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Minsud announces results of Phase 2 drilling program at Chita Valley Project, San Juan, Argentina

Exploration Programs

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TSX-V: MSR

February 5, 2021

Minsud announces results of Phase 2 drilling program at Chita

Valley Project, San Juan, Argentina

TORONTO, ONTARIO – Minsud Resources Corp. (TSX-V: MSR) (“Minsud” or the “Company” ),

is pleased to announce the completion of Phase 2 diamond drilling program, comprised of 12 holes,

5,818 meters, with variable depths between 350-650 meters, completed at the Chita and Chinchillones

porphyry targets, part of the Chita Valley Project . Together with Phase 1, the Company completed a

total of 9,377 meters during 2020, as shown in Map 1.

The program tested targets identified during the systematic multidisciplinary exploration program

conducted in the sector during Phase 1 drilling program completed during first half of 2020, and the

results from the pole -dipole geophysical survey covering 68 kilometers over 13 Induced Polarization

(IP) lines completed on July 2020.

Map 1: Chinchillones and Chita Polymetallic and Porphyry Complex

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Target Chinchillones: Scouting drill holes CHDH20-04 and CHDH20-05 (Phase 1) together with drill

hole CHDH20-17 (Phase 2) confirm the presence of a deep porphyry system and linked shallow

polymetallic Cu-Au-Pb-Zn mineralizations hosted in breccias and veins at the North West edge

of the Chita Valley. Early Chalcopyrite -molybdenum veins crosscut by hydroth ermal late veins

suggests a telescoping hydrothermal event overimpossed to the porphyry system, potassium alteration

(Magnetite-Biotite) appear s as a re lict in the widespread Quartz-sericite alteration. At the southern

edge of the Chinchillones area , the porphyry system appear s to be intrude d by a late phreato

magmatic breccia (Diatreme) and a Dacite Dome. Intermediate sulphidation (IS) Pb-Zn-Mn-Au-Ag

mineralization types, appear to be relate d with these magmatic hydrothermal breccias aligned in the

North North East direction. Anomalous values of Cu-Au-Ag-Pb-Zn detected in drillhole CHDH20-08

are a typical dome-related mineralization.

The Cu-Mo and Pb-Zn +/- Au Ag mineralization identified at the Chinchillones area confirms that this

area constitutes a high priority target with significant potential of exploration.

Phase 2: Chinchillones area - Summary of Analytical Results

Hole ID From To Length Au Ag Cu Mo Pb Zn

(mt) (mt) (mts) (*) g/t g/t % ppm ppm ppm

CHDH20-07 66 82 16 0.07 13.63 0.46 81 728 2,276

including 66 68 2 0.11 25.30 2.68 99 1,950 8,610

120 186 66 0.11 14.35 0.14 65 1,321 3,061

264 393 129 0.02 9.69 0.05 99 1,047 4,926

CHDH20-08 42 68 26 0.12 4.80 0.07 2 756 1,629

114.5 115.3 0.8 0.99 307.00 7.45 7 3,000 18,850

303 309 6 0.34 54.22 0.27 32 498 3,579

354 450 96 0.07 15.16 0.03 3 2,140 5,467

CHDH20-09 122 128 6 0.19 24.26 0.11 6 737 1,553

450 456 6 0.07 76.64 0.17 5 1,728 4,973

CHDH20-10 12 22 10 0.36 75.79 2.66 4 22,489 7,079

including 16 18.3 2.3 0.60 163.78 8.43 6 49,170 23,052

65 69 4 0.10 14.40 0.10 47 541 3,763

132 136 4 0.11 10.65 0.03 2 5,493 20,810

235 241 6 0.13 35.87 0.19 2 2,153 16,743

CHDH20-17 100 178 78 0.16 6.47 0.21 87 144 3,531

240 347 107 0.20 24.07 0.11 16 2,046 5,942

464 524 60 0.02 1.49 0.24 137 59 740

CHDH20-18 104 238 134 0.07 3.38 0.19 76 68 190

including 107 108 1 0.32 102.00 3.52 15 430 2,850

285 292 7 0.35 5.00 0.28 39 60 167

388 398 10 0.06 11.71 0.25 57 76 408

(*) Intervals reported in the above table are not true thicknesses

Target Chita North porphyry (PNO): This target was tested through drill holes CHDH20-11,

CHDH20-12, CHDH20-14, CHDH20-15 and CHDH20-16. The main rock type intercepted corresponds

to an Andesite porphyry. The dominant hydrothermal alteration correspond s to a marginal propylitic

Py halo (3%-5%). Drill hole CHDH20 -12, approximately at 412 meters deep, intercepted a porphyry

with Potassium alteration type , conformed by Biotite -Magnetite +/ - Potassium Feldspar. The

mineralization is scarce , associated to N orth North East structures with Chalcopyrite -Sphalerite

(intermediate sulphidation system ) and relict of primary Molybdenite mineralization. The continuity to

the north of the potassiu m alteration detected at the southern margin of the Chita Valley is still not

clear and should be confirmed through future geological mapping and drillings.

Target Chita South porphyry (PSU): It was only tested through drill hole CHDH20-13. Mineralization

of 0.3% to 0.4% Cu, up to 100 - 120 meters. The best grades are associated with Chalcocite (product

of a secondary enrichment process) coating on Pyrite and Chalcopyrite, together with copper oxide

fillings (mix Cu Ox –Sulphur zone).

