ROKEBY RESOURCES LIMITED - Capital/Financing Update 2021

Targeting a new generation of Tier-1 mineral discoveries in Peru and Australia

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ASX Announcement │ 3 May 2021 │ ASX: ICG

COPPER-BEARING VEIN SYSTEM DOUBLES IN WIDTH AT JEAN ELSON

Mapping confirms significant copper potential at NT project as key tenements are granted

Highlights

Jean Elson tenements now granted, clearing the way for major exploration activities to commence
Recent field trip identifies additional copper-quartz-iron veins at the key Ningaloo Prospect, Camel Creek
Previously reported 500m-wide zone of copper-bearing mineralised veins now approximately 1,000m wide

Inca Minerals Limited ( Inca or the Company ) is pleased to announce the granting of Exploration Licences ( EL ) EL32485 and EL32486 that make up its Jean Elson Project in the Northern Territory (Figure 1), together with positive outcomes from a recent exploration field trip conducted immediately following the successful AGES Conference in Alice Springs.

The Jean Elson Project is located 450km north-east of Alice Springs and, together with the Lorna May and Hay River Projects, makes up the Company’s East Arunta Group Project. It is located approximately 380km south of Inca’s Frewena Group Project in the emerging East Tennant region.

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Figure 1. The Jean Elson Project comprises two granted EL’s each containing the major prospect areas, Mt Cornish South, located on EL32485, and Camel Creek, located on EL32486. Both prospects were investigated during the recent field trip.

ASX: ICG │ Shares on issue 402.97m

Suite 1/16 Nicholson Road, Subiaco, WA 6008 │PO BOX 38, West Perth, WA 6872 Telephone: +61 (08) 6145 0300 │

Website: www.incaminerals.com.au │ ABN: 36 128 512 907

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Recent Mapping and Sampling Field Work

Immediately following the AGES conference and the inspection of diamond core from the NTGS-Minex CRC NDI drill-holes (see ASX announcements 22 April 2021 and 27 April 2021), the Company conducted a brief mapping and sampling program at the two main prospects at Jean Elson – Mt Cornish South and Camel Creek (and sub-prospect location Ningaloo).

A total of 45 rock-chip samples were collected, seven from Mt Cornish South and 38 from the general area of Camel Creek.

Camel Creek (Ningaloo Prospect)

As previously reported (ASX Announcement 23 October 2020), Ningaloo hosts a north-west to south-east ( NW-SE ) trending multi-phase quartz-haematite vein ( Qtz-Fe ) swarm up to 500m wide (Figure 2). This vein system hosts strong copper ( Cu ) mineralisation, including a maximum value of 10.3% Cu, that is associated with Qtz-Fe veins. The Cu-Qtz-Fe veins vary in true thickness from 1.0m to 5.0m. Prior to the field trip reported in this announcement, the vein swarm consisted of six individual veins and was considered open in all directions (hidden below sand cover).

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Figure 2. Rock-chip sample location and copper geochemistry of Ningaloo showing Inca’s previous reconnaissance samples (coloured triangles) and historically reported samples (coloured squares). A series of parallel veins with strong Cu grades are partially exposed within the dry bed of Camel Creek. At the time, the vein swarm defined a 500m mineralised corridor (solid yellow lines). Please refer to Appendix 2, Table 2 for selected assay results.

For the purposes of testing the across-strike extent of the NW-SE vein system, mapping focused on areas both upstream and downstream of the dry creek bed and flanking alluvial plains. Pleasingly, multiple new Cu-Qtz-Fe veins, Qtz-Fe veins and quartzvein alteration zones were identified in both directions.

Based on these finds, the width of the NW-SE vein system is now estimated be approximately 1,000m – double that of the previous estimate. Notwithstanding the fact that gravel beds of Camel Creek and alluvial sediments cover the veins system in all directions, the general decrease in vein float material in the creek upstream and downstream suggests that the vein system is not significantly broader than a kilometre.

