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SKRR Exploration Drill Program Intersects Arsenopyrite Sulphides and Disseminated Arsenopyrite and Quartz Veining

Drill Results

SKRR Exploration Drill Program Intersects

Arsenopyrite Sulphides and Disseminated

Arsenopyrite and Quartz Veining

VANCOUVER, BC

, Oct. 14, 2020 /CNW/ - SKRR Exploration Inc. (TSXV: SKRR) (OTC:

SKKRF) (FSE: B04Q) ("

SKRR

" or the "

Company

") is pleased to report intersections of arsenopyrite

bearing sulphides and disseminated arsenopyrite and quartz veining in the current and ongoing drill

program at the Olson property in the Trans Hudson Corridor, Saskatchewan.

Sherman Dahl

, Chief Executive Officer of SKRR comments:

"

The visual indications of mineralization for which assays are pending, are encouraging."

The drill program at the Olson property is advancing well. To date a total of 7 holes totaling

968m

have been completed on 3 separate target areas; Jena/Juba, Point and Tuscan.

Jena/Juba – Twenty surface samples from outcrops taken earlier this summer returned values

>1000 ppb Au, with a maximum of 15.7 g/t Au from quartz arsenopyrite veins (see News

Release

June 02, 2020

). One hole (OL20001) tested beneath the Juba arsenopyrite-bearing

trenches. Two holes (OL20002 and OL0003) tested the south Jena area to test a significant IP

chargeability anomaly with coincident with the northwest dipping contact between a feldspar

porphyry to the east and meta-sediments to the west.

OL20001 was an angle hole, drilled to the SE and completed to a depth of

116m

. The hole

tested a coincident conductive IP geophysics anomaly associated with arsenopyrite bearing

metasedimentary rocks in surface trenches. Formational pyrite and graphite were

encountered in the hole and likely accounted for the IP anomaly. No obvious mineralization

was encountered.

OL20002 was an angle hole oriented to the west and completed to a depth of

152m

. The

hole collared in granodiorite and intersected a sedimentary contact at

76.6m

. Intermittent

intervals of quartz and sulphide (pyrite, arsenopyrite +/- chalcopyrite) mineralized zones

were encountered between

67m

to

76.6m

. The hole continued in sedimentary schist until

103.6m

then back into intrusive rocks (porphyritic monzonite) to

116m

. Well developed

quartz and sulphide mineralization was encountered from

114m

to

116.14m

with 3-10%

arsenopyrite both disseminated and in massive blebs.

OL20003 was an angle hole collared from the same set-up as OL2002 but at 23 degree

azimuth change to the south. The hole collared in granodiorite, encountered a single

sedimentary contact, which had some notable arsenopyrite occurrence, but not the intensity

of mineralization as in the previous hole.

Point – Three angle drill holes (OL20004, OL20005 and OL20006) tested the Point target

where earlier field work this summer identified anomalous soil geochemistry (80 ppb to 2704.6

ppb Au) and prospecting returned assays up to 9.8 g/t Au. All three holes were collared in

granodiorite, and were designed to test for mineralization associated with an interpreted meta-

sedimentary contact projected to be encountered around ~230m depth.

OL20004 was an angle hole oriented to the west and designed to test a projected

sediment contact around

230m

, beneath

Michael Lake

. The hole was collared in

granodiorite and encountered sediments at only

27m

depth. Multiple pods of intrusive rock

were present to

91m

. Arsenopyrite was encountered in every unit from top to bottom of

this hole with the strongest occurrences in the upper

40m

of Granodiorite, present in

disseminated and massive blebs. Significant arsenopyrite (up to 3% disseminated and

massive blebs) was also present within the fine grained meta-pelitic sediments associated

with numerous narrow quartz-chlorite veins, particularly abundant between

114m

to

141m

.

From

146m

to

151m

strong arsenopyrite (2-5%) was present within foliated sediments.

OL20005 was an angle hole collared from the same set-up as OL20004, but at 60 degree

azimuth change to the south. The hole collared in granodiorite which continued to

20.2m

,

after which the sediment contact was encountered. The hole remained in sediments to the

end of hole at

80m

. Abundant disseminated arsenopyrite was encountered in the top

26m

of the hole within granodiorite and dropped off rapidly after

26m

.

OL20006 was an angle hole drilled to the south. The hole was designed to test a series of

stacked mineralized shears within granodiorite where surface rock samples returned up to

3 g/t Au. The hole intersected granodiorite from top to bottom. Trace sulphides were

present throughout, but 2 shear zones with narrow quartz-chlorite veins stand out with

mineralization of 1-5% arsenopyrite;

32.2m

to

62m

and

95m

to

105m

.

