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Porphyry system extended to surface and depth at Trundle Park Assay results for TRDD014W1 return significant higher gold grade skarn intervals and broad intervals of porphyry style intrusions at the Trundle Park prospect;

Drill Results

Porphyry system extended to surface and

depth at Trundle Park

Assay results for TRDD014W1 return significant higher gold grade skarn intervals and broad

intervals of porphyry style intrusions at the Trundle Park prospect;

42m

@ 0.42 g/t gold and 0.12% copper from

358m

, including:

10m

@ 1.13 g/t gold and 0.32% copper from

382m

48m

@ 0.19 g/t gold and 0.03% copper from

458m

122m

@ 0.16g/t gold and 0.03% copper from

596m

10m

@ 0.21g/t gold and 0.06% copper from

750m

16m

@ 0.11g/t gold and 0.07% copper from

860m

For the first time at the Trundle Park prospect most recently completed hole TRDD028

intersected broad porphyry style intrusions from near surface (to

467m

), with the targeted

deeper intrusive body also intersected (assay results pending);

Assay results for TRDD022 (

162m

@ 0.24 g/t gold and 0.04% copper, including

18m

@ 0.75

g/t gold and 0.09% copper), TRDD014/W1 and visual interpretation of TRDD028 provided

further confidence of proximity to the core of a large porphyry intrusive system, vectors for

follow up drilling and support the working model of a vertically extensive mineralized intrusive

system that has both open pit and underground target potential;

Hole TRDD029 has commenced testing nearer surface intrusive potential, and also western and

southern strike for both skarn and porphyry type intrusion mineralization at depth.

MELBOURNE, Australia

,

Dec. 7, 2021

/CNW/ - Kincora Copper Limited (the Company, Kincora)

(TSXV: KCC) (ASX: KCC) is pleased to provide an exploration update from ongoing drilling at

Trundle Park prospect situated at the brownfield Trundle project, located in the Macquarie Arc of the

Lachlan Fold Belt (LFB) in NSW,

Australia

.

John Holliday

, Technical Committee chair, and

Peter Leaman

, VP of Exploration, noted:

"The occurrence of the targeted porphyry intrusive system from surface to depth in

TRDD028 (assay results pending) provides a new nearer surface and potentially open pit

target in addition to the known deeper parts of the system at the Trundle Park prospect.

This is a very positive development and consistent with a number of the vertically extensive

intrusive deposits at Northparkes that extend from nearer surface to depth.

Assay results for TRDD014W1 confirmed our initial visual interpretations with broad

intrusive intervals and higher-grade skarn zones. The widths of mineralised intervals

returned in TRRD014W1 and visual intrusions in TRDD028 are very encouraging.

We continue to see the right rocks and alteration in what is an increasingly large intrusive

system. The recently commenced hole TRDD029 will test the nearer surface intrusive, and

southern and western depth potential, with the west and south still open for further follow up

drilling as we seek to intersect the higher grade and inner potassic core of the intrusive

system."

Figure 1:

Assay results pending for both the Trundle and Fairholme projects

Favourable locations of the key porphyry belts of the Macquarie Arc

Advance stage exploration projects with demonstrated large scale mineralised systems

Hallmarks to neighbouring world-class deposits

Figure 2:

Trundle is the only brownfield porphyry project held by a listed junior in the

Lachlan Fold Belt (LFB), located within Northparkes Igneous Complex which already hosts

the 2

nd

largest porphyry mine in

Australia

(endowment 5.5Moz Au & 4.5Mt

Cu

1

)

Large geochemical footprints with a cluster of concealed intrusive deposits at Northparkes

1

Bespoke March 2020 report by Richard Schodde, MinEx Consulting, for Kincora

Trundle Park prospect

Recent drilling at the Trundle Park prospect has confirmed a significant area and multiple intrusive

porphyry system with a mineralised zone emerging. The latest hole (TRDD028) now also

demonstrates nearer surface potential for a multiple intrusive system (assay results pending).