The presence of a kilometre-wide vein swarm within which multiple Cu-Qtz-Fe veins contain significant levels of copper is a very pleasing result. To date, sampling has focused on these Cu-Qtz-Fe veins because of the occurrence of visual mineralisation.

The mineralised Qtz-Fe veins are generally poorly exposed and show high variability in terms of mineralogy, metal grade and morphology. Noted variations include thin (1m wide) zones of stockwork quartz and quartz-haematite veins/veinlets within altered granite, 1.0m-2.0m wide quartz-(haematite) veins, and more complex zoned veins varying from 1.0m-5.0m width.

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Complex veins generally consist of an inner zone (1-2m wide) of massive specular haematite that is flanked by banded quartzhaematite material grading towards quartz-rich in the outer zones.

The variation evident in veins suggests multiple hydrothermal fluid phases occurred with each phase having a different geochemistry (i.e. silica rich, Fe rich, silica-Fe-Cu rich, silica-Cu rich).

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K-Vein
J-Vein
No outcrop area
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Figure 3 Rockchip sample location and Cu geochemistry of Ningaloo showing Inca’s past (coloured triangles) and new reconnaissance samples (white triangles). A series of parallel veins with strong Cu grades are partially exposed within the dry bed of Camel Creek. The revised vein swarm width is approximately 1,000m wide (thick dashed lines). The J and K veins are highlighted.

Two large veins are worth singling out (Figure 3). The J-Vein varies in thickness from 1m to 5m and comprises a haematite-rich central suture with quartz-rich margins. The K-vein has a similar thickness, from 1m to 5m, but contains locally more complex internal zoning with lateral and longitudinal changes of quartz and haematite dominance. At least two haematite sutures are present at one location along the K-Vein.

The Cu-Qtz-Fe veins vary also in dip (angle into the ground), from approximately 60° dipping south (the J-Vein) to vertical (the K-Vein). This variability leads to the possibly of veins joining at depth.

As previously reported, the principal form of copper mineralisation occurring in exposes rocks at surface is supergene malachite (Figures 4 and 5), with lesser amounts of chrysocolla and azurite, that coats fractures and in-fills pore spaces.

Very fine (<0.5mm) chalcopyrite is also noted in several samples of both quartz-haematite and specular haematite material (Figure 4) .

Another objective of the mapping and sampling was to understand the vein variability and in particular the distribution of copper (and silver) within the large Qtz-Fe veins. To this end, K-Vein and J-Vein were channel sampled across the vein separating quartz dominant parts of the vein from iron-dominant parts, as well as from foot and hanging wall margins.

In the downstream direction, mapping identified additional malachite-bearing, Qtz-Fe veins within granites. This area also hosts numerous, small scale pods of altered to fresh mafic units. Zones of intense brecciation were also noted with increasingly stronger epidote alteration in addition to chlorite in the ‘downstream’ portion of Ningaloo. Fracture zones at times hosted latestage calcite, limonite, and Mn oxide coatings.

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Figure 4. Photo of rock chip sample JE0101 collected at Ningaloo (Figure 3 for location). It is quartz-haematite breccia, the quartz forms the clasts (white) and the haematite from the matrix (red-brown). Disseminated chalcopyrite and malachite occurs in the matrix. This one sample reveals two phases of hydrothermal activity, a first phase of milky white quartz and a second phase of haematite-copper.

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Figure 5. Photo of rock chip sample JE0107 collected at the location of a new Cu-Qtz-Fe vein at Ningaloo (Figure 3 for location). The sample comprises massive malachite and thin quartz veins in what was originally a granite.

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Several occurrences of chalcopyrite have now been noted at Ningaloo. JE0101 is a good example of an earlier stage quartz vein being later brecciated by haematite-rich fluids (Figure 4). Fine (0.5-1mm) blebs of chalcopyrite occur disseminated throughout and are partially weathered to haematite with associated malachite staining.

This sample confirms primary Cu-sulphides and also indicates rapid weathering of sulphides to haematite (a secondary form of haematite rather than primary form as that which occurs in the massive specular haematite veins at Ningaloo).

