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Alkane Resources Capital/Financing Update 2021

Feb 15, 2021

48579_rns_2021-02-15_2dc4af2e-e9c9-407c-90ca-9628f6656672.pdf

Capital/Financing Update

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ASX and MEDIA RELEASE

16 February 2021

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Updated San Antonio Resource Estimation Shows Contained Ounces for Tomingley Extension of ~1.1Moz

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  • The Global Mineral Resource (Indicated and Inferred) for the San Antonio Deposit has been updated after an additional 37,000 metres of drilling, and now stands at:

7.3 million tonnes grading 1.72g/t gold (406,000oz)

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  • The San Antonio resource remains open for extensions at depth, with particular focus on the high-grade gold structures within the western monzodiorite and the extension of the northern andesite to the Rosewood Fault, where drilling is restricted due the location of the Newell Highway.

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  • The Global Mineral Resource (Indicated and Inferred) for the Tomingley Extension Project, which includes both the Roswell and San Antonio Deposits now stands at:

  • Indicated 13.8 million tonnes grading 1.96g/t gold (871,000oz) Inferred 3.6 million tonnes grading 1.69g/t gold (195,000oz) Total 17.4 million tonnes grading 1.90g/t gold (1,066,000oz)

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  • Drilling is continuing within the Tomingley Gold Corridor south of San Antonio and north of Roswell, as well as at other, regional near-mine targets.

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  • Detailed mine plans for Roswell and San Antonio, to enable an economic assessment, continue as does community and regulator consultation. These will be released later in Q1 2021.

CONTACT

INVESTORS MEDIA

: NIC EARNER, MANAGING DIRECTOR, ALKANE RESOURCES LTD, TEL +61 8 9227 5677

  • : NATALIE CHAPMAN, CORPORATE COMMUNICATIONS MANAGER, TEL +61 418 642 556

: JOHN GARDNER, CITADEL-MAGNUS, TEL +61 413 355 997

Ground Floor, 89 Burswood Road, Burswood WA 6100, AUSTRALIA (PO Box 4384, Victoria Park WA 6979, AUSTRALIA)

Telephone: +61 8 9227 5677 Facsimile: +61 8 9227 8178 www.alkane.com.au [email protected]

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Alkane Resources Managing Director, Nic Earner, said:

“The updated San Antonio Resource delivers us the opportunity to achieve a further 10+ year mine life for Tomingley. The combined Resources for both Roswell and San Antonio are over 1 million ounces, and over 80% of those ounces are in the Indicated category. This gives us a very solid footing from which to finalise the mine plans for economic assessment. This assessment, combined with stakeholder feedback from consultation and environmental reports, will allow us to progress to the next stage of planning approval with the submission of the Environmental Impact Statement.

“We continue to explore in the region around Tomingley, as well as making small extensions to the known deposits underground. The area is highly prospective and we are looking to growing the resources further as our exploration program continues.”

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Alkane Resources Ltd – San Antonio Resource 16 February 2021

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Tomingley Gold Project

Alkane Resources Ltd 100%

The Tomingley Gold Project (TGP) covers an area of approximately 440km[2 ] stretching 60km north-south along the Newell Highway from Tomingley in the north, through Peak Hill and almost to Parkes in the south. The TGP contains Alkane’s currently producing Tomingley Gold Operations (TGO), an open pit mine and underground operation with a 1Mtpa processing facility.

Over the past three years Alkane has conducted an extensive regional exploration program, which led to the definition Resources at the Roswell and San Antonio prospects.

Alkane has continued consultation with its key stakeholders, including landholders and regulators. The Company has approval to develop an exploration drive from the Wyoming One deposit to Roswell and has prepared preliminary plans for both open-cut and underground mines beneath Roswell and San Antonio. These plans are the basis of Alkane’s current consultation activities as it seeks approval for both underground and open cut mining (refer ASX Announcement 19 August 2020).

Detailed mine plans for Roswell and San Antonio, to enable an economic assessment, will be prepared and released later in Q1 2021.

Geology

The Tomingley gold deposits are interpreted as orogenic gold systems positioned within a major structural zone. This style of deposit is well documented globally with the more significant examples in Australia being the Archean greenstone belts of the Yilgarn Craton in WA and the Paleozoic slate belts in Victoria.

The San Antonio deposit is hosted in the Mingelo Volcanic Formation, a strongly deformed and hydrothermally altered Ordovician belt of volcanics that are predominantly andesitic volcaniclastic breccias, lesser sandstone/siltstone units, lavas and black mudstones. The volcanics are overlain by the younger Cotton Formation siltstones.

The San Antonio deposit is located south of the Roswell deposit (10.1Mt grading 2.04g/t Au for 660,000oz, ASX Announcement 4 November 2020) dextrally displaced and separated by the Rosewood Fault. The drilling has defined north to north-northeast striking, sub-vertically dipping, deformed and attenuated andesitic volcanic and volcaniclastic stratigraphy. The mineralisation at San Antonio is primarily hosted by three ‘brittle’ volcanic units as per the structural setting observed at the Tomingley gold deposits. These volcanics host structural zones generated by a competency contrast between the ‘brittle’ volcanics and ‘ductile’ volcaniclastic meta-sediments. Litho-geochemistry has identified a phosphorous enriched (apatite bearing) andesite 70m to 80m thick with a 10m wide brecciated basal contact that hosts the majority of mineralisation in the northern half of San Antonio. The andesite thins to a thickness of less than 20m to the south and is offset by the west-northwest trending ‘Kenilworth Fault’. The fault appears to rotate the volcanic stratigraphy sinistrally 15[o] to the east. South of the Kenilworth Fault, intruding near or along the margins of the andesite are two thin, less than 10m thick, feldspar phyric dacitic intrusions. These intrusions are invariably mineralised and are the focus to the mineralisation in the southern section of the deposit. A third volcanic unit, approximately 50m thick, is a monzodiorite sub-volcanic sill that is positioned west of the andesite in a similar stratigraphic position as observed at the Roswell deposit. The monzodiorite appears only mineralised north of Kenilworth Fault

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Alkane Resources Ltd – San Antonio Resource 16 February 2021

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forming mineralised lodes with strike lengths of up to 200m. This unit remains poorly constrained by drilling due to the restricted access of the Newell Highway.

