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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
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Seventy-two samples were analyzed.
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1 > 500 g/t silver-equivalent (AgEq)
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6 > 200 g/t AgEq
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6 > 100 g/t AgEq
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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
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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 |