Sample ID	Easting (ms)	Northing (ms)	RL(ms als)	*Table 1*: Rock chip sample photo locations (Figures 4 and 5).
JE0101	688682	7460649	246
JE0107	688473	7460058	235

The assay results of this sampling will help determine the broader nature and style of mineralisation occurring at Ningaloo. The Company has already flagged the possibility of the Iron Ore Copper Gold ( IOCG ) association, for reasons relating to the geophysical signature and the Fe-rich quality of the Cu-bearing veins.

However, the Cu-Qtz-Fe vein swarm is also reminiscent of a Winu-style of copper deposit. Winu consists of a system of subvertical, stacked multi-generation hydrothermal copper-silver-gold veins and breccias. The vein swarm at Ningaloo has many of these traits.

Mt Cornish South Prospect

A single-day reconnaissance was undertaken at Mt Cornish South covering the 3.5km of prospect strike that was not visited during the 2020 field trip (the 2020 field trip assessed the western 1km portion of MCS). A total of seven rock chip samples were taken in areas not previously walked by Inca, with a focus on sampling of rock types not seen during the 2020 trip. Mapping and sampling was of a preliminary nature to obtain a general understanding of the entire Qtz-Fe breccia system.

Mt Cornish South is a very large (c. 5km E-W strike) prospect that consists of a fault disjointed ridge standing above relatively subdued topography. The topographic ridge largely consists of consists of hydrothermally altered granite, ferruginous sandstones, Fe breccias, felsic breccias, quartz veins, quartz stockwork zones, massive Fe-rich zones, and metasedimentary units. The pervasive nature of the hydrothermal quartz-Fe oxide alteration and vein-forming events is now doubt responsible for the formation of this ridge (resulting from increased resistance to erosion).

As previously reported, historical sampling at Mt Cornish South reports peak rock-chip results for Cu-uranium ( U ) and Fe mineralisation with elevated levels of silver ( Ag ), lead ( Pb ), zinc ( Zn ), molybdenum ( Mo ), nickel ( Ni ), and cobalt ( Co ).

The ridge partially forms a ring around a regional gravity high ridge with the northern and eastern topographic highs being qtzhem veined and some of the southern topographic highs older granites. All topographic highs truncate to the west.

The geochemical expression of the large Qtz-Fe vein-breccia system has clear IOCG affinity. Plus, its long-distance regional projection along strike from the Camel Creek Prospect makes Mt Cornish South, despite its lower rock chip assay values, of major exploration interest.

A wide array of vein styles is noted that includes vein/veinlets, stockworking, breccias, and pervasive silica and/or Fe-oxide flooding. Multiple phases of hydrothermal activity are noted, each phase differing in Qtz-Fe and metal content. This reflects variations in hydrothermal temperatures and pressures over a sustained period.

Reconnaissance work has confirmed that Mount Cornish South hosts a very large hydrothermal-style system that is moderately well exposed at surface but best expressed in higher topographical features. Sampling by Inca has corroborated historical sampling and indicates that the Prospect warrants additional exploration. This is likely best done through geophysical surveying to assess sub-surface features in order to define drill targets to evaluate the metal endowment of the area.

Next Steps

The 2020 and 2021 field trips (the latter the subject of this announcement) have confirmed the exploration potential of the Jean Elson Project, which is highly prospective for IOCG, orogenic gold and “Winu”-style mineralisation.

Inca is committed to a fast-paced exploration program at this project, without compromising exploration standards. The Company has already engaged a firm for the purposes of conducting a project-wide airborne magnetic and radiometric survey (AMAGRAD) and has also applied for a NTG co-funding grant this for program.

The AMAGRAD program is scheduled to commence in the second half of 2021.