These results provided further confidence of proximity to the core of a porphyry intrusive system

such as the multiple deposits at the neighbouring Northparkes mine or at Cadia-Ridgeway – where

Figure 1 outlines our target model - and supports the working geological concept of a vertically

extensive mineralized intrusive system that has both open pit and underground target potential.

Figure 3:

The clusters of deposits at the neighbouring Northparkes mine and at Cadia-

Ridgeway exhibit multiple intrusive systems and an alteration, lithology and mineralised

setting not dissimilar to the Trundle Park prospect around discrete mineralized cores of only

hundreds of metres width that are vertically extensive

Assay results have been received for TRDD014W1 that intersected significant higher gold grade

skarn intervals and broad intervals of porphyry style intrusions. Highlights include:

42m

@ 0.42 g/t gold and 0.12% copper from

358m

, including:

10m

@ 1.13 g/t gold and 0.32% copper from

382m

48m

@ 0.19 g/t gold and 0.03% copper from

458m

122m

@ 0.16g/t gold and 0.03% copper from

596m

10m

@ 0.21g/t gold and 0.06% copper from

750m

16m

@ 0.11g/t gold and 0.07% copper from

860m

Further details and significant intervals are included in Table 1 and see Figure 4 (c) for a cross

section.

This hole was a wedge drilling off previous hole TRDD014, seeking to extend the original hole to

greater depth and provide coverage towards TRDD022. TRDD014W1 has confirmed, expanded and

returned higher grade skarn intervals, and extended the intrusive systems returned in both TRDD014

and TRDD022 to depth and on strike.

Assay results for TRDD014W1 confirmed our initial visual interpretations with broad intrusive

intervals and higher-grade skarn zones, and the widths of and multiple intervals returned are very

encouraging.

The lithologies, alteration, veining, mineral tenor and structural interpretations have provided further

confidence of a proximal environment to the targeted causative intrusion at the Trundle Park

prospect, as well as vectors for follow up drilling.

Initial follow up hole TRDD028 was drilled parallel and west of TRDD014/W1, and further expanded

the deeper intrusive system to the west but importantly also intersected a broad and nearest to

surface intrusive system identified to date at the prospect.

Figure 4:

Recently completed TRDD028 has intersected broad intervals of the targeted

intrusive system nearer surface than previously recognized at the Trundle Park prospect

and expanded the system to depth and the west of previous drilling.

Recently commenced follow up hole TRDD029 is further testing the nearer surface and deeper

intrusive system to the west and south.

(a) Plan view of Trundle Park prospect and planned hole TRDD029 - see Figure 3 (b) for section

(b) Working Leapfrog model and design of hole TRDD029 – Trundle Park prospect section

(Section line through Figure 3 (a). Length ~900m and width ~1000m, ~400m to the NNE with

only the trace of TRDD029 and TRDD017 to the SSE)

(c) Insert with mineralised intervals and illustration of strike/down dip target of TRDD029, noting the

distance from TRDD029 to TRDD028 is ~150m and

95m

west to TRDD014/17

(Length ~700m and width ~420m)

Table 1:

Trundle Park target hole TRDD014W1 - Significant broad mineralized intervals

Porphyry gold and copper intercepts are calculated using a lower cut of 0.10g/t and 0.05%

respectively.

Internal dilution is below cut off; and, * Dilutions related with Core loss

From initial logging of TRDD028 notable zones include (with assay results pending):

1

.

Upper intrusions (surface –

467m

)

: a weathered monzodiorite intrusion was intersected from

surface to

39m

down-hole followed by a short interval of volcanoclastic sandstones and

siltstones to

69m

. A broad upper interval of monzodiorite was then intersected to

467.3m

, which

was in-turn intruded in multiple zones by red (interpreted potassic altered) monzonite dyke-like

bodies (<2 and >

10m

wide). Quartz-sulphide veins were also observed in the monzonite dykes.

See Figure 6 (a) and (b) for examples of core from this zone.

2

.