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Mineralisation is characterised as Tomingley-style orogenic gold mineralisation, as quartz-carbonatepyrite-arsenopyrite veins hosted in phyllic altered volcanics and volcaniclastics. These sheeted quartz veins are orientated from steeply east dipping to vertical forming sigmoidal shapes, striking approximately north-south to 15[o] east of north, and hosted within subvertical dipping stratigraphy. The mineralisation has been defined by drilling over a strike length of approximately 1,000m and remains open at depth. The more significant sized and higher grading zones of mineralisation are hosted in the andesite in the north and in the dacitic intrusives in the southern sections of San Antonio.

Mineral Resource

A Mineral Resource estimation has been calculated on the San Antonio deposit with a nominal 20 metre drill hole spacing to depths ranging from 30mRL to -200mRL and averaging approximately 250m below ground surface:

Table 1 Mineral Resources at San Antonio and Roswell

Project Resource
Category
Cut-Off Tonnes
(Mt)
Gold Grade
g/t
Gold Metal
(Koz)
San Antonio Indicated 0.5g/t Au 5.93 1.82 347
Inferred 0.5g/t Au 1.39 1.32 59
Total 0.5g/t Au 7.32 1.72 406
Roswell Indicated 0.5g/t Au 7.88 2.07 524
Inferred 0.5g/t Au 2.19 1.93 136
Total 0.5g/t Au 10.1 2.04 660
Total Resource Inventory Indicated 0.5g/t Au 13.80 1.96 871
Inferred 0.5g/t Au 3.58 1.69 195
Total 0.5g/t Au 17.4 1.90 1066

Full details are provided in the appended JORC Table 1 and text summary below

The Mineral Resource will be subject to further infill and extensional drilling with a view to both define the continuity of the mineralisation and high-grade zones at depth.

A 3D model of the San Antonio mineralisation is displayed below.

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Exploration Upside at San Antonio

The Mineral Resource estimation was calculated down to the 20mRL on average and there is upside to test further depth extensions to the main zones of mineralisation. In particular in the south of San Antonio targeting the dacitic host that appears to correlate well with strong mineralisation.

Other exploration targets at San Antonio that remain poorly understood are due to the restricted access of the Newell Highway and include the western monzodiorite which is a significant host rock for mineralisation at the Tomingley gold deposits and the northern zone proximal to the Rosewood Fault.

The western monzodiorite is currently defined by deep drilling to a 500m strike length. The unit commonly hosts visible gold bearing structures including intercepts such as RWRC213 – 15m grading 7.43g/t Au from 147m within the central portion of the lithology. The monzodiorite host is open along strike and is poorly constrained by the current drilling due to the position of the Newell Highway.

The area between the northern contact of the andesite and the Rosewood Fault is approximately 100m in strike length and also remains poorly tested due to the restricted access of the Newell Highway. Drilling has defined the northern contact to the andesite as steeply north plunging. This area within the andesite host has a similar structural setting as the Roswell mineralisation immediately north of the Rosewood Fault and further drilling is planned to test this.

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SAN ANTONIO MINERAL RESOURCE – Supporting information

The Mineral Resource Statement for the San Antonio Mineral Resource Estimate (MRE) is reported according to the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (the ‘JORC Code’) 2012 edition.

In the opinion of Alkane, the resource estimation reported is a reasonable representation of the global gold mineral resource within the San Antonio deposit, based on reverse circulation and diamond drilling sampling data available as of January 2021, and is detailed below:

Drilling Techniques

The San Antonio deposit has been evaluated using all of Alkane’s reverse circulation (RC) and diamond drilling (DD) holes within the prospect area. No previous companies’ exploration drilling in the region (shallow air-core and RAB holes) or Alkane’s reconnaissance air-core drilling was used in the assessment.

Drilling at the San Antonio deposit has been completed in six phased programs since January 2018 for a total of 345 RC and diamond core holes for 75,196 metres. Mitchells Services Ltd were contracted for the initial phase of resource definition RC drilling and 2 diamond core holes. Ophir Drilling Pty Ltd were used for the remainder of the diamond core drilling. Strike Drilling Pty Ltd were contracted to complete the infill resource RC drilling. Drilling statistics are summarised in Table 2.

Table 2 Summary Drilling Statistics

San Antonio Drilling Statistics (reconnaissance air-core drill holes excluded)
Hole Type Reverse Reverse
Circulation
HQ3 Diamond PQ3 Diamond Total

Air-Core
Circulation

(pre-collars)
(pre-collars)
No. Holes 13 36 296 46 3 345
Metres 1,026.9 5,294.6 57,952.5 10,556.4 365.5 75,195.9

Initial shallow reconnaissance drilling to fresh rock is completed using 90mm (3.5”) air core. Gold and arsenic anomalism was followed up with deeper drilling completed by RC (144mm or 5¾”) and HQ3 and PQ3 diamond core drilling. Resource definition drilling has been completed on east-west sections. Drill sections are spaced 20m apart with drill holes at 20m intervals along these sections. Air-core drilling was not included in the resource estimation.

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Sampling and Sub-Sampling Techniques

Sampling on all drilling techniques was conducted from the base of alluvium (the transported overburden contains no economic gold grades) to the bottom of hole. Sampling via the different drilling techniques used is described as follows:

RC Drilling:

Samples from the RC drilling were collected at 1 metre intervals via a cyclone into large plastic bags. Spear samples were collected from each 1 metre sample and composited to 3 metre for initial analysis unless the geologist on site determined visually strong mineralisation, then 1 metre samples were collected via a splitter below the cyclone and sent for analysis.

All composites assaying ≥0.2g/t Au together with their upper and lower bounding composite samples were re-split as 1 metre samples collected at the time of drilling into a calico bag via a splitter below the cyclone.

Diamond Core Drilling:

Half core samples were collected from all geologically logged and potential mineralised zones from the diamond core drill holes. The core was sampled for assay in a range of 0.3 metre to 1.3 metre intervals as determined by the geologist based on lithological contacts, alteration zones and mineralisation zones. Geotechnical and bulk density measurements were collected as well as lithology logging and structural data. The remainder of the core was transferred to racking and stored at the decommissioned Peak Hill Gold Mine.

Sample Analysis Method

All samples were submitted to ALS Chemex Laboratory in Orange. Samples were oven dried prior to crushing to <6mm using a jaw crusher (in the case of diamond core), split to 3kg if required then pulverised in an LM5 (or equivalent) to ≥85% passing 75µm. Bulk rejects for all samples were discarded. A pulp packet (±100g) is stored for future reference.