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Investor inquiries - Ross Brown, Managing Director - Inca Minerals - 0407 242 810 Media Inquiries/Investor Relations - Nicholas Read, Read Corporate - 0419 929 046

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Ross Brown
Managing Director
Inca Minerals Limited
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Competent Person’s Statements

The information in this report that relates to exploration activities for the Jean Elson Project, located in the Northern Territory, is based on information compiled by Mr Ross Brown BSc (Hons), MAusIMM, SEG, MAICD Managing Director, Inca Minerals Limited, who is a Member of the Australasian Institute of Mining and Metallurgy; and by Mr Robert Heaslop BSc (Hons), MAusIMM, Consultant Geologist for Inca Minerals Limited, who is a Member of the Australasian Institute of Mining and Metallurgy. Both Mr Brown and Mr Heaslop have sufficient experience, which is relevant to the exploration activities, style of mineralisation and types of deposits under consideration, and to the activity which has been undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr Brown, who is a fulltime employee of Inca Minerals Limited, and Mr Heaslop both consent to the report being issued in the form and context in which it appears.

Appendix 1: Key Assay Results from the Prior 2020 Sampling Programs at Ningaloo Prospect

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Table 2: Peak rockchip sample results from Ningaloo show high grade Cu, variable Fe, and elevated Au-Ag.

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Appendix 2: Selected Key Words Used in this Announcement (order of appearance and cross reference)

Reconnaissance
Sampling
Rockchip Sampling
Ore-forming Minerals
Gangue Minerals
IOCG (Deposit)
Deposit
Chalcopyrite
Malachite
Fe-oxides
Mn-oxides
Haematite
Specularite
Limonite
Granite/granitic
Footwall
Hangingwall
Limestone
Calcrete
Silcrete
Geochemistry (-ical)
Alteration
Propylitic alteration
Phyllic Alteration
Potassic alteration
Breccia
Clast
Matrix
Vein(s)
Veinlet(s)
Stockwork
Boxwork (texture)
Disseminated
Massive
Epidote
Quartz
Magnetics
Gravity

