Rokmaster Samples 657.0 g/t Ag and 11.46% Zn on the Selkirk Project

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VANCOUVER, BC, Nov. 5, 2024 /CNW/ - Rokmaster Resources Corp. (TSXV: RKR) (OTCQB: RKMSF) (FSE: 1RR1) ("Rokmaster" or "the Company") is pleased to provide an update for its 100% owned Selkirk Project.

Selkirk Project Map (CNW Group/Rokmaster Resources Corp.)
Selkirk Project Map (CNW Group/Rokmaster Resources Corp.)

The Selkirk Project is comprised of three properties: (a) the Keystone Property; (b) the Rift Property; and (c) the Downie Gold Property located north of Revelstoke in southeastern British Columbia (Figure 1). These three properties have been advanced by Rokmaster since 2021 with positive results generated from geological mapping, prospecting, channel sampling, and soil sampling. A field work program was completed in August 2024 on the Keystone Property and the Rift Property. Further encouraging assay results1 have been returned from the rock and soil samples collected in 2024 and are described below.

The 5,276 hectare Keystone Property is underlain by early Paleozoic sedimentary and volcanic rocks of the Index Formation. The northern extension of the mapped Akolkolex Thrust fault occurs within and proximal to the property, providing potential for orogenic-style gold mineralization. During one of the Company's first visits to the Keystone Property in 2021, a historical trench was found which exposes arsenopyrite mineralization grading 4.51 g/t Au, 274 g/t Ag, and 2.92% Zn in a grab sample. Replacement and vein-hosted sphalerite and galena mineralization has been discovered throughout the large property during later field work programs collecting grab samples (Figure 2). The 2024 field work found further high-grade silver, lead, and zinc mineralization with grab samples in two new areas of the property, termed the Western and Eastern Expansion areas, where zones of dense quartz-galena-sphalerite veining is hosted in deformed dolostone.

Table 1: Keystone Property Highlighted 2024 Rock Sample Results1

2024 Sample

Area

Easting

Northing

Pb+Zn %

Ag g/t

Pb %

Zn %

Au g/t

BD0093

Western Expansion

410605

5700759

26.07

657.0

14.61

11.46

0.107

JD03

Western Expansion

410444

5700960

7.66

177.0

7.58

0.08

0.106

BD0089

Western Expansion

410275

5701000

6.54

229.0

6.51

0.03

0.16

BD0088

Western Expansion

410309

5700931

3.95

76.7

3.77

0.18

0.034

BD0086

Western Expansion

410273

5700824

3.29

49.7

2.14

1.15

0.18

CM13

Eastern Expansion

411347

5701216

32.48

459.0

28.10

4.38

0.024

CM11

Eastern Expansion

411461

5701564

20.62

327.0

19.37

1.25

0.053

CM05

Eastern Expansion

411487

5700484

15.18

103.0

5.14

10.04

1.44

BD0082

Eastern Expansion

411677

5701290

13.68

54.5

2.91

10.77

0.029

BD0083

Eastern Expansion

411416

5701203

3.13

58.1

2.49

0.64

0.043

BD0085

Eastern Expansion

411246

5701320

2.16

27.4

2.02

0.14

0.0025

CM06

Eastern Expansion

411487

5700484

4.98

82.3

1.81

3.17

3.07

The 299 hectare Rift Property hosts the Rift Showing where grab samples collected in 2022 assayed up to 35.25% Zn, 8.60% Pb from a stratabound massive sphalerite-galena horizon in pelitic schist. The sulphide mineralization averages 1.0 metre in thickness and is exposed for approximately 25 metres of strike length in the incised creek gully of Rift Creek, before being lost under cover (Figure 3). Drillhole M-85-2 was completed in 1985 approximately 460 m east of the Rift Showing and encountered 22.21% Zn and 4.82% Pb over 1.82 m and may represent the on-strike continuity of the Rift stratiform zinc-lead massive sulphide horizon2,3. Soil sampling in 2024 tested the eastern continuation of a soil anomaly generated in 2022. Although the soil anomaly was not extended, the results give credence to the theory that the mineralization encountered in drillhole M-85-2 represents a blind extension of the massive sphalerite-galena mineralization outcropping at the Rift Showing.