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AUCU.CN ·

Inflection Resources Provides Exploration Update On Copper-Gold Projects In Northern New South Wales

Exploration Programs

Suite 1210 – 1130 West Pender Street

Vancouver, British Columbia, Canada, V6E 4A4

T +1 (604) 681-9100

[email protected]

Inflection Resources Provides Exploration Update On

Copper-Gold Projects In Northern New South Wales

Vancouver, British Columbia, May 27, 2021: Inflection Resources Ltd. (CSE: AUCU) (FSE:

5VJ) (OTCQB: AUCUF) (the "Company" or "Inflection") is pleased to provide an exploration

update from its copper-gold drill projects in Northern New South Wales, Australia.

Summary Highlights

• First-pass drilling on the Mundadoo target intercepted zones of intense and favourable high

temperature potassic-style biotite overprinted by sericite alteration suggesting proximity to a

new and additional, previously unrecognised porphyry centre;

• Further step-out drilling on the high priority Trangie target has identified the most intense zone

of alteration and mineralisation intercepted to date, suggesting a potential porphyry centre

located to the northeast, possibly associated with an untested magnetic low;

• First-pass drilling on the Foster target intercepted zones of native copper associated with

quartz-magnetite veins; and

• Drilling continues in New South Wales across the portfolio of 100% owned copper-gold and

gold targets. The program is systematically drilling untested regional targets as well as

completing a series of step-out vectoring drill holes on high priority targets where favourable

alteration and mineralisation has been identified.

Exploration Update

The Company is continuing to explore its large portfolio of 100% owned projects for large alkalic

copper-gold and gold deposits in the northern extension of the Macquarie Arc, Australia’s premier

porphyry gold -copper province. Nine additional holes have been completed across the

Mundadoo, Trangie, Myallmundi, Foster and Newhaven targets totalling 2,280 metres. Inflection

has now completed forty-six holes totalling 10,097 metres since the inception of the Northern New

South Wales drill program.

First-pass drilling on the Mundadoo target intercepted zones of intense and favourable high

temperature potassic-style alteration manifest as early biotite veins, the degree and style of which,

together with the amount of sulphide is considered highly encouraging and suggests potential

proximity to an additional, previously unrecognised porphyry centre. The Company considers this

hole highly significant and immediately ranks Mundadoo as a high priority target warranting follow-

up, step-out drilling.

Step-out drilling on the high priority Trangie target has identified the most intense zone of

alteration and mineralisation intercepted to date. Hole TRNDDH013 intercepted strong propylitic

and potassic alteration and significant sulphide mineralisation. The alteration, mineralisation and

green rock geochemical indicators all suggest a vector towards the northeast, potentially

associated with a distinct magnetic low identified in the airborne magnetics.

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First-pass drilling on the Foster target intercepted several intervals of native copper associated

with quartz-magnetite veins that indicate the presence of an additional hydrothermal centre.

Drilling was delayed for periods over the last quarter due to extremely wet weather , widely

reported in the Australian press as a once in a hundred year event. This rare weather event

impacted Eastern Australia and in particular blocked access to a number of key drill targets for a

number of weeks.

Alistair Waddell, Inflection’s President and CEO, states “Our ongoing Northern New South Wales

drill program continues to provide very encouraging results. The strong biotite vein development,

which is indicative of porphyry -proximal potassic -style alteration, encountered in drill hole

MUNDH002 into the Mundadoo target is very exciting considering the target has never been

previously drilled. This indicative porphyry style alteration suggests Inflection has identified an

additional porphyry centre. The next phase of drilling will be very exciting as we follow up on

Mundadoo and the other high priority targets already defined, as well as continue our first -pass

regional drill program.”

Figure 1: Northern NSW Project – Drill target location and status map.

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Further Technical Details

Mundadoo Target – First-Pass Drilling

The previously undrilled Mundadoo target is located within the central part of the inferred

Macquarie Arc in the northern sector of Inflection’s tenement holding. The large interpreted

magnetic complex displays similar geophysical characteristics to that of the North parkes district

as indicated by the amplitude of the aeromagnetic and Bouguer gravity data. Inflection drilled two

initial holes, MUNDH001 and MUNDH002, which are separated by approximately 3.5 kilometres.