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Phase 2: Chita PSU and PNO - Summary of Analytical Results

Hole ID From To Length Au Ag Cu Mo Pb Zn

(mt) (mt) (mts) (*) g/t g/t % ppm ppm ppm

CHDH20-11 424 480 56 0.02 0.64 0.09 271 7 29

CHDH20-12 32 48 16 0.08 4.74 0.39 40 155 492

including 39.5 40 0.5 0.88 64.20 3.47 351 118 780

332 342 10 0.05 2.76 0.17 35 72 263

CHDH20-13 24 126 102 0.08 2.06 0.33 253 39 104

152 192 40 0.04 0.87 0.11 189 18 181

CHDH20-14 120 124 4 0.06 2.37 0.06 22 96 5,765

174 182 8 0.08 2.81 0.04 6 610 3,303

CHDH20-15 288 292 4 0.21 9.30 0.16 5 110 300

CHDH20-16 Intercepts hydrothermal pyrite halo

(*) Intervals reported in the above table are not true thicknesses

The results of this Phase 2 scout drilling exploration program confirm very interesting intercepts that

support effectively the presence at shallow and at down depth level of a Zn-Pb-Cu-(Ag-Au) polymetallic

epithermal system and deeper parental porphyry Cu -Mo-Au open to the North North East at

Chinchillones area.

The geological team is currently working on detailed re-logging of the Phase 2 drill core and mapping,

together with the review of all the available structural and geochemical data in order to assist on

targeting for the next Phase 3 drill program that is being designed and scheduled to commence during

the first half of 2021.

Conceptual Geological Model

Different magmatic -hydrothermal breccias observed at Chita and Chinchillones reflect a complex

sequence of multiple events that can be linked to explosive events developing in the upper parts of the

porphyry system during their emplacement, uplift and unroofing. In fact, at Chita and Chinchillones, a

large part of the evolution of this porphyry system would have developed in a tectonic framework

characterized by the occurrence of high rates of regional tectonic uplift and erosion, which would have

favored the generation of telescoping processes related to mineralization process and the formation

of the diatreme complex.

Quality Assurance/Quality Control

All core samples were submitted to the ALS Laboratories in Mendoza, Argentina for preparation and

analysis. All samples were analyzed for Au by fire assay/ AA finish 50g, plus a 48-element ultra-trace

four acid digest with ICP -MS and ICP -AES finish. Minsud followed industry standard procedures for

the work with a quality assurance/quality control (QA/QC) program. Field duplicates, standards and

blanks were included with all sample shipments to the principal laboratory. Minsud detected no

significant QA/QC issues during review of the data.

Mr. Mario Alfaro, Professional Geoscientist, VP -Exploration of the Company, is a qualified person as

defined by Canadian National Instrument 43 -101. Mr. Alfaro visited the property and has read and

approved the contents of this release.

About the Chita Valley Project, San Juan Province:

The Chita Valley Project is a large expl oration stage porphyry system with classic alteration features,

widespread porphyry s tyle Cu -Mo-Ag-Au mineralization and associated gold and s ilver-bearing

polymetallic veins of intermediate sulfide composition that conformed an outcropping porphyry system

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at Chita and a lithocap of a porphyry system at Chinchillones. San Juan Province of Argentina has a

robust mining sector and recognizes the important economic benefits of responsible development of

its substantial Mineral Resource endowment.

About Minsud Resources Corp.

Minsud is a mineral exploration company focused on exploring its flagship Chita Valley Cu-Mo- Au-Ag

Project, in the Province of San Juan, Argentina. The Company also holds a 100% owned portfolio of

selected early stage prospects, including 6,000 ha in Santa Cruz Province, Argentina.

FOR FURTHER INFORMATION PLEASE CONTACT

Ramiro Massa

President and Chief Executive Officer

[email protected]

+1 416-479-4466

CAUTIONARY STATEMENT REGARDING FORWARD-LOOKING INFORMATION:

This news release includes certain information that may constitute forward -looking information under

applicable Canadian securities laws. Forward -looking information includes, but is not limited to,

statements about strategic plans, spending commitments, f uture operations, results of exploration,

anticipated financial results, future work programs, capital expenditures and objectives. Forward -

looking information is necessarily based upon a number of estimates and assumptions that, while

considered reasonable, are subject to known and unknown risks, uncertainties, and other factors which

may cause the actual results and future events to differ materially from those expressed or implied by

such forward-looking information including, but not limited to: fluctuations in the currency markets (such

as the Canadian dollar, Argentina peso, and the U.S. dollar); changes in national and local

government, legislation, taxation, controls, regulations and political or economic developments in

Canada and Argentina or other countries in which the Corporation may carry on business in the future;

operating or technical difficulties in connection with exploration and development activities; risks and

hazards associated with the business of mineral exploration and development (i ncluding

environmental hazards or industrial accidents); risks relating to the credit worthiness or financial

condition of suppliers and other parties with whom the Company does business; presence of laws and

regulations that may impose restrictions on min ing, including those currently enacted in Argentina;

employee relations; relationships with and claims by local communities; availability and increasing

costs associated with operational inputs and labour; the speculative nature of mineral exploration and

development, including the risks of obtaining necessary licenses, permits and approvals from

government authorities; business opportunities that may be presented to, or pursued by, the Company;

challenges to, or difficulty in maintaining, the Company’s tit le to properties; risks relating to the

Company’s ability to raise funds; and the factors identified under “Risk Factors” in the Company's Filing

Statement dated April 27, 2011. There can be no assurance that such information will prove to be

accurate, as actual results and future events could differ materially from those anticipated in such

information. Accordingly, readers should not place undue reliance on forward -looking information. All

forward-looking-information contained in this news release is given as of the date hereof and is based

upon the opinions and estimates of management and information available to management as at the

date hereof. The Company disclaims any intention or obligation to update or revise any forward-looking

information, whether as a result of new information, future events or otherwise, except as required by

law.

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

policies of the TSX Venture Exchange) accepts responsibility for t he adequacy or accuracy of this

release.