For all samples used in the resource estimate, gold was determined using a 50g charge fused at approximately 1100°C with alkaline fluxes, including lead oxide. The resultant prill was dissolved in aqua regia and gold determined by flame AAS.

In addition to gold assay, RC samples were assayed for As, Cu, Ni, P, and Ti by aqua regia digest AAS finish (ALS method code ME-ICP41). Diamond core analyses in addition to gold, were assayed for a full multielement suite using a multi-acid complete digest, with an AES and MS finish.

Commercially prepared Certified Reference Materials (CRM) and blanks were inserted at approximately 1 in 35 samples. CRM’s were not identifiable to the laboratory. Standards were deemed to be within tolerance if the result was within 3 standard deviations and 10% of the expected value. When a standard fell outside this tolerance, the standard along with a selection of samples from the batch were resubmitted. These “failed” samples are not included in the resource estimation. Overall, the CRM pass rate over 99.9%.

Field duplicate samples were inserted at 1 in 45 samples (alternate to CRM’s). Field duplicate samples were collected by riffle splitting the RC sample. The coefficient of determination for gold is relatively high at 0.95 showing good repeatability for a gold deposit. A high correlation coefficient of 0.98 for arsenic

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indicates that the lower correlation coefficient in gold is due to a small nugget effect rather than improper sampling procedures.

Laboratory QAQC sampling includes insertion of CRM samples, internal duplicates and screen tests. This data was reported for each sample submission. Umpire laboratory check samples were forwarded to SGS Laboratory in West Wyalong for Au analyses over the course of the resource drilling campaign as a 1.5% proportion of total assays. In general, the results were repeatable between the laboratories with no statistically significant bias detected.

In the competent persons opinion, the laboratory has performed satisfactorily over the resource drilling campaign and any noted discrepancies are acceptable for the resource classification applied.

Geology and Geological Interpretation

The geology, structural setting, alteration and mineralisation is very similar to the deposits at the Tomingley Gold Operations. The total resource inventory of the four deposits at Tomingley totalled 14.29 million tonnes grading 2.0g/t gold at a 0.5g/t cutoff for 921,000 ounces of gold before commencement of mining.

The Tomingley, San Antonio and Roswell deposits are positioned within a gold-arsenic structural zone termed the Tomingley Gold Corridor that is approximately 500m wide and located immediately east of the Cotton Formation contact. The Tomingley Gold Corridor begins approximately 5km north of Tomingley, is approximately 30km in length, and strikes south through Peak Hill. The individual prospects and deposits within the corridor all have their own structural nuances and mineralisation is dominantly hosted within brittle sub-volcanic sills or lavas or along their immediate contacts with volcaniclastic metasediments.

The alteration appears multiphase with repeated cracking, crushing, veining and sealing, leading to heterogeneous, patchy alteration and discontinuous veins. It is characterised by a bleaching white mica (muscovite)-carbonate (ankerite)-albite-silica ± chlorite as pervasive replacement of the host rock around strong quartz-carbonate (ankerite)-pyrite-arsenopyrite ± albite veining.

Multiple phases and recrystallisation of pyrite and arsenopyrite occur early in the paragenesis. Late fractures in earlier pyrite and arsenopyrite have served as nucleation sites for the precipitation of gold which occurs within or disseminated near the selvages of the quartz-ankerite vein assemblage.

The San Antonio Deposit is positioned south of a regional northwest trending Rosewood Fault. This structure, originally identified in the aeromagnetics, appears dextral and is of a similar orientation to the structure that dextrally displaces the Caloma deposits from the Wyoming deposits at Tomingley, positioned in the centre of the mined deposits. A second significant structure named the Kenilworth Fault is orientated west-northwest and transects the southern section of the San Antonio deposit. These important cross-cutting structures may cause transpression after an intense period of compression during an orogeny, resulting in suitable volcanic host rocks to act as structural buttresses in which hydrothermal fluids pond and precipitate gold.

The stratigraphy at San Antonio comprises immature volcaniclastic sandstones and conglomerates with lesser siltstones/mudstones. More evolved, fine grained plagioclase phyric multi-phased andesite lavas, are slightly magnetic, and hosts a significant proportion of the gold mineralisation. In thin section, the andesite lavas have abundant tiny apatite needles within the plagioclase, accounting for the slightly

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elevated phosphorous concentration in comparison to the other volcaniclastics and lavas within the stratigraphic package.

Intruding into this volcanic package west of the andesite lava, is a monzodiorite that appears to have the same petrographic qualities as the sub-volcanic sills that host the majority of the mineralisation at the Tomingley deposits. This unit is poorly constrained by drilling with only a few drill holes testing along strike from mineralisation defined within the central portion of this unit. This favourable unit for hosting mineralisation is open along strike.

A second type of intrusive, feldspar phyric dacites, are identified only in the southern portion of San Antonio and intrude along or proximal to the contacts of the andesite. Although less than 10m thick where intersected these intrusives are usually strongly mineralised.

The mineralisation at San Antonio is characterised as quartz-carbonate-pyrite-arsenopyrite veins hosted in phyllic altered volcanics and volcaniclastics. The mineralised zones range from 2m to 20m wide and form as sheeted sigmoidal tension veins, sometimes becoming more brecciated and shear hosted along the eastern contact with the andesite host.

The mineralisation at San Antonio can be displaced by an occasional 1m - 3m thick post mineralisation dolerite dykes. The dolerite dykes in the region are Devonian aged and have a similar orientation, dipping steeply to the north-northeast.

Weathering of the mineralised bedrock has developed a saprolitic clay profile extending approximately 35 metres from the base of alluvium to fresh rock. The mineralised bedrock lies beneath a Cainozoic alluvium overburden between 20m - 60m thick.

The andesites, monzodiorite, dacites, dolerites, alluvium and base of oxidation were modelled in 3D and formed the basis of wireframing the mineralisation in the estimation. The wireframes were built by Alkane geologists. This informed the estimates and along with grade guided the interpretation of the ore envelope wireframes at a nominal 0.2g/t Au lower cut-off. Where the intercept gold value was below the nominal cut-off and the mineralisation continuity was supported by veining and alteration, the intercept was included within the domain due to the commodity and the style of deposit.