Hole MUNDH002 tested the anulus of a discrete magnetic low within the southwest margins of

the interpreted magnetic complex. The hole cut a sequence of post-mineral sedimentary cover

before intercepting Paleozoic basement at 139.2 metres before being terminated at 180.9 metres.

The basement sequence comprises of volcaniclastic units separated by andesite s. The entire

core sequence displays strong favourable high-temperature potassic alteration manifested by

dense early biotite veins with a later seri cite-pyrite vein overprint. Significant pyrite and trace

chalcopyrite, occurs throughout the core as disseminations, and within veinlets and various styles

of quartz vein s. Some veins comprising quartz -pyrite-sericite-chlorite +/ -chalcopyrite are

interpreted to be “D-style”. Occasional pervasive albite alteration is also apparent.

The degree and style of the potassic alteration intersected in this hole, together with the amount

of sulphide, is considered highly encouraging and suggests the hole is located potentially in the

vicinity of an additional, previously unrecognised porphyry centre. It is interpreted that the sericite

alteration overprint on the potassic alteration is manifest in aeromagnetic data as a low or zone

of magnetite depletion. The Company considers this hole highly significant and immediately ranks

Mundadoo as a high priority target warranting follow-up drilling. Going forward the Company is

planning a series of step-out drill holes to further test this target.

Figure 2: Drill hole MUNDH002: (A) biotite altered andesite with strong sericite -pyrite veining (B) strong

biotite altered fine-grained andesite with sericite alteration overprint. (C) biotite altered feldspar porphyritic

andesite cut by quartz-pyrite vein with sericite alteration margins (“D-veins”).

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Hole MUNDH001 targeted a magnetic high in the northern part of the interpreted intrusive

complex and intersected a highly magnetic monzodiorite . Fine disseminated pyrite occurs

throughout the core, but no significant alteration other than hematite flooding was encountered.

No further work is planned on this specific magnetic feature.

Trangie Target – Step-Out Drilling

Three further holes have been completed to follow up on the significant alteration and

mineralisation intersected in drill hole TRNDH007 (Infection News Release February 1, 2021).

Drill holes TRNDH011 and TRNDH012 were drilled approximately 250 metres to the northwest

and southeast of TRNDH007 and hole TRNDH013 was collared approximately 50 metres east of

TRNDH007 and drilled northeastwards at a shallow angle (-38 degrees below the unconformity)

towards a coincidental magnetic low and high temperature anomaly as inferred from the “green

rock” geochemistry study. “Green rock” geochemistry is a vectoring methodology the Company

is using to focus exploration towards potential porphyry-related copper-gold mineralisation.

All three Trangie holes intersected strong propylitic alteration (epidote-quartz-chlorite) typically in

sequences of andesites and volcaniclastics . Strongly potassically -altered monzonite was

intersected in TRNDH013.

In TRNDH011 pervasive albitization has made the host rock very hard, reflected in the shallower

unconformity of 161 metres compared with an average of around 180 metres for the target area.

TRNDH013 intersected a much larger lateral intercept area due to the shallow angle of the drill

hole resulting in a greater variety of rock types and alteration assemblages. The upper part of

the hole shows two high temperature alteration events: a high temperature calcic sodic event

typified by albite-epidote-magnetite and a high temperature potassic event represented by biotite

– magnetite-pyrite-chalcopyrite, both pervasive and fracture controlled. Pyrite and chalcopyrite

were intersected in all three holes , occurring predominantly as disseminations, in sulphide-only

fine veinlets, and within quartz-epidote +/-magnetite veins.

The results of the drilling have further confirmed the prospectivity of the Trangie target, particularly

the nature of the high temperature alteration. These results together with green rock geochemical

results and the airborne magnetic data indicate a vector toward the northeast of holes TRNDH007

and TRNDH013. This area will be tested as part of the on-going drill program. Samples from the

three drillholes have been submitted for assay and results are pending.