Tuscan – drilling at Tuscan is designed to test the east west intrusive contacts observed at the

Tuscan surface showing. Field work from the earlier summer program included prospecting at

Tuscan, where assay results returned peaks up to 45.1 g/t Au.

OL20007 was an angle hole drilled to the south and completed to a depth of

137m

. The

hole collared in granodiorite and intersected the contact with sedimentary rocks at

96.65m

.

A second granodiorite was intersected at

120.75m

. Promising mineralization was

encountered in 2 distinct zones of sulphide mineralization (

100.5m

to

105.8m

and

112.85m

to

115.55m

) with the most significant being the interval from

112.85m

to

115.55m

which

contained semi-massive to massive sulphide mineralization with up to 40% pyrite and 15%

arsenopyrite.

Table 1: Drill Hole Summary

Collar

Hole ID

Zone

Azimuth

Dip

Total Depth

(m)

OL20001

Juba

135

-45

116

OL20002

Jena

310

-45

152

OL20003

Jena

287

-45

137

OL20004

Point

280

-45

209

OL20005

Point

220

-50

80

OL20006

Point

180

-50

137

OL20007

Tuscan

190

-45

137

Total

968m

Samples from all seven (7) drill holes have been delivered to the laboratory and assay results are

pending.

A variety of core photos are now available

www.skrr.ca

.

Qualified Person

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

approved by

Ross McElroy P.Geol

, a director of the Company and a "Qualified Person" as defined

in National Instrument 43-101 –

Standards of Disclosure

for Mineral Projects

. Mr. McElroy verified

the data disclosed which includes a review of the sampling, analytical and test data underlying the

information and opinions contained therein.

About SKRR Exploration Inc.:

SKRR is a Canadian-based precious metal explorer with properties in

Saskatchewan

- one of the

world's highest ranked mining jurisdictions. The primary exploration focus is on the Trans-Hudson

Corridor in

Saskatchewan

in search of world class precious metal deposits. The Trans-Hudson

Orogen - although extremely well known in geological terms has been significantly under-explored in

Saskatchewan

. SKRR is committed to all stakeholders including shareholders, all its partners and

the environment in which it operates.

ON BEHALF OF THE BOARD

Sherman Dahl

President & CEO

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 the adequacy or accuracy of

this release

.

Forward-Looking Information

This news release contains "forward-looking information or statements" within the meaning of

applicable securities laws, which may include, without limitation, statements that address the drilling

on the Olson property, receipt of assays, other statements relating to the technical, financial and

business prospects of the Company, its projects and other matters. All statements in this news

release, other than statements of historical facts, that address events or developments that the

Company expects to occur, are forward-looking statements. Although the Company believes the

expectations expressed in such forward-looking statements are based on reasonable assumptions,

such statements are not guarantees of future performance and actual results may differ materially

from those in the forward-looking statements. Such statements and information are based on

numerous assumptions regarding present and future business strategies and the environment in

which the Company will operate in the future, including the price of metals, the ability to achieve its

goals, that general business and economic conditions will not change in a material adverse manner,

that financing will be available if and when needed and on reasonable terms. Such forward-looking

information reflects the Company's views with respect to future events and is subject to risks,

uncertainties and assumptions, including those filed under the Company's profile on SEDAR at

www.sedar.com

. Factors that could cause actual results to differ materially from those in forward

looking statements include, but are not limited to, continued availability of capital and financing and

general economic, market or business conditions, adverse weather conditions, decrease in the price

of gold and other metals, equipment failures, failure to maintain all necessary government permits,

approvals and authorizations, the impact of Covid-19 or other viruses and diseases on the

Company's ability to operate, failure to maintain community acceptance (including First Nations),

increase in costs, litigation, and failure of counterparties to perform their contractual obligations. The

Company does not undertake to update forward–looking statements or forward–looking information,

except as required by law.

Olson Project - Trans Hudson Corridor - Jena/Juba zone (CNW Group/SKRR Exploration Inc.)

SOURCE

SKRR Exploration Inc.

View original content to download multimedia:

http://www.newswire.ca/en/releases/archive/October2020/14/c3309.html

%SEDAR: 00027214E

For further information:

Rich Matthews, Investor Relations, Integrous Communications,

[email protected], +1 6047577179

CO: SKRR Exploration Inc.

CNW 13:41e 14-OCT-20