Kingsmen Resources - Las Coloradas Project - High Grade Analyses

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - October 7, 2024) - Kingsmen Resources Ltd. (TSXV: KNG) (OTCQB: KNGRF) ("Kingsmen" or the "Company") is pleased to report high-grade multi-element analyses from the 2.5 km long Silvia - La Plata (SLP) trend on the 100% owned Las Coloradas project, is in the Parral mining district of the Central Mexican Silver Belt, Chihuahua Mexico. The trend as currently recognized, comprises two areas referred to as the Silvia Trend and La Plata Zone. Results are presented in Figure 1 and Table 1.

Highlights

  • Seventy-two samples were analyzed.

  • 1 > 500 g/t silver-equivalent (AgEq)

  • 6 > 200 g/t AgEq

  • 6 > 100 g/t AgEq

  • 6 > 0.54 g/t gold

The Silvia zone is located at the intersection of the NE-oriented Silvia - La Plata (SLP) trend and the NW-oriented Soledad/Soledad II structures/vein systems. The La Plata zone contains numerous high-grade AgEq samples and NE, NW and N-trending structures/veins are recognized. N-trending structures/vein systems are unusual in the project area. Of immediate interest is a broadly N-trending intrusive body with AgEq values ranging from 8 to 303g/t AgEq (Figure 1). The curvilinear aspect of this and nearby intrusives may be reflecting a buried quartz porphyry (QP) intruding the volcanic country rock that is generating the mineralization.

The La Plata and Silvia zones contain pathfinder element concentrations in variable combinations including Au, As, Sb, Pb, Zn, Cu, Hg, Mo, Te and Tl. The different combinations of pathfinder elements likely represent different stages or pulses of mineralization. Their distributions provide evidence for district-wide, structurally controlled mineralization.

The Las Coloradas project area is situated on the southeast flank of a prominent aeromagnetic high interpreted to be a buried felsic intrusive body. The felsic intrusives associated with the La Plata and Silvia zones, the Soledad and Soledad II structures and other structures are likely linked to this body. The setting is favourable for porphyry, skarn and epithermal vein mineralization.

Scott Emerson, President, commented: "The presence of high-grade samples hosted in intrusive, volcanic and sedimentary rocks of the La Plata - Silvia zones confirm these are highly prospective area and targets for further exploration to identify drill targets."

Figure 1

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/9640/225772_plata_b_map_550full.jpg

Sample #

Width (m)

Ag ppm

Ag Eq g/t

Au ppm

Cu ppm

Pb ppm

Zn ppm

1

Grab

129

192

0.54

204

17350

4310

2

Grab

182

459

1.01

445

47000

53500

3

0.4

1.62

3

0

10.2

341

304

4

Grab

240

337

0.12

43.8

36800

21700

5

Grab

156

333

1.77

24

37300

1545

6

0.6

30.2

42

0.22

35.9

350

589

7

0.3

3.61

31

0.39

5

101.5

196

8

0.5

0.29

5

0.07

1.4

20.7

8

9

1

8.93

14

0.09

7.5

149

47

10

0.7

0.68

6

0.08

2

22.3

16

11

1

0.85

3

0.03

1.8

14.4

18

12

0.3

0.55

6

0.08

1.6

8.1

12

13

0.5

1.84

11

0.13

2.5

16.2

21

14

0.5

5.7

68

0.9

8.8

33.6

171

15

1

2.95

19

0.23

4.9

12.6

23

16

0.3

1.79

3

0.02

2.4

18.2

26

17

0.3

86.4

96

0.38

18.8

41.3

88

18

Grab

70.8

202

0.26

142.5

34600

20000

19

Grab

12.35

22

0.05

89.4

2060

1455

20

0.2

23.1

23

0.04

15.8

536

127

21

0.5

1.07

3

0.03

5.7

118

51

22

Grab

6.17

21

0.22

10.6

284

93

23

0.3

1.56

2

0

3.8

138.5

42

24

Grab

432

550

0.06

134

46700

37800

25

0.15

1.44

2

0

3.8

77.6

56

26

0.1

1.02

2

0

53.9

110.5

264

27

0.15

2.83

8

0

60

309

1810

28

0.15

3.6

7

0.05

9

86.6

117

29

0.1

13.3

15

0.04

8.4

661

67

30

0.15

20.4

28

0.1

26.4

1645

215

31

0.1

7.18

7

0

16.6

350

63

32

0.2

5.38

9

0.06

8.4

92.4

136

33

0.2

1.41

25

0.33

10.2

138.5

39

34

Grab

161

161

0.23

230

974

1430

35

0.6

24.4

26

0

36.3

2380

272

36

0.5

7.82

20

0.13

18.6

1905

130

37

0.6

1.8

3

0.02

5

38.2

58

38

0.4

0.4

4

0.05

3.8

21.2

77

39

0.3

1.1

2

0

5.6

504

97

40

Grab

5.87

7

0.02

4.4

391

43

41

0.3

1.02

2

0

9.2

259

43

42

0.5

58.9

59

0.02

54.4

1760

220

43

0.1

11

26

0.19

46.7

1355

125

44

0.1

0.55

6

0.07

14.8

127.5

128

45

Grab

51.2

55

0.12

112

2140

82

46

0.1

28.4

30

0

41

243

46

47

Grab

85.8

176

0.71

20.4

24600

1745

48

0.1

25.4

77

0.54

43.2

7800

630

49

0.5

182

183

0.27

294

851

464

50

0.3

43.3

43

0.03

87.2

2360

165

51

Grab

46.2

44

0.07

19.2

641

59

52

2

1.3

10

0.12

2.8

27.6

77

53

1

9.71

16

0.1

7.4

319

208

54

Grab

9.85

16

0.11

15.2

43.1

103

55

Grab

135

303

0.15

223

80100

3400

56

Grab

58.7

167

0.25

68.1

15300

26900

57

Grab

31.2

43

0.02

17.8

5330

1820

58

4

1.94

7

0.02

8.1

1355

604

59

0.15

42.5

55

0.07

152

4370

1880

60

0.8

6.37

13

0.03

92.1

1020

911

61

0.15

18.85

23

0.03

197.5

1430

299

62

Grab

97.3

175

0.11

82.8

38700

1750

63

0.1

0.75

3

0.02

5.6

181

49

64

Grab

153

296

0.09

157.5

72900

3030

65

Grab

3.16

9

0

6.1

2590

319

66

2

19.9

30

0.11

53.4

1330

994

67

0.2

14.95

20

0.09

19.8

415

124

68

Grab

4.48

11

0.02

23.7

2090

332

69

Grab

4.05

8

0

21

1600

396

70

Grab

7.09

20

0

36.9

6160

422

71

Grab

2.16

3

0

59.1

96.3

100

72

0.3

0.38

1

0

3.9

23.5

119