Figure 3: TRNDH013 ~253.0 m. Highly altered porphyritic andesite drill core. Early albite-epidote-chlorite

cut by vein selvedges and patches of biotite/sericite and magnetite.

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Myallmundi Target – Step-Out Drilling

Two drill holes were planned to test favourable geochemical and “heat” vectors determined from

analysis of “green rock” geochemistry of epidote and chlorite, undertaken by Dr. Josh Phillips in

association with the Centre for Ore Deposits and Earth Sciences (CODES) at the University of

Tasmania. Both targets are based on both favourable geochemical trends from the study and

inferred “heat trends”.

Drill hole MYLDH012 tested the inferred high-temperature trend and was drilled relatively close

to previous drilled holes MYLD001 and MYLDH005 which returned strong propylitic alteration with

pyrite and chalcopyrite. Despite proximity to this hole , MYLDH012 intercepted weakly to

moderately foliated volcanics of little economic interest. Minor epidote-carbonate-quartz veining

occurs throughout the drillhole and is cut by late -stage carbonate quartz veins with r are,

disseminated pyrite.

An additional priority target remains to be drilled at Myallmundi but as a result of the extremely

wet weather that occurred in April, access has been problematic due to boggy ground.

Figure 4: Trangie and Myallmundi targets - Drill hole location map with RTP TMI magnetics

Foster Target – First-Pass Drilling

The Foster target was selected to evaluate the eastern part of a large 3.0 x 1.5 kilometre magnetic

feature. Inflection used magnetic inversion processing to better define the magnetic feature.

The Inflection drill hole intersected Paleozoic basement at 285.6 metres and continued to 336.9

metres with the basement interpreted comprising quartz and chlorite veined, clay-hematite altered

volcaniclastic sediments grading to chlorite -clay altered. Overall alteration in the basement is

limited except for patchy epidote-biotite-magnetite alteration.

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Native copper occurs sporadically throughout the hole typically associated with quartz-magnetite

veins. No sulphides were observed in the hole which makes the presence of native copper

intriguing. The Company is currently revaluating the target and obtaining petrology to define the

next steps.

Figure 5: Drill hole FOSDH002 –290.20 metres - Native copper occurring in within small quartz vein

stockwork

Newhaven Target – First-Pass Drilling

One 300 metre deep hole was drilled into the Newhaven target targeting an interpreted zoned

intrusive complex. The hole failed to reach the Paleozoic basement and due to the depth of cover

no further work is planned on this target.

Northern NSW Exploration Plans Going Forward

Drilling is currently continuing across the portfolio of untested regional targets that are located in

an area extending over approximately 200 kilometres in Northern NSW (Figure 1). The next

targets to be tested are Marra, Melmiland, Waratah and Myallmundi.

Approvals are also currently being sought to drill additional step-out/vectoring holes at Mundadoo,

Trangie, and Myallmundi targets.

Further updates will be provided as additional drill holes are completed.

Northern NSW - Exploration Strategy

Inflection is systematically drill testing a series of Cu -Au and Au targets within the interpreted

northern extension of the Macquarie Arc, part of the Lachlan Fold Belt in New South Wales. The

Company is using cost-effective mud-rotary drilling to cut through the unmineralized post-mineral

sedimentary cover. Once basement is reached, the rig transitions to diamond core drilling. It is

well documented that mineralized bodies elsewhere in the belt, in particular porphyry and intrusive

related systems, hav e large district -scale alteration and geochemical halos or footprints

surrounding them. The Company is completing a series of short diamond drill holes into bedrock

rather than just one or two deep and more expensive diamond drill holes. Multiple data po ints

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gained from alteration and mineral geochemistry is then used to vector additional deeper holes.

This is a proven exploration strategy in the covered segments of the Macquarie Arc having been

directly responsible for the discovery of the Northparkes and Cowal deposits.

Qualified Person

The scientific and technical information contained in this news release has been reviewed and

approved by Mr. Carl Swensson (FAusIMM), Inflection’s VP Exploration, and a “Qualified Person”

(“QP”) as defined in National Instrument 43- 101 – Standards of Disclosure for Mineral Projects.