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Estimation Methodology

Grade estimation was completed using Ordinary Kriging (OK) with dynamic anisotropy to optimise search ellipse orientation within the lodes. All wireframing and estimation was completed with Datamine Studio RM software.

Exploratory data analysis of the capped and declustered composited gold variable within each domain was undertaken by Cube Consulting with variograms being produced using Datamine/Snowden Supervisor software. Sample data was composited into one metre downhole lengths using a best fit methodology.

Cube conducted an estimation search neighbourhood analysis to determine optimal search parameters for Ordinary Kriging (OK) estimation of gold grade. This analysis was carried out on only the well informed domains. This determined an optimum block size to be 5mX x 10mY x 10mZ and sub-blocking down to 2.5mX x 2.5mY x 2.5mZ. Less well-informed domains utilised variogram model parameters substituted from other, better informed lodes based on statistical similarity. Blocks in very poorly informed domains (i.e. due to small volume and very few samples) were assigned the mean sample grade of that domain.

A top cut analysis was carried out by a visual inspection of the data using histograms, log-transformed probability plots, percentile analysis and sensitivity analysis for individual domains to identify population outliers. The spatial location of the outliers was also taken into consideration for the application of the grade caps. The sensitivity analysis involved analysing varying cap values, to estimate the contribution of each sample to the overall metal content. Capping was deemed necessary for most of the well informed domains.

Distance limiting threshold was used during the estimation process on domains that had evidence for high-grade shoots in order to prevent undue propagation of these high-grade values.

Estimation utilised a 2-way skin within 5m either side of the modelled oxide surface between the oxide and fresh domains. All other domain boundaries are hard boundaries where only composite samples within that domain were used to estimate blocks coded as within that domain.

Validation of the modelling parameters and processes of estimation included visual inspections in section, plan and in 3D and a comparison of an ID2 model vs the OK model. In the competent persons opinion, all methods of validation produced acceptable results.

Classification Criteria

Mineral Resources were classified as Inferred or Indicated to appropriately represent confidence and risk with respect to data quality, drill hole spacing, geological and grade continuity, mineralisation volumes, as well as metal distribution. There is no material classified as Measured.

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

  • Drill spacing was averaging a nominal 20m, or where drilling was within 20m of the block estimate; and

  • Estimation quality is considered to be of high confidence in respect to low kriging variance.

Remaining estimated blocks within the defined mineralisation domains were classified as Inferred Resources (this included most blocks in the less well-informed domains and all blocks in the very poorlyinformed and unclassified domains). The dimensions of the search ellipse were based on the recommended search neighbourhood parameters.

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Cut-Off Grade

The Mineral Resource cut-off grade for reporting of global gold resources for the San Antonio deposit chosen as 0.5g/t gold for open cut mining. This was based upon economic parameters utilised at Tomingley Gold Operations where deposits of the same style, commodity, comparable size and mining methodology are currently being extracted.

Mining

It was assumed that mineralisation at the San Antonio deposit would be extracted using open cut methods of a similar scale and size as per the Tomingley Gold Operations (TGO). Underground could be potentially mined via medium to small scale mechanised underground mining methods, like that currently being implemented at TGO.

No dilution or cost factors were applied to the estimate.

Metallurgy

The metallurgy of the Tomingley deposits is well studied. Tomingley Gold Operations has been processing ore since 2014 from its four deposits and during this time no metallurgical issues have arisen, with recoveries ranging between 92% - 94%. Preliminary metallurgical work on San Antonio ore suggests it has similar metallurgical qualities as per the Tomingley deposits. Further metallurgical test work is underway.

No metallurgical recovery factors were applied to the Mineral Resources or Resource Tabulations.

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Competent Person

Unless otherwise advised above, the information in this report that relates to exploration results and mineral resources being reported for the first time is based on information compiled by Mr David Meates MAIG, (Alkane Exploration Manager NSW) who has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Meates has provided his prior written consent to the inclusion in this report of the matters based on his information in the form and context in which it appears.

The information in this report that relates to previously reported exploration results and exploration targets is extracted from the Company’s ASX announcements noted in the text of the announcement and are available to view on the Company’s website. The Company confirms that it is not aware of any new information or data that materially affects the information included in the original announcements and that the form and context in which the Competent Person’s findings are presented have not been materially altered.

Disclaimer

This report contains certain forward looking statements and forecasts, including possible or assumed reserves and resources, production levels and rates, costs, prices, future performance or potential growth of Alkane Resources Ltd, industry growth or other trend projections. Such statements are not a guarantee of future performance and involve unknown risks and uncertainties, as well as other factors which are beyond the control of Alkane Resources Ltd. Actual results and developments may differ materially from those expressed or implied by these forward looking statements depending on a variety of factors. Nothing in this report should be construed as either an offer to sell or a solicitation of an offer to buy or sell securities.

This document has been prepared in accordance with the requirements of Australian securities laws, which may differ from the requirements of United States and other country securities laws. Unless otherwise indicated, all ore reserve and mineral resource estimates included or incorporated by reference in this document have been, and will be, prepared in accordance with the JORC classification system of the Australasian Institute of Mining, and Metallurgy and Australian Institute of Geoscientists.

ABOUT ALKANE ‐ www.alkane.com.auASX: ALK

Alkane Resources is poised to become Australia’s next multimine gold producer.

The Company’s current gold production is from the Tomingley Gold Operations in Central West New South Wales, where it has been operating since 2014 and is currently expediting a development pathway to extend the mine’s underground and open pit potential.

Alkane has an enviable exploration track record and controls several highly prospective gold and copper tenements. Its most advanced exploration projects are in the tenement area between Tomingley and Peak Hill, which have the potential to provide additional ore for Tomingley’s operations.

Alkane’s exploration success includes the landmark porphyry gold-copper mineralisation discovery at Boda in 2019. With a major drill program ongoing at Boda throughout FY2021, Alkane is confident of further consolidating Central West New South Wales’ reputation as a significant gold production region.

Alkane’s gold interests extend throughout Australia, with strategic investments in other gold exploration and aspiring mining companies, including ~19.9% of Genesis Minerals (ASX: GMD) and ~10.3% of Calidus Resources (ASX: CAI).

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The following tables are provided to ensure compliance with the JORC Code (2012) edition requirements for the reporting of exploration results.