Skarn altered volcanoclastic rocks (467 –

741m

)

: a volcanoclastic dominated sequence

(mainly grey sandstones and siltstones) was intersected with multiple intervals of zoned skarn

alteration spaced approximately

100m

apart and occurring close by to intrusion contacts. In the

upper (retrograde) skarn two cavities were observed comprising green garnet-carbonate-

epidote-magnetite-pyrite and minor chalcopyrite and trace bornite – see Figure 6 (c).

3

.

Lower intrusions (741 –

868.3m

)

: A broad lower interval of monzodiorite was intersected,

with similarities to those observed in TRDD014W1. Comparatively, to the upper zone, this larger

monzodiorite intrusion is cut by two zones (smaller) of red monzonite intrusions. See Figure 6

(d).

4

.

Thrust fault with a slice of volcanoclastic sequence then conglomerate (868 – 879m)

: the

interpreted regionally significant westerly dipping thrust fault (the Tullamore thrust) was

intersected in close proximity to the forecast depth at

870m

and defined by sheared red clays

to

873m

down-hole, followed by a preserved slice of a sheared volcanoclastic sequence +/-

pyrite intersected from 873-

878.8m

. A dark red conglomerate unit with fragments of grits, shale

and rounded pebble sized felsic intrusive rock clasts was observed between 878.8-

879.4m

to

end of hole and is interpreted to be similar to those observed at the end of in hole TRDD015

and considered to be Devonian aged.

See Figure 6 for examples of the described rock types in TRDD028 and interpreted section for

TRDD028 below.

Figure 5:

The occurrence of the targeted preserved porphyry intrusive systems from surface

to depth in TRDD028 (assay results pending) provides a new nearer surface and potentially

open pit target in addition to the ongoing deeper parts of the system at the Trundle Park

prospect

Key observations include: the multiple phase, multiple intrusive setting returned in TRDD022 (

162m

@ 0.24 g/t gold and 0.04% copper, including

18m

@ 0.75 g/t gold and 0.09% copper), TRDD026

and TRDD014/W1, endoskarn intersected in TRDD014W1, TRDD028 coupled with returned mineral

tenor in TRDD022, TRDD014/W1 and TRDD001 (

21.1m

@ 0.25 g/t gold and 0.03% copper to

EOH), and provides indicators of a proximal environment to the targeted core of an intrusive

porphyry system and vectors for follow up drill testing.

A recently commenced hole (TRDD029) is an offset scissor hole stepping out to the west of

TRDD028 drilling towards the south-southeast testing for nearer surface porphyry type intrusive

potential, and the western and southern strike coverage for both skarn and porphyry mineralization

at depth.

The west and south remain open for further follow up drilling within an identified mineralized corridor.

The Company is also reviewing previous air-core drilling that have returned shallow intrusions

(generally at less than

20m

vertical depth from surface), and may warrant infill coverage to assist

advance a shallow, open pit intrusive system target.

Figure 6:

Examples of the rock types in hole TRDD028 at the Trundle Park prospect

(a) Monzodiorite – Upper interval example from

389m

with increasing K-spar (interpreted potassic)

alteration (reddening) along quartz-carbonate-pyrite veins (inset photo).

(b) Red monzonite (interpreted potassic alteration) cut by quartz-pyrite veins, then in turn by

carbonate veins (inset @

402.8m

).

(c) Basaltic andesite lava host rock with a cavity filled by retrograde skarn comprising green garnet-

carbonate-epidote-magnetite-pyrite, minor chalcopyrite and trace bornite (purple).

(d) Monzodiorite (grey-brown) – Lower interval example from

793m

with increasing dykes of

(interpreted potassic altered) monzonite (red).

Photos of selected intervals which are not representative of the mineralization hosted on the whole

property or Trundle Park prospect but are of the alteration and lithology's intersected in the

mineralized zones in these sections of drill holes TRDD028, and current working geological

interpretation presented in Figure 3. There is insufficient drilling data to date to demonstrate

continuity of mineralized domains and determine the relationship between mineralization widths

and intercept lengths. True widths are not known.