Sampling Quality Control

Drilling was conducted using a truck -mounted multi-purpose drill rig. Mud rotary drilling was

utilised to drill through the cover sequence before transitioning to diamond drilling using NQ sized

core at the unconformity. Core was logged at the Company’s field office, photographed and

marked before being cut to the Company’s specified sample intervals. Half core samples were

placed in bags with internationally certified blanks and standards inserted.

Samples were dispatched to ALS Laboratories in Orange NSW an accredited analytical laboratory

meeting ISO/IEC 17025:2005 and ISO 9001:2015. Samples were prepared by crushing and

grinding via ALS methods CRU -21 and PUL-32 respectively. The pulps were then assayed for

48 elements via ALS method ME-MS61 using a 25g sample after a four acid near total digest with

an ICP-MS finish. Gold was assayed by fire assay using ALS method Au -AA23 using a 30g

sample charge and AAS finish. Laboratory standards and QA-QC are monitored by the Company.

Coarse rejects from the sample preparation are subjected to spectral analysis.

About Inflection Resources Ltd. Inflection is a technically driven copper-gold and gold focused

mineral exploration company listed on the Canadian Securities Exchange under the symbol

“AUCU” and on the OTCQB under the symbol “AUCUF” with projects in Australia. The Company

is systematically drill testing a large portfolio of projects in New South Wales and in Queensland.

The Company is exploring for large copper-gold and gold deposits in the northern interpreted

extension of the Macquarie Arc, part of the Lachlan Fold Belt in New South Wales. The Macquarie

Arc is Australia’s premier porphyry gold-copper province being host to Newcrest Mining’s Cadia

deposits, the CMOC Northparkes deposits and Evolution Mining’s Cowal deposits plus numerous

exploration prospects including Boda, the recent discovery made by Alkane Resources.

For more information, please visit the Company’s website at www.inflectionresources.com.

On Behalf of the Board of Directors

“Alistair Waddell”

President and CEO

For further information, please contact:

Brennan Zerb

Investor Relations Manager

+1 (778) 867-5016

[email protected]

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Forward-Looking Statements: This news release includes certain forward -looking statements and

forward-looking information (collectively, "forward -looking statements") within the meaning of applicable

Canadian securities legislation. All statements, other than statements of historical fact, included herein

including, without limitation, statements regarding future capital expenditures, anticipated content,

commencement, and co st of exploration programs in respect of the Company's projects and mineral

properties, and the anticipated business plans and timing of future activities of the Company, are forward -

looking statements. Although the Company believes that such statements ar e reasonable, it can give no

assurance that such expectations will prove to be correct. Often, but not always, forward looking information

can be identified by words such as "pro forma", "plans", "expects", "may", "should", "budget", "scheduled",

"estimates", "forecasts", "intends", "anticipates", "believes", "potential" or variations of such words including

negative variations thereof, and phrases that refer to certain actions, events or results that may, could,

would, might or will occur or be taken or achieved. Forward-looking statements involve known and unknown

risks, uncertainties and other factors which may cause the actual results, performance or achievements of

the Company to differ materially from any future results, performance or achievements expressed or implied

by the forward-looking statements. Such risks and other factors include, among others, statements as to

the anticipated business plans and timing of future activities of the Company, including the Company's

exploration plans. the proposed expenditures for exploration work thereon, the ability of the Company to

obtain sufficient financing to fund its business activities and plans, delays in obtaining governmental and

regulatory approvals (including of the Canadian Securities Exchange), perm its or financing, changes in

laws, regulations and policies affecting mining operations, the Company's limited operating history,

currency fluctuations, title disputes or claims, environmental issues and liabilities, as well as those factors

discussed under the heading "Risk Factors" in the Company's prospectus dated June 12, 2020 and other

filings of the Company with the Canadian Securities Authorities, copies of which can be found under the

Company's profile on the SEDAR website at www.sedar.com.

Readers are cautioned not to place undue reliance on forward -looking statements. The Company

undertakes no obligation to update any of the forward-looking statements, except as otherwise required by

law.