APPENDIX 1

JORC Code, 2012 Edition – Table 1 report – San Antonio February 2021

Section 1 Sampling Techniques and Data

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

Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
Sampling
techniques

Nature and quality of sampling (eg cut channels, random chips, or specific specialised
industry standard measurement tools appropriate to the minerals under investigation,
such as down hole gamma sondes, or handheld XRF instruments, etc). These examples
should not be taken as limiting the broad meaning of sampling.
The San Antonio deposit has been evaluated using reverse circulation and diamond drilling
techniques.
Reverse Circulation (RC) samples are collected at one metre intervals via a cyclone and riffle
or cone splitter. Intervals outside of visual ore zones are composited to 3 metres.
Diamond Drilling (DD) sample intervals are defined by geologist during logging to honour
geological boundaries.

Include reference to measures taken to ensure sample representivity and the appropriate
calibration of any measurement tools or systems used.
RC drilling completed to industry standards.
Core is laid out in suitably labelled core trays. A core marker (core block) is placed at the end
of each drilled run (nominally 3 or 6m) and labelled with the hole number, down hole depth,
length of drill run. Core is aligned and measured by tape, comparing back to this down hole
depth consistent with industry standards.

Aspects of the determination of mineralisation that are Material to the Public Report. In
cases where ‘industry standard’ work has been done this would be relatively simple (eg
‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire assay’). In other cases more explanation
may be required, such as where there is coarse gold that has inherent sampling
problems. Unusual commodities or mineralisation types (eg submarine nodules) may
warrant disclosure of detailed information.
RC Drilling - approximately 10% (3kg) of total sample is delivered via cone or riffle splitter
into a calico bag with the remaining sample delivered into a large plastic bag and retained
for future use if required.
DD Drilling – sample intervals defined by geologist during logging to honour geological
boundaries.
All samples sent to laboratory are crushed and pulverised to produce a ~100g pulp for assay
process.
All samples are fire assayed using 50g charge.
Visible gold is occasionally observed in core.
Drilling
techniques

Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger,
Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of
diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what
method, etc).
The resource is based on 296 RC drill holes totalling 64,274 metres (including pre-collars for
diamond holes) and 49 diamond core (DD) drill holes totalling 10,922 metres of core.
Conventional RC drilling using 100mm rods and 144mm face sampling hammer.

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Criteria JORC Code explanation Commentary
Diamond drill holes were pre-collared using either air core or RC drilling through to competent
material in fresh rock for an average depth of 130m and cased down to triple tube HQ3
(64mm diameter) and PQ3 (83mm diameter) core tails. Diamond core is oriented using the
“Reflex” core orientation tool.
Drill
sample
recovery

Method of recording and assessing core and chip sample recoveries and results
assessed.
RC - sample recovery is visually estimated and generally very good (>90%) aided using
oversized shrouds through oxide material. Samples are even sized. Samples are
occasionally damp or wet in RC holes drilled below 250 metres. Sample quality is assessed
by the sampler by visual approximation of sample recovery and if the sample is dry, damp or
wet. Riffle and cone splitters were used to ensure a representative sample was achieved on
all 1 metre samples.
DD - core loss is identified by drillers and calculated by geologists when logging. Generally,
≥99% was recovered.

Measures taken to maximise sample recovery and ensure representative nature of the
samples.
RC drilling completed using oversized shrouds to maintain sample return in oxide zone and all
samples are split using riffle or cone splitters. Use of RC rigs with high air capacity assists in
keeping samples dry.
Triple tube coring is used at all times to maximise core recovery.

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.
There is no known relationship between sample recovery and grade.
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.
RC - each one metre interval is geologically logged for characteristics such as lithology,
weathering, alteration (type, character and intensity), veining (type, character and
intensity) and mineralisation (type, character and volume percentage).
DD - all core is laid out in core trays and geologically logged for characteristics such as
lithology, weathering, alteration (type, character and intensity), veining (type,
character and intensity) and mineralisation (type, character and volume percentage).
A detailed geotechnical log is also undertaken collecting parameters such as core
recovery, RQD, fracture count, and fracture type and orientation.

Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc)
photography.
All logging is qualitative with visual estimates of the various characteristics.
RC - A representative sample of each one metre interval is retained in chip trays for future
reference.
DD - Core is photographed and all unsampled core is retained for reference purposes.

The total length and percentage of the relevant intersections logged.
All DD core and RC chip samples have been geologically and geotechnically logged by
qualified geologists.

If core, whether cut or sawn and whether quarter, half or all core taken.
DD - zones of visual mineralisation and/or alteration are marked up by the geologist and cut
in half usinga Corewise automatic core cuttingsaw. The right half is sampled to sampling

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
Sub-sampling
techniques and
sample
preparation
intervals that are generally based on geology but do not exceed 1.3 metres in length. The
left half is archived. All mineralised zones are sampled, plus >5m of visibly barren wall rock.
Laboratory Preparation – drill core is oven dried prior to crushing to <6mm using a jaw
crusher, split to 3kg if required then pulverised in an LM5 (or equivalent) to ≥85% passing
75µm. Bulk rejects for all samples are discarded. A pulp packet (±100g) is stored for future
reference.

If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or
dry.
RC - for each one metre interval with visual mineralisation and/or alteration the calico sample
bag is numbered and submitted to the laboratory for analysis. Intervals without visual
mineralisation and/or alteration are spear sampled and composited over three metres. Damp
or wet samples are recorded by the sampler. For composited intervals returning grades
>0.2g/t Au the calico bags are retrieved for assay.
Laboratory Preparation – the entire RC sample (3kg) is dried and pulverised in an LM5 (or
equivalent) to ≥85% passing 75µm. Bulk rejects for all samples are discarded. A pulp packet
(±100g) is stored for future reference.

For all sample types, the nature, quality and appropriateness of the sample preparation
technique.
ALK sampling techniques are of industry standard and considered adequate.

Quality control procedures adopted for all sub-sampling stages to maximise
representivity of samples.
RC – field duplicate samples collected at every stage of sampling to control procedures
DD – external laboratory duplicates used.

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.
RC - Duplicate samples are riffle split from the riffle/conical split calico from the drill rig.
Duplicates show generally good repeatability, indicating a negligible “nugget” effect.