Trundle Project background

The Trundle Project includes one single license covering 167km

2

and was secured by Kincora in the

March 2020

agreement with RareX Limited ("REE" on the ASX). Kincora is the operator, holds a

65% interest in the Trundle Project and is the sole funder until a positive scoping study is delivered at

which time a fund or dilute joint venture will be formed.

This announcement has been authorised for release by the Board of Kincora Copper Limited

(ARBN 645 457 763)

Forward-Looking Statements

Certain information regarding Kincora contained herein may constitute forward-looking statements

within the meaning of applicable securities laws. Forward-looking statements may include estimates,

plans, expectations, opinions, forecasts, projections, guidance or other statements that are not

statements of fact. Although Kincora believes that the expectations reflected in such forward-looking

statements are reasonable, it can give no assurance that such expectations will prove to have been

correct. Kincora cautions that actual performance will be affected by a number of factors, most of

which are beyond its control, and that future events and results may vary substantially from what

Kincora currently foresees. Factors that could cause actual results to differ materially from those in

forward-looking statements include market prices, exploitation and exploration results, continued

availability of capital and financing and general economic, market or business conditions. The

forward-looking statements are expressly qualified in their entirety by this cautionary statement. The

information contained herein is stated as of the current date and is subject to change after that date.

Kincora does not assume the obligation to revise or update these forward-looking statements,

except as may be required under applicable securities laws.

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is

defined in the policies of the TSX Venture Exchange) or the Australian Securities Exchange

accepts responsibility for the adequacy or accuracy of this release.

Table 2:

Trundle project - Collar Information

For further details, including QAQC procedures, please refer to the following press releases:

1.

July 6, 2020 - Kincora announces high-grade gold-copper results from first hole at Trundle

2.

July 23, 2020 - Kincora reports further strong encouragement at Trundle

3.

September 3, 2020 - Kincora provides update on expanded drilling program at Trundle

4.

November 30, 2020 - Kincora intersects broad mineralized zones at Trundle

5.

January 20, 2021 - Kincora intersects further shallow mineralization at Trundle

6.

March 2021 - Independent Technical Report for the ASX prospectus

7.

April 22, 2021 - Exploration Update

8.

July 8, 2021 - Exploration portfolio drilling update

9.

August 17 2021 - Significant gold-bearing intervals at Trundle Park

10.

December 2021 - Porphyry system extended to surface and depth at Trundle Park

Table 3:

Trundle Park target hole 23 - Significant broad mineralized intervals

Table 4:

Trundle Park target hole 26 - Significant broad mineralized intervals

Porphyry gold and copper intercepts are calculated using a lower cut of 0.10g/t and 0.05%

respectively.

Internal dilution is below cut off; and, * Dilutions related with Core loss

Drilling, Assaying, Logging and QA/QC Procedures

Sampling and QA/QC procedures are carried out by Kincora Copper Limited, and its contractors,

using the Company's protocols as per industry best practise.

All samples have been assayed at ALS Minerals Laboratories, delivered to Orange, NSW,

Australia

.

In addition to internal checks by ALS, the Company incorporates a QA/QC sample protocol utilizing

prepared standards and blanks for 5% of all assayed samples.

Diamond drilling was undertaken by DrillIt Consulting Pty Ltd, from Parkes, under the supervision of

our field geologists. All drill core was logged to best industry standard by well-trained geologists and

Kincora's drill core sampling protocol consisted a collection of samples over all of the logged core.

Sample interval selection was based on geological controls or mineralization or metre intervals,

and/or guidance from the Technical Committee provided subsequent to daily drill and logging

reports. Sample intervals are cut by the Company and delivered by the Company direct to ALS.

All reported assay results are performed by ALS and widths reported are drill core lengths. There is

insufficient drilling data to date to demonstrate continuity of mineralized domains and determine the

relationship between mineralization widths and intercept lengths.

True widths are not known at this stage.

Significant mineralised intervals for drilling at the Trundle project are reported based upon two

different cut off grade criteria:

Interpreted near surface skarn gold and copper intercepts are calculated using a lower cut of

0.20g/t and 0.10% respectively; and,

Porphyry intrusion system gold and copper intercepts are calculated using a lower cut of 0.10g/t

and 0.05% respectively.