Refers to very early-stage, in some cases, first-pass, [often rockchip] sampling recording, location, rock type
structure,alteration_and_mineralisation.
An exploration method to obtain_geochemical_ data from rock outcrop. This program type is often deployed as part
of_reconnaissance_exploration [mapping and sampling] but may also be deployed over targets that are relatively
well defined.
Minerals which are economically desirable, as contrasted to_Gangue Minerals.
Valueless minerals in ore.
A type of _deposit_containing _ore-forming minerals occurring as disseminations_and _veinlets in a large volume of rock.
The rock is typically iron rich (a distinction from porphyry deposits). IOCG deposits_are economically very significant.
A [mineral]_deposit is a naturally occurring accumulation or concentration of metals or minerals of sufficient size
and concentration that might, under favourable circumstances, have economic value (Geoscience Australia). It is
not a defined term in the JORC Code 2012 for Australasian Reporting of Exploration Results, Mineral Resources and
Ore Reserves (JORC 2012).
Copper iron sulphide with the chemical formula CuFeS2with 34.63% Cu by mol. weight.
A hydrated copper oxide with a chemical formula: Cu2(CO3)(OH)2; 57.48% Cu mol weight.
A group of oxide minerals containing iron (Fe), including but not limited to_haematite_, limonite and goethite.
A group of oxide minerals containing manganese (Mn), including but not limited to pyrolusite, franklinite, jacobsite.
An iron oxide reddish-brown to silvery grey coloured group pf minerals with a general formula of Fe2O3.
A variety of haematite that is metallic in colouring.
A hydrated iron oxidewith a chemical formula: FeO(OH).nH2O
An intrusive_rock in which quartz constitutes 1- to 50% of the felsic component and in which the alkali feldspar/total
feldspar ratio is generally restricted to 65% to 90%.
The lower or underside wall of an inclined vein, fault, zone of mineralisation or other geologic structure.
The upper or overhanging wall of an inclined vein, fault, zone of mineralisation or other geologic structure.
A calcium carbonate sedimentary rock typically formed by ancient coral reefs.
A sedimentary rock, a hardened natural cement of calcium carbonate that binds other materials—such as gravel,
sand, clay, and silt. It occurs worldwide in arid or semiarid regions.
An indurated (resists crumbling or powdering) soil duricrust formed when surface sand and gravel are cemented by
dissolved silica. The formation of silcrete is similar to that of_calcrete, formed by calcium carbonate, and ferricrete,
formed by iron oxide. It is a hard and resistant material and id common in the arid and semiarid regions.
The study of the distribution and amounts of the chemical elements in minerals, ores, rocks, soils, water and the
atmosphere.Geochemical sampling programs may include_stream sampling_,soil sampling,rock chip sampling.
A process that involves the_alteration_ of (change to) a rock, mineral or_mineralisation_by processes involving, but
not limited to, the presence of hydrothermal fluids.
Alteration typically associated with hydrothermal activities in which_epidote_,chlorite and_calcite_ are produced.
Alteration typically associated with hydrothermal activities in which_quartz_, sericite and_pyrite_are produced.
Or K-Feldspar alteration that is characterised by the formation of new K-feldspar and/or biotite minerals. It typically
represents the highest temperature form of alteration within porphyry deposits, forming in the core of the system.
Broken or fragmented rock. Breccia veins which are common at Riqueza, are narrow fissures containing numerous
rock fragments. The rock fragments are called clasts and the space around the clasts is called the matrix. Often the
matrix in the breccia veins at Riqueza contains the ore-forming minerals.
The broken or fragmented, generally coarse component of a breccia.
The fine component of a breccia, occurring between the clasts.
A tabular or sheet-like form of mineralisation, often resulting from in-filling a vertical or near-vertical fracture. They
often cut across country rock.
A small and narrow mineral filling of a fracture in country rock that is tabular or sheet-like in shape. Veinlets are
narrow versions of veins.
A mineral deposit in the form of a profusion of_veinlets_ diffused in the country rock.
Said of a rock fabric that comprises empty cubic/near-cubic (“boxes”) that are spaces created by the weathering
and removal of crystal sulphides.
Descriptor of_mineralisation_ said to be fine grained and generally evenly distributed.
Descriptor of_mineralisation_ said to comprise more than 20% of the rock.
A common secondary mineral that is often a product of_hydrothermal_ alteration. In the field_epidote_ is often apple
green in colour.
One of the most common minerals on Earth.Quartz_is often a product of_hydrothermal alteration.
A measurement of the intensity of the earth’s magnetic field caused by the contrasting content of rock-forming
magnetic minerals in the Earth’s crust. This allows sub-surface mapping of geology, including structures.An airborne
survey is flown either by plane or helicopter with the magnetometer kept at a constant height above the surface.
A measurement of a rock’s, zone of mineralisation’s, etc…gravity (or density).

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Appendix 3: ASIC Compliancy Table

The following information is provided to comply with the JORC Code (2012) exploration reporting requirements.

SECTION 1 SAMPLING TECHNIQUES AND DATA

Criteria: Sampling techniques

JORC CODE Explanation

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 hand-held XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.

Company Commentary

This announcement refers to reconnaissance mapping and sampling field work conducted at the Jean Elson Project. Forty five rock chip samples were taken. Rock samples were collected that were considered representative of the source material and were recorded as either in situ or float material. This announcement also refers to exploration results conducted by Inca and by previous parties and recorded in the Northern Territory Mines Department databank, assessed and reviewed by the Company. Strong correlation is seen between the Company’s assay results as those of previous explorers.

Two rock chip sample rock specimen photos are included in this announcement. However, no new assay results are referred to in this announcement.

JORC CODE Explanation

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

Company Commentary

JORC CODE Explanation

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

Company Commentary

No drilling results are referred to in this announcement. JORC CODE Explanation

If non-core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry. Company Commentary

No drilling results are referred to in this announcement. JORC CODE Explanation For all drill sample types, the nature, quality and appropriateness of the sample preparation technique. Company Commentary No drilling results are referred to in this announcement. JORC CODE Explanation Quality control procedures adopted for all sub-sampling stages to maximise “representivity” of samples. Company Commentary No drilling results are referred to in this announcement.