Whether sample sizes are appropriate to the grain size of the material being sampled.
Sample sizes are assumed to be within industry standard and considered appropriate.
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.
Gold is determined using a 50g charge fused at approximately 1100°C with alkaline fluxes,
including lead oxide. The resultant prill is dissolved in aqua regia and gold determined by
flame AAS.
For other geochemical elements samples are digested in either aqua regia or a multi-acid
digest with each element concentration determined by ICP Atomic Emission Spectrometry
or ICP Mass Spectrometry. These additional elements are generally only used for geological
interpretation purposes, are not of economic significance and are not routinely reported.

For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters
used in determining the analysis including instrument make and model, reading times,
calibrations factors applied and their derivation, etc.
Not applicable to this report or deposit.

Nature of quality control procedures adopted (eg standards, blanks, duplicates, external
laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and
Commercially prepared Certified Reference Materials (CRM) are inserted at 1 in 35 samples.
CRM’s are not identifiable to the laboratory.

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Criteria JORC Code explanation Commentary
precision have been established. Field duplicate samples are inserted at 1 in 45 samples (alternate to CRM’s).
Laboratory QAQC sampling includes insertion of CRM samples, internal duplicates and
screen tests. This data is reported for each sample submission.
Failed standards result in re-assaying of portions of the affected sample batches.
1.5% of gold assay results from ALS Orange were checked using SGS West Wyalong as an
external umpire laboratory.
Verification
of
sampling
and
assaying

The verification of significant intersections by either independent or alternative company
personnel.
Drill data is compiled, collated and reviewed by senior Alkane staff. Cube Consulting was
used to verify exploration data to determine the resource estimation parameters.

The use of twinned holes.
Twinned holes have not been used at San Antonio.

Documentation of primary data, data entry procedures, data verification, data storage
(physical and electronic) protocols.
Early drill hole logging and sampling data is hard keyed into excel spreadsheet for transfer
and storage in an access database with verification protocols in place. More recent data is
verified in the field and uploaded using Geobank.
All primary assay data is received from the laboratory as electronic data files which are
imported into sampling database with verification procedures in place. QAQC analysis is
undertaken for each laboratory report.
Digital copies of Certificates of Analysis (COA) are stored in a central database with regular
(daily) backup.
Data is also verified on import into mining related software.

Discuss any adjustment to assay data.
No assay data was adjusted. In the case of assay checks the original assay is utilised as
there was no statistical variability.
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.
Drill holes are laid out using handheld GPS (accuracy ± 2m) then surveyed accurately with
DGPS_RTK (± 0.1m) by TGO trained surveyors on completion.
RC drill holes are surveyed using a single shot electronic camera at a nominal 30m down
hole interval.
DD are surveyed at nominal 30m down hole during drilling to maintain drilling direction and
then at 6m intervals on retrieval of rod string using a multi shot electronic camera.

Specification of the grid system used.
MGA94 grid system was used.

Quality and adequacy of topographic control.
A site based digital terrain model was developed from accurate (± 0.1m) survey control by
licenced surveyors.

Data spacing for reporting of Exploration Results.
Nominal drill hole spacing is 20m x 20m, moving out to variable spacing approaching 40m at
depth.

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
Data
spacing
and distribution
The data spacing is deemed to be sufficient in reporting a Mineral Resource.

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 drill hole spacing has been shown to be appropriate by variography.

Whether sample compositing has been applied.
RC – samples with no visible mineralisation or alteration are composited to 3m with 1m
resamples assayed if the composite returned a gold value of >0.2g/t gold. One metre
samples override 3m composites in the database.
DD – core is sampled to geology with sample sizes ranging from 0.3m to 1.3m.
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.
Much care is given to attempt to intersect structure at an optimal angle but in complex ore
bodies this can be difficult. Intersections are approximately 60% of true widths.

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.
It is not thought that drilling direction will bias assay data at San Antonio.
Sample
security

The measures taken to ensure sample security.
All samples are bagged in tied numbered calico bags, grouped into larger tied polyweave
bags and transported 5 minutes away to Tomingley Gold Mine. The samples are placed in
large sample cages with a sample submission sheet and couriered to ALS in Orange via
freight truck. All sample submissions are documented via ALS tracking system and all assays
are reported via email.
Sample pulps are returned to site and stored for an appropriate length of time (minimum 3
years).
The Company has in place protocols to ensure data security.
Audits
or
reviews

The results of any audits or reviews of sampling techniques and data.
The Company does not routinely have external consultants verify exploration sampling
techniques. The Company has provided accurate resource estimations at Tomingley Gold
Operations using these described sampling techniques.
Cube Consulting is used to verify exploration data and to determine the resource estimation
parameters.

Section 2 Reporting of Exploration Results

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(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.
EL5675 wholly owned by Alkane Resources Ltd (ALK).

The security of the tenure held at the time of reporting along with any known impediments
to obtaining a licence to operate in the area.
EL5675 is due to expire 17 January 2023.
Exploration
done by other
parties

Acknowledgment and appraisal of exploration by other parties.
All reported drilling completed by ALK.
Geology
Deposit type, geological setting and style of mineralisation.
Mineralisation at San Antonio is similar to the well documented Tomingley Gold Deposits.
San Antonio like Tomingley is associated with quartz veining and alteration focused within
andesitic volcanics and adjacent volcaniclastic sediments. The deposits appear to have
formed as the result of a competency contrast between the volcanics and the surrounding
volcaniclastic sediments, with the volcanics showing brittle fracture and the sediments ductile
deformation and have many similarities to well documented orogenic - lode-style gold
deposits.
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
o
hole length.
Too many, not practical to summarise all drill hole data used.
All material information has been previously reported in the following announcements:
29 March 2019, ASX Announcement;
12 June 2019, ASX Announcement;
12 August 2019, ASX Announcement;
23 September 2019, ASX Announcement;
6 November 2019, ASX Announcement;
5 December 2019, ASX Announcement;
17 January 2020, ASX Announcement;
9 March 2020, ASX Announcement;
9 April 2020, ASX Announcement.
22 June 2020, ASX Announcement;

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
16 July 2020, ASX Announcement;
28 August 2020, ASX Announcement;
16 December 2020, ASX Announcement;
27 January 2021, ASX Announcement.

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.
Exclusion of drill hole data will not detract from the understanding of this report. All drill data
has been previously reported, holes are close spaced and near a developed mining area.
Data
aggregation
methods

In reporting Exploration Results, weighting averaging techniques, maximum and/or
minimum grade truncations (eg cutting of high grades) and cut-off grades are usually
Material and should be stated.
Exploration results previously reported –
for uncut gold grades;
Intercepts are defined (bounded) by 0.25g/t gold outer limit and may contain
some internal waste;
Only intervals grading ≥0.5 g/t gold are reported;
Grades are calculated by length weighted average.