Significant mineralised intervals are reported with dilution on the basis of:

Internal dilution is below the aforementioned respective cut off's; and,

Dilutions related with core loss as flagged by a "*".

The following assay techniques have been adopted for drilling at the Trundle project:

Gold: Au-AA24 (Fire assay), reported.

Multiple elements: ME-ICP61 (4 acid digestion with ICP-AES analysis for 33 elements) and ME-

MS61 (4 acid digestion with ICP-AES & ICP-MS analysis for 48 elements), the latter report for

TRDD001 and former reported for holes TRDD002-TRDD022.

Copper oxides and selected intervals with native copper: ME-ICP44 (Aqua regia digestion with

ICP-AES analysis) has been assayed, but not reported.

Assay results >10g/t gold and/or 1% copper are re-assayed.

Qualified Person

The scientific and technical information in this news release was prepared in accordance with the

standards of the Canadian Institute of Mining, Metallurgy and Petroleum and National Instrument 43-

101 – Standards of Disclosure for Mineral Projects ("NI 43-101") and was reviewed, verified and

compiled by Kincora's geological staff under the supervision of

Paul Cromie

(BSc Hons. M.Sc.

Economic Geology, PhD, member of the Australian Institute of Mining and Metallurgy and Society of

Economic Geologists), Exploration Manager Australia, who is the Qualified Persons for the purpose

of NI 43-101.

JORC Competent Person Statement

Information in this report that relates to Exploration Results, Mineral Resources or Ore Reserves

has been reviewed and approved by Mr.

Paul Cromie

, a Qualified Person under the definition

established by JORC and have sufficient experience which is relevant to the style of mineralization

and type of deposit under consideration and to the activity being 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'.

Paul Cromie

(BSc Hons. M.Sc. Economic Geology, PhD, member of the Australian Institute of

Mining and Metallurgy and Society of Economic Geologists), is Exploration Manager Australia for the

Company.

Mr.

Paul Cromie

consents to the inclusion in this report of the matters based on his information in the

form and context in which it appears.

The review and verification process for the information disclosed herein for the Trundle, Fairholme

and Nyngan projects have included the receipt of all material exploration data, results and sampling

procedures of previous operators and review of such information by Kincora's geological staff using

standard verification procedures.

JORC TABLE 1

Section 1 Sampling Techniques and Data

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

Criteria

JORC Code explanation

Commentary

Sampling

techniques

Nature and quality of sampling (e.g. cut channels, random chips, or specific

specialised industry standard measurement tools appropriate to the minerals under

investigation, such as down hole gamma sondes, or handheld XRF instruments,

etc.). These examples should not be taken as limiting the broad meaning of sampling.

Include reference to measures taken to ensure sample representivity and the

appropriate calibration of any measurement tools or systems used.

Aspects of the determination of mineralisation that are Material to the Public Report.

In cases where 'industry standard' work has been done this would be relatively

simple (e.g. 'reverse circulation drilling was used to obtain 1 m samples from which

3 kg was pulverised to produce a 30 g charge for fire assay'). In other cases more

explanation may be required, such as where there is coarse gold that has inherent

sampling problems. Unusual commodities or mineralisation types (eg submarine

nodules) may warrant disclosure of detailed information

Kincora Copper Limited is the operator of the Trundle

Project, with drilling using diamond coring methods by DrillIt

Consulting Pty Ltd, from which sub-samples were taken

over 2 m intervals and pulverised to produce suitable

aliquots for fire assay and ICP-MS.

Diamond drilling was used to obtain orientated samples

from the ground, which was then structurally,

geotechnically and geologically logged.

Sample interval selection was based on geological controls

and mineralization.

Sampling was completed to industry standards with 1⁄4

core for PQ and HQ diameter diamond core and 1⁄2 core

for NQ diameter diamond core sent to the lab for each

sample interval.

