -72 317 323 Massive
323 328 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 4 of 6

==> picture [494 x 713] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
292 308 Massive
SSD162 729171.66 7660024.374 1281.461 366 189.49 -66
308 332 Disseminated/ Stringer
224 277 Massive
SSD163 729083.088 7659871.502 1326.804 312 117.52 -81
277 290 Disseminated/ Stringer
300 317 Massive
SSD164 729170.75 7660024.794 1281.509 354 197.38 -69
317 338 Disseminated/ Stringer
296 315 Massive
SSD165 729083.488 7659876.082 1327.031 360 54.55 -85
315 348 Disseminated/ Stringer
SSD167 729076.236 7659875.956 1327.079 318 307.98 -86 296 299 Massive
366 393 Massive
SSD168 729167.725 7660031.965 1281.354 426 258.29 -80.57
393 406 Disseminated/ Stringer
294 318 Massive
SSD169 729070.137 7659870.68 1327.162 414 245.1 -73.98 368 378 Massive
378 389 Disseminated/ Stringer
276 292 Massive
SSD171 729300.327 7659854.648 1344.708 309 224.5 -80.72
292 309 Disseminated/ Stringer
364 380 Massive
SSD172 729285.86 7660050.76 1261 402 216.69 -71.62
380 395 Disseminated/ Stringer
249 282 Massive
SSD173 729299.782 7659854.097 1344.875 312 226 -74.18 282 283 Disseminated/ Stringer
293 296 Massive
366 387 Massive
SSD174 729078.009 7659879.203 1327.168 420 311.11 -85.34
387 409 Disseminated/ Stringer
320 330 Massive
SSD175 729296.684 7659858.441 1344.889 366 271.36 -85.14
330 331 Disseminated/ Stringer
37.7 39.15 Massive
SSD178 729027 7659697 1255 180 242 -75 89.4 114 Massive
114 128.4 Disseminated/ Stringer
15 23 Massive
SSP016 729167.203 7659691.898 1283.69 51 222 -66
23 43 Disseminated/ Stringer
40 64 Massive
SSP017 729170.987 7659700.504 1284.37 78 42 -85
64 65 Disseminated/ Stringer
64 87 Massive
SSP018 729203.52 7659727.514 1290.1 108 222 -75
87 88 Disseminated/ Stringer
74 111 Massive
SSP019 729226.183 7659725.36 1289.95 135 222 -80
111 112 Disseminated/ Stringer
46 54 Massive
SSP020 729138.54 7659711.275 1298.29 92 222 -55
54 55 Disseminated/ Stringer
54 64 Massive
SSP021 729142.13 7659720.029 1298.83 87 222 -73 64 65 Disseminated/ Stringer
70 72 Massive
51 66 Massive
SSP023 729143.738 7659722.381 1298.91 87 180 -65
66 67 Disseminated/ Stringer
76 89 Massive
89 104.839 Massive
SSP024 729143.22 7659722.902 1298.97 123 291 -68
104.839 108 Disseminated/ Stringer
108 114.888 Disseminated/ Stringer
30 39 Massive
SSP025 728901.79 7659611.28 1290.9 42 222 -65
39 41 Disseminated/ Stringer
SSP026 728900.67 7659608.5 1290.9 33 0 -90 21 33 Massive
SSP027 728831.095 7659662.03 1344.33 118 222 -83 91 118 Massive
76 83 Massive
SSP028 728838.799 7659662.854 1344.52 141 136 -63 96 140 Massive
140 141 Disseminated/ Stringer
SSP030A 729004.25 7659716.385 1254.52 57 222 -65 41 42 Massive
65 86 Massive
SSP031 729033.833 7659681.196 1256.41 119 222 -50
86 107 Disseminated/ Stringer
77 81 Massive
SSP033 728868.385 7659701.139 1329.63 108 222 -50
100 108 Massive
81 85 Massive
SSP034 728871.502 7659707.979 1328.57 113 222 -63
107 113 Massive
SSP036 728998.008 7659752.671 1252.91 75 222 -55 59 64 Massive
170 180 Massive
SSP041 728866 7659914 1247.36 265 148.9 -57 228 237 Massive
237 256 Disseminated/ Stringer
159 166 Massive
SSP042 728870 7659910 1248 241 175.9 -53 190 206 Massive
206 218 Disseminated/ Stringer
168 169 Massive
SSP043 728868 7659926 1246.128 277 164.9 -63
222 259 Massive
259 262 Disseminated/ Stringer
180 182 Massive
SSP044 728863 7659916 1247.27 300 174.9 -77
280 295 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 5 of 6

==> picture [494 x 333] intentionally omitted <==

----- Start of picture text -----

Hole Easting (m) Northing (m) mRL Total Depth (m) Collar Azimuth (°) Collar Dip (°) Downhole intercept Mineralisation Type
From (m) To (m)
148 162 Massive
SSP045 728778 7659882 1254 199 169.9 -50 173 181 Massive
181 193 Disseminated/ Stringer
170 194 Massive
SSP046 728772 7659874 1254 223 174.9 -64
194 218 Disseminated/ Stringer
229 241 Massive
SSP047 728776 7659878 1256 259 159.9 -82 241 250 Disseminated/ Stringer
277 289 Massive
289 294 Disseminated/ Stringer
SSP050 729287 7659886 1343.099 310 204.9 -75
299 308 Massive
342 355 Massive
SSP051 729288 7659888 1342.85 390 199.9 -84
355 356 Disseminated/ Stringer
243 258 Massive
SSP052 728774 7659878 1256 265 154.9 -88
258 260 Disseminated/ Stringer
190 192 Massive
SSR001 728885.76 7659933.73 1249.552 292 193.9 -54.84 214 233 Massive
233 240 Disseminated/ Stringer
174 190 Massive
SSR002 728855 7659916.66 1246 274 195.95 -63.37 222 236 Massive
236 239 Disseminated/ Stringer
216 240 Massive
SSR003 728772.88 7659878.9 1252.2 280 215.7 -82.15
240 242 Disseminated/ Stringer
184 196 Massive
SSR004 728854.15 7659917.11 1247.76 274 204.98 -55.01 219 225 Massive
225 243 Disseminated/ Stringer
229 236 Massive
SSR005 728772.2 7659878.7 1252.2 292 254.33 -75.78
236 253 Disseminated/ Stringer
217 223 Massive
SSR006 728772.68 7659878.71 1252.2 298 241.94 -72.98
223 237 Disseminated/ Stringer
SSR007 728903 7659607 1290.9 125 41.4 -60 34 125 Massive
30 96 Massive
SSR008 728901 7659613 1290.9 108 359.43 -71.23 96 104.741 Massive
104.741 108 Disseminated/ Stringer
----- End of picture text -----

Collar coordinates in MGA94_Zone50 grid system. Dip angle convention for Dip measurements: positive is up, negative is down, zero is horizontal.

Page 6 of 6