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.
Exploration results previously reported as length weighted average grades with internal high
grade intercepts reported separately.

The assumptions used for any reporting of metal equivalent values should be clearly
stated.
No metal equivalents are reported.
Relationship
between
mineralisation
widths
and

These relationships are particularly important in the reporting of Exploration Results.
o
If the geometry of the mineralisation with respect to the drill hole angle is known, its
nature should be reported.
o
If it is not known and only the down hole lengths are reported, there should be a clear
Previously reported exploration results include an estimate of true width. The mineralisation
is structurally complex and true widths are variable depending on the ore zone intersected
however range between 50% and 70% of drill intersection.

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
intercept
lengths
statement to this effect (eg ‘down hole length, true width not known’).
Diagrams
Appropriate maps and sections (with scales) and tabulations of intercepts should be
included for any significant discovery being reported These should include, but not be
limited to a plan view of drill hole collar locations and appropriate sectional views.
Cross sections and a plan showing geology with drill collars were included with previously
reported exploration results detailing the unfolding significant discovery.
Various plans and sections illustrating the modelled ore zones with all drill traces are
attached.

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Criteria JORC Code explanation Commentary
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.
Data relating to all exploration drill holes has been reported in previous documentation of
exploration results.
Other
substantive
exploration
data

Other exploration data, if meaningful and material, should be reported including (but not
limited to): geological observations; geophysical survey results; geochemical survey
results; bulk samples – size and method of treatment; metallurgical test results; bulk
density, groundwater, geotechnical and rock characteristics; potential deleterious or
contaminating substances.
No additional or new drilling results are being reported at this time.
Further work
The nature and scale of planned further work (eg tests for lateral extensions or depth
extensions or large-scale step-out drilling).
Additional drilling is planned into the deeper parts of the deposit to infill the drilling to 20m x
20m spacing to convert the inferred resources to Indicated and Measured. Deep core drilling
is also being planned to test the continuation high grade mineralised structures at depth. The
lateral extensions north, south and west of San Antonio remain open due to the restricted
access of the Newell Highway. Future drilling is planned from the western side of the highway
to better test these extensions.

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary

Diagrams clearly highlighting the areas of possible extensions, including the main
geological interpretations and future drilling areas, provided this information is not
commercially sensitive.
The attached image above shows estimated blocks coloured showing different grades of
mineralisation highlighting the high grade potential down dip for further exploration.

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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.
In the early stages of the exploration at San Antonio logging data is entered into Excel via
drop down menus. All raw data is loaded directly to the Datashed database from the assay,
logging and survey derived files. More recent data is captured directly through Geobank
Mobile and validated before uploading into the Geobank database.

Data validation procedures used.
There are validation checks to avoid duplications of data.
The data are further validated for consistency when loaded into Geobank and desurveyed.
Site visits
Comment on any site visits undertaken by the Competent Person and the outcome of
those visits.
(If no site visits have been undertaken indicate why this is the case.)
The Competent Person has visited drill sites, regularly visits the exploration office for
geological discussions, drilling updates, viewing of the data and of the core. The deposit is
completely covered by 20m to 60m of barren alluvium and there is nothing to see on the
surface.
Geological
interpretation

Confidence in (or conversely, the uncertainty of ) the geological interpretation of the
mineral deposit.
The geological model is built on structural data from core and lithological logging. The lode
strike orientations are similar to Tomingley which approximate the strike of the volcanic
bodies. The domain wireframes were built by Alkane geologists.

Nature of the data used and of any assumptions made.
Structural measurements from oriented drill core was used to assist in the geological
interpretation along with lithological, alteration and mineralisation logging of RC chips.
Lithogeochemistry was used to help define the different lithologies.

The effect, if any, of alternative interpretations on Mineral Resource estimation.
A steeply east dipping interpretation was initially proposed over the entire San Antonio
deposit however this was inconsistent with structural measurements obtained from oriented
drill core in some sections of the deposit. This original orientation remains the case for the
northern domains, however domains in the southern andesite are vertical and in the central
monzodiorite are vertical to slightly overturned and steep west dipping. This alternative
interpretation had a marginal negative effect (<5%) on the initial Inferred Resource Estimate.

The use of geology in guiding and controlling Mineral Resource estimation.
Geological (lithological) logging together with lithogeochemistry was used to develop a
geological model. Alteration and mineralisation estimates along with grade guided the
interpretation of the ore envelope wireframes.
Most of the mineralisation is hosted by quartz veins within an andesite host rock, or along its
margins within the volcaniclastics. A thin and high-grade domain is hosted within a
monzodiorite positioned west of the San Antonio deposit. A third volcanic body was identified
by recent lithogeochemistry as a dacite intrusive and hosts a significant amount of
mineralisation in the southern section of San Antonio.

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Criteria JORC Code explanation Commentary
Dolerite dykes post-date mineralisation and all mineralised lodes are truncated and stoped
out by the modelled dolerites.

The factors affecting continuity both of grade and geology.
Mineralisation is directly associated with alteration and veining.
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.
Strike length ~ 1,000m
Width ~ 10m to ~ 80m
Depth ~ 20m to ~ 60m from below surface to ~ 250m to ~ 350m below surface from deepest
drilling intercept.
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.
The resource model has used all the exploration drill data.
26 mineralisation wireframes (domains), 4 dolerite wireframes, 2 fault wireframes and 4
volcanic wireframes were interpreted and used as constraints for the resource modelling.
Three surfaces were also used to separate material types - topography, alluvium and base
of oxidation surfaces.
The material type classification was used to allocate density values.
The drillhole data was flagged by the domain wireframes in priority order, to prevent double
use of the data in any intersecting zones.
The drill hole data was flagged by dolerite and mineralised domain wireframes in priority
order, to prevent double use the data in the intersecting zones. The mineralised zones of
greater than 0.20g/t gold were wireframed and the samples within their respective zones
were flagged, in order to prevent any overestimation that could be caused by use of assays
outside these boundaries.
Top-cuts were selected for each domain based on a visual inspection of the data using
histograms, log-transformed probability plots, percentile analysis and sensitivity analysis for
individual domains. Spatial location of the outliers was also taken into consideration for the
application of the grade caps. The sensitivity analysis involved analysing varying cap values,
to estimate the contribution of each sample to the overall metal content. Capping was
deemed necessary for most of the domains.
An estimation search neighbourhood analysis was used to determine optimal search
parameters for Ordinary Kriging (OK) estimation of gold grade. This analysis was carried out
on only the well informed domains. This determined an optimum block size to be 5mX x
10mY x 10mZ and taking in account of the SMU used at TGO determined a sub-blocking
size of 2.5mX x 2.5mY x 2.5mZ.
Grade estimation was completed using Ordinary Kriging (OK) with dynamic anisotropy. All
wireframing and estimation was completed with Datamine Studio RM and checked using ID2.