Samples were assayed via the following methods:

Gold: Au-AA24 (Fire assay)

Multiple elements: ME-ICP61 (4 acid digestion with

ICP-AES analysis for 33 elements) and ME-MS61

(4 acid digestion with ICP-AES & ICP-MS analysis

for 48 elements)

Copper oxides and selected intervals with native

copper: ME-ICP44 (Aqua regia digestion with ICP-

AES analysis) has been assayed, but not reported

Assay results >10g/t gold and/or 1% copper are

re-assayed

Historic sampling on other projects included soils, rock

chips and drilling (aircore, RAB, RC and diamond core).

Drilling

techniques

Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger,

Bangka, sonic, etc) and details (e.g. core diameter, triple or standard tube, depth of

diamond tails, face-sampling bit or other type, whether core is oriented and if so, by

what method, etc.).

Drilling by Kincora at Trundle used diamond core drilling

with PQ, HQ and NQ diameter core depending on drilling

depth.

All Kincora core was oriented using a Reflex ACE

electronic tool.

Historic drilling on Kincora projects used a variety of

methods including aircore, rotary air blast, reverse

circulation, and diamond core. Methods are clearly stated in

the body of the previous reports with any historic

exploration results.

Drill sample

recovery

Method of recording and assessing core and chip sample recoveries and results

assessed.

Measures taken to maximise sample recovery and ensure representative nature of

the samples.

Whether a relationship exists between sample recovery and grade and whether

sample bias may have occurred due to preferential loss/gain of fine/coarse material.

Drill Core recovery was logged.

Diamond drill core recoveries are contained in the body of

the announcement.

Core recoveries were recorded by measuring the total

length of recovered core expressed as a proportion of the

drilled run length.

Core recoveries for most of Kincora's drilling were in

average over 96.7%, with two holes averaging 85.6%

Poor recovery zones are generally associated with later

fault zones and the upper oxidised parts of drill holes.

There is no relationship between core recoveries and

grades.

Logging

Whether core and chip samples have been geologically and geotechnically logged to

a level of detail to support appropriate Mineral Resource estimation, mining studies

and metallurgical studies.

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

etc.) photography.

The total length and percentage of the relevant intersections logged.

All Kincora holes are geologically logged for their entire

length including lithology, alteration, mineralisation

(sulphides and oxides), veining and structure.

Logging is mostly qualitative in nature, with some visual

estimation of mineral proportions that is semi-quantitative.

Measurements are taken on structures where core is

orientated.

All core is photographed.

Historic drilling was logged with logging mostly recorded on

paper in reports lodged with the NSW Department of Mines.

Sub-

sampling

techniques

and sample

preparation

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

If non-core, whether riffled, tube sampled, rotary split, etc. and whether sampled

wet or dry.

For all sample types, the nature, quality and appropriateness of the sample

preparation technique.

Quality control procedures adopted for all sub-sampling stages to maximise

representivity of samples.

Measures taken to ensure that the sampling is representative of the in situ material

collected, including for instance results for field duplicate/second-half sampling.

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

sampled.

Once all geological information was extracted from the drill

core, the sample intervals were cut with an Almonte

automatic core saw, bagged and delivered to the

laboratory.

This is an appropriate sampling technique for this style of

mineralization and is the industry standard for sampling of

diamond drill core.

PQ and HQ sub-samples were quarter core and NQ half

core.

Sample sizes are considered appropriate for the

disseminated, generally fine-grained nature of

mineralisation being sampled.

Duplicate sampling on some native copper bearing intervals

in TRDD001 was undertaken to determine if quarter core

samples were representative, with results indicating that

sampling precision was acceptable. No other duplicate

samples were taken.

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.

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

parameters used in determining the analysis including instrument make and model,

reading times, calibrations factors applied and their derivation, etc.

Nature of quality control procedures adopted (e.g. standards, blanks, duplicates,

external laboratory checks) and whether acceptable levels of accuracy (ie lack of

bias) and precision have been established.

Gold was determined by fire assay and a suite of other

elements including Cu and Mo by 4-acid digest with ICP-

AES finish at ALS laboratories in Orange and Brisbane.