JORC CODE Explanation

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.

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Company Commentary

The samples taken from mineralised outcrop are considered representative of such mineralisation and hydrothermal alteration outcropping at the various locations mapped and sampled. Approximately 2kg of sample was taken from each sample location. The historic sample assay results referred to in this announcement were generated by a previous exploration company. The sampling distribution appears controlled by the limit of exposed rock in a dry creek bed. To this extent, the sampling technique appears representative of the limited rock exposure in the creek bed. Additionally, strong correlation between the Company’s assay results and those of previous explorers indicate representative sampling has been achieved.

JORC CODE Explanation

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

Company Commentary

The average rockchip sample size of approximately 2kg is considered appropriate.

Criteria: Quality of assay data and laboratory tests

JORC CODE Explanation

Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.

Company Commentary

SECTION 2 REPORTING OF EXPLORATION RESULTS

Criteria: Mineral tenement and land tenure status

JORC CODE Explanation

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.

Company Commentary

Tenement Type: Two Northern Territory Exploration Licences (EL): EL 32485 and EL32486 applications.

Ownership: The Company has the right to earn 100% of EL 32485 & EL32486 with a residual 1.5% NSR payable to MRG Resources Pty Ltd ( MRG ), through an executed Joint Venture and Royalty Agreement (JVRA) with MRG.

JORC CODE Explanation

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

JORC CODE Explanation

A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:

Easting and northing of the drill hole collar
Elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar.
Dip and azimuth of the hole.
Down hole length and interception depth.
Hole length.

Company 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.

Company Commentary

This announcement refers to mapping and sampling field work conducted at the Jean Elson Project. Forty five rock chip samples were taken. Visible mineralisation and alteration is discussed in this announcement. Two photos (with scale) are provided that shows the nature of the mineralisation, among other parameters. The location of the samples and photos are provided in a plan. No new sample assay results are included in this announcement.

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AI assistant

ROKEBY RESOURCES LIMITED — Capital/Financing Update 2021

65707_rns_2021-05-02_08a627ff-5342-48e4-959e-1705af6b1d88.pdf

ASX Announcement │ 3 May 2021 │ ASX: ICG

COPPER-BEARING VEIN SYSTEM DOUBLES IN WIDTH AT JEAN ELSON

Mapping confirms significant copper potential at NT project as key tenements are granted

Highlights

Recent Mapping and Sampling Field Work

Camel Creek (Ningaloo Prospect)

Mt Cornish South Prospect

Next Steps

Competent Person’s Statements

Appendix 1: Key Assay Results from the Prior 2020 Sampling Programs at Ningaloo Prospect

Appendix 2: Selected Key Words Used in this Announcement (order of appearance and cross reference)

Appendix 3: ASIC Compliancy Table

SECTION 1 SAMPLING TECHNIQUES AND DATA

Criteria: Sampling techniques

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

Criteria: Drilling techniques

JORC CODE Explanation

Company Commentary

Criteria: Drill sample recovery

JORC CODE Explanation

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JORC CODE Explanation

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JORC CODE Explanation

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Criteria: Logging

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

Criteria: Sub-sampling techniques and sample preparation

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

Criteria: Quality of assay data and laboratory tests

JORC CODE Explanation

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JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

Criteria: Verification of sampling and assaying

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

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JORC CODE Explanation

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JORC CODE Explanation

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Criteria: Location of data points

JORC CODE Explanation

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JORC CODE Explanation

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JORC CODE Explanation

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Criteria: Data spacing and distribution

JORC CODE Explanation

Data spacing for reporting of Exploration Results.

Company Commentary

JORC CODE Explanation

Company Commentary

JORC CODE Explanation

Company Commentary

Criteria: Orientation of data in relation to geological structure

JORC CODE Explanation

ROKEBY RESOURCES LIMITED Capital/Financing Update 2021