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary

The availability of check estimates, previous estimates and/or mine production records
and whether the Mineral Resource estimate takes appropriate account of such data.
The previous estimate was an Inferred Resource calculation based on shallower broadly
spaced drilling. There is no previous production data to provide any validation.

The assumptions made regarding recovery of by-products.
No assumptions made - estimates were made only for gold.

Estimation of deleterious elements or other non-grade variables of economic significance
(eg sulphur for acid mine drainage characterisation).
No deleterious elements identified for estimation.

In the case of block model interpolation, the block size in relation to the average sample
spacing and the search employed.
An optimum block size to be 5mX x 10mY x 10mZ and a sub-blocking size of 2.5mX x 2.5mY
x 2.5mZ was determined as appropriate for a 20m x 20m drilled resource.
The average drill hole spacing was 20m.
Variogram model parameters were determined for most of the domains. Where there were
poorly informed domains and where variogram models were not produced recommended
variogram substitution was based on statistical similarity.

Any assumptions behind modelling of selective mining units.
No assumptions made

Any assumptions about correlation between variables.
No assumptions made

Description of how the geological interpretation was used to control the resource
estimates.
Only data form the same domain were used to make estimates.

Discussion of basis for using or not using grade cutting or capping.
Top-cuts were selected for each domain based on a visual inspection of the data using
histograms, log-transformed probability plots, percentile analysis and sensitivity analysis for
individual domains. Spatial location of the outliers was also taken into consideration for the
application of the grade caps. The sensitivity analysis involved analysing varying cap values,
to estimate the contribution of each sample to the overall metal content. Capping was
deemed necessary for majority of the domains.

The process of validation, the checking process used, the comparison of model data to
drill hole data, and use of reconciliation data if available.
Validation of the modelling parameters and processes of estimation included visual
inspections in section, plan and in 3D; and a comparison of an ID2 model vs the OK model.
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 tonnage basis.
Cut-off
parameters

The basis of the adopted cut-off grade(s) or quality parameters applied.
The cut-off grade 0.5 g/t gold is above the cut-off used for the low grade stockpiles calculated
for the Tomingley deposits 3km to the north. This considers likely mining costs and
metallurgical recovery for similar material.
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
theprocess of determining reasonableprospects for eventual economic extraction to
No mining factors were invoked into the San Antonio Resource estimation process.

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Criteria JORC Code explanation Commentary
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.
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 rigorous. Where this is the case, this should be
reported with an explanation of the basis of the metallurgical assumptions made.
The metallurgy of the nearby other Tomingley deposits is well studied. A preliminary
metallurgical study suggests San Antonio has similar metallurgical characteristics.
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.
The Tomingley Gold Operations has been operating since 2013 with an approved EIS plan
and environmental licences. A new EIS will need to be conducted over the San Antonio and
Roswell Deposits. San Antonio is positioned in highly modified agricultural land and a new
mining development will have little potential environmental impacts.
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.
Density determinations for the fresh rock were based on 787 measurements from diamond
core holes. A downhole density gamma probe which collects a density reading every 0.1m
down hole was used to calculate an average density for the alluvium and oxide material.
Surficial alluvium was given a density of 2.01t/m3(572 measurements), oxide material was
calculated a density of 2.25 t/m3(10,408 measurements), and fresh host rock was calculated
a density of 2.77t/m3(540 measurements).

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.
SG measurements completed on all material types – see above.

Discuss assumptions for bulk density estimates used in the evaluation process of the
different materials.
No assumptions made – SG determined and individual values applied to each material type
based on wireframed surfaces.
Classification
The basis for the classification of the Mineral Resources into varying confidence
categories.
Resource Model
Mineral Resources were classified as Inferred or Indicated to appropriately represent
confidence and risk with respect to data quality, drill hole spacing, geological and grade
continuity, mineralisation volumes, as well as metal distribution. There is no material
classified as Measured.

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Criteria
JORC Code explanation
Criteria
JORC Code explanation
Commentary
Indicated Mineral Resources were defined where a high level of geological confidence in
geometry, continuity, and grade, was demonstrated, and were identified as areas where:
- Drill spacing was averaging a nominal 20m, or where drilling was within 20m of the block
estimate; and
- Estimation quality is considered to be of high confidence in respect to low kriging variance.
Remaining estimated blocks made within the defined mineralisation domains in the first
search pass were classified as Inferred Resources (this included blocks in the less well-
informed and very poorly informed domains and all blocks in the unclassified domains).

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).
The use of RC drilling limits the amount of geological information that can be logged, and
boundaries of mineralisation zones cannot be precisely located.

Whether the result appropriately reflects the Competent Person’s view of the deposit.
The classification reflects the Competent Persons view of the deposit and its supporting data.
Audits
or
reviews

The results of any audits or reviews of Mineral Resource estimates.
Cube Consulting reviewed the gold grade estimation parameters including the domains
created by Alkane geologists.
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 or geostatistical
procedures 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.
No statistical or geostatistical method (non-linear or simulation) was used to quantify the
relative accuracy of the estimate within confidence limits. Accuracy of the estimate is
dependent on:
accuracy of the interpretation and geological domaining;
accuracy of the drill hole data (location and values);
orientation of search ellipses used; and
estimation parameters which are reflected in the variogram model used.

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 resources are Indicated and Inferred, being based on drill hole spacing and geological
continuity.
To ensure the resources have ‘reasonable prospects of eventual economic extraction’ the
resources have been restricted to all material above a gold cutoff grade of +0.5g/t Au.

These statements of relative accuracy and confidence of the estimate should be
compared with production data, where available.
There has not been any production from San Antonio.

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Alkane Resources Ltd – San Antonio Resource 16 February 2021