Over-grade Cu (>1%) was diluted and re-assayed by

AAS.

Techniques are considered total for all elements. Native

copper mineralisation in TRDD001 was re-assayed to

check for any effects of incomplete digestion and no

issues were found.

For holes up to TRDD007 every 20th sample was either a

commercially supplied pulp standard or pulp blank. After

TRDD007 coarse blanks were utilised.

Results for blanks and standards are checked upon receipt

of assay certificates. All standards have reported within

certified limits of accuracy and precision.

Historic assays on other projects were mostly gold by fire

assay and other elements by ICP.

Verification

of sampling

and

assaying

The verification of significant intersections by either independent or alternative

company personnel.

The use of twinned holes.

Documentation of primary data, data entry procedures, data verification, data

storage (physical and electronic) protocols.

Discuss any adjustment to assay data.

Significant intercepts were calculated by Kincora's

geological staff.

No twinned holes have been completed.

The intercepts have not been verified by independent

personal.

Logging data is captured digitally on electronic logging

tablets and sampling data is captured on paper logs and

transcribed to an electronic format into a relational

database maintained at Kincora's Mongolian office.

Transcribed data is verified by the logging geologist.

Assay data is received from the laboratory in electronic

format and uploaded to the master database.

No adjustments to assay data have been made.

Outstanding assays are outlined in the body of the

announcement.

Location of

data points

Accuracy and quality of surveys used to locate drill holes (collar and down-hole

surveys), trenches, mine workings and other locations used in Mineral Resource

estimation.

Specification of the grid system used.

Quality and adequacy of topographic control.

Collar positions are set up using a hand-held GPS and later

picked up with a DGPS to less than 10cm horizontal and

vertical accuracy.

Drillholes are surveyed downhole every 30m using an

electronic multi-shot magnetic instrument.

Due to the presence of magnetite in some alteration zones,

azimuth readings are occasionally unreliable and magnetic

intensity data from the survey tool is used to identify these

readings and flag them as such in the database.

Grid system used is the Map Grid of Australia Zone 55,

GDA 94 datum.

Topography in the area of Trundle is near-flat and drill

collar elevations provide adequate control

Data

spacing

and

distribution

Data spacing for reporting of Exploration Results.

Whether the data spacing and distribution is sufficient to establish the degree of

geological and grade continuity appropriate for the Mineral Resource and Ore

Reserve estimation procedure(s) and classifications applied.

Whether sample compositing has been applied.

Kincora drilling at Trundle is at an early stage, with drill

holes stepping out from previous mineralisation intercepts

at various distances.

Data spacing at this stage is insufficient to establish the

continuity required for a Mineral Resource estimate.

No sample compositing was applied to Kincora drilling.

Historic drilling on Trundle and other projects was

completed at various drill hole spacings and no other

projects have spacing sufficient to establish a mineral

resource.

Orientation

of data in

relation to

geological

structure

Whether the orientation of sampling achieves unbiased sampling of possible

structures and the extent to which this is known, considering the deposit type.

If the relationship between the drilling orientation and the orientation of key

mineralised structures is considered to have introduced a sampling bias, this should

be assessed and reported if material.

The orientation of Kincora drilling at Trundle has changed

as new information on the orientation of mineralisation and

structures has become available.

The angled drill holes were directed as best possible

across the known lithological and interpreted mineralized

structures.

There does not appear to be a sampling bias introduced by

hole orientation in that drilling not parallel to mineralised

structures.

Sample

security

The measures taken to ensure sample security.

Kincora staff or their contractors oversaw all stages of

drill core sampling. Bagged samples were placed inside

polyweave sacks that were zip-tied, stored in a locked

container and then transported to the laboratory by Kincora

field personnel.

Audits or

reviews

The results of any audits or reviews of sampling techniques and data.

Mining Associates has completed an review of sampling

techniques and procedures dated January 31st, 2021, as

outlined in the Independent Technical Report included in the

ASX listing prospectus, which is available at:

https://www.kincoracopper.com/investors/asx-prospectus

Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)

Criteria

JORC Code explanation

Commentary