Kuya Silver Expands Mineralized Vein Zone in Phase 2 Drilling at Campbell-Crawford Target, Silver Kings Project
Kuya Silver Expands Mineralized Vein Zone in Phase 2 Drilling at Campbell-Crawford Target, Silver Kings Project
Newly-defined Toms Vein assays 2,180 g/t silver and 0.36% cobalt over 0.40 m within wider zone assaying 199 g/t silver over 7.00 m
新定義的 Toms Vein 在 0.40 m 的更寬區域內測定 2,180 g/t 銀和 0.36% 的鈷,在 7.00 m 範圍內測定 199 g/t 銀
Six drill holes from Campbell-Crawford and Airgiod target areas are pending and visible silver and/or cobalt mineralization was observed in all remaining drill holes
來自坎貝爾-克勞福德和艾爾吉德目標區域的六個鑽孔尚待鑽探,在所有剩餘的鑽孔中都觀察到明顯的銀和/或鈷礦化
Toronto, Ontario--(Newsfile Corp. - January 11, 2024) - Kuya Silver Corporation (CSE: KUYA) (OTCQB: KUYAF) (FSE: 6MR1) (the "Company" or "Kuya Silver") is pleased to present the first assay results from a diamond drilling program at the grassroots Campbell-Crawford target area, at its wholly-owned Silver Kings Project, where drilling in March 2023 intersected high-grade silver in a new grassroots vein structure. Results from holes 23-SK-14 to -26 are presented; in total, 18 oriented NQ drill holes were completed (23-SK-14 to -31) for a combined total of 5,834 m in this program. With additional diamond drilling performed in this target area, Kuya Silver is identifying a cluster of mineralized veins in proximity to the Angus Vein discovery, often in intersecting orientations, which is similar and comparable to other major historical mines in the Cobalt camp.
安大略省多倫多--(Newsfile Corp.,2024 年 1 月 11 日)——Kuya Silver Corporation(CSE:KUYA)(場外交易代碼:KUYAF)(FSE:6MR1)(the”公司“或”庫亞·西爾弗“)很高興在其全資Silver Kings項目的基層坎貝爾-克勞福德目標區域公佈鑽石鑽探項目的第一份化驗結果,2023年3月的鑽探在新的基層礦脈結構中與高品位銀相交。給出了從 23-SK-14 到 -26 個鑽孔的結果;在該項目中,總共完成了 18 個 NQ 定向鑽孔(23-SK-14 至 -31 個),總鑽孔總長度爲 5,834 米。通過在該目標區域進行更多金剛石鑽探,Kuya Silver正在安格斯礦脈發現附近發現一組礦化礦脈,這些礦脈通常是相交方向,與鈷礦營地中的其他主要歷史礦山相似和可比。
Highlights:
亮點:
- Diamond drilling was focused on defining the geometry and grade of mineralized structures in the Campbell-Crawford area, following up on the March 2023 grassroots Angus Vein drill intercept of 15,372 g/t silver over 3.34 m
- Six major, variably-mineralized and traceable veins were intersected in drilling, plus secondary veins, with dominantly E-W, NW-SE and NNE-SSW trends
- Up to seven mineralized veins intersected per drill hole
- Veins commonly bend and pinch and swell along trend, and high-grade mineralization is commonly localized in these bends and at (or near) vein intersections
- Drilling tested a relatively restricted subsurface area of approximately 1.7 ha (130 x 130 square meters) within the ideal mineralized horizon at depth. The total size of the Campbell-Crawford and Airgiod properties is 41.8 ha
- Results from the newly-recognized Toms Vein include 2,180 g/t (70 oz/t) silver, 0.36% cobalt (2,315 g/t AgEq*) over 0.40 m in hole 23-SK-26 within a wider mineralized zone assaying 199 g/t (6.4 oz/t) silver, 0.02% cobalt (208 g/t AgEq*) over 7.00 m
- Original Angus Vein silver intersection from hole 23-SK-08 (15,372 g/t silver over 3.34 m) traced 70 m deeper with cobalt-rich intercept in hole 23-SK-20 from 314.79 m, with 8.70 g/t silver, 0.26% cobalt over 2.41 m (108 g/t AgEq*; from 314.79 m), including 24 g/t silver, 0.85% cobalt over 0.45 m (342.43 g/t AgEq*)
- Six drill holes from Campbell-Crawford and Airgiod target areas are pending
- Visible silver and/or cobalt mineralization observed in all remaining drill holes
- 金剛石鑽探的重點是確定坎貝爾-克勞福德地區礦化結構的幾何形狀和品位,這是繼2023年3月安格斯脈基層鑽探在3.34 m上截獲15,372克/噸白銀的後續行動
- 鑽探中橫穿了六條主要的、礦化程度可變且可追溯的礦脈,外加次生礦脈,主要是東南、西北和西南和新南偏南的趨勢
- 每個鑽孔最多有七條礦化礦脈相交
- 礦脈通常會彎曲、擠壓並沿着趨勢膨脹,而高品位礦化通常侷限於這些彎道和礦脈交叉點(或附近)處
- 鑽探測試了在理想的礦化地層深度內相對有限的地下區域,約爲 1.7 公頃(130 x 130 平方米)。坎貝爾-克勞福德和艾爾吉德房產的總面積爲41.8公頃
- 新發現的 Toms Vein 的結果包括 2,180 g/t(70 oz/t)銀、0.36% 的鈷(2,315 g/t AgeQ*),在更寬的礦化區內測出 199 g/t(6.4 oz/t)銀,0.02% 的鈷(208 g/t AgeQ*),超過 7.00 m 的 0.02% 鈷(208 g/t AgeQ*)23-SK-26
- 23-SK-08 孔(超過 3.34 m 的 15,372 g/t 銀)的原始安格斯靜脈銀交叉點追溯到 70 米深,從 314.79 米處的 23-SK-20 孔中富含鈷的截距,8.70 g/t 銀,0.26% 的鈷 2.41 m(108 g/t AgeQ*;從 314.79 m 開始),包括 24 g/t 銀,0.45 m(342.43 g/t AgeQ*)上的 0.85% 鈷 *)
- 來自坎貝爾-克勞福德和艾爾吉德目標區域的六個鑽孔正在等待中
- 在所有剩餘的鑽孔中觀察到可見的銀和/或鈷礦化
David Lewis, Vice President Exploration, commented: "When we first drilled the Angus Vein in March, 2023, there was no doubt about the buried potential for new economic deposits at the Campbell-Crawford property. We have now begun defining at least six E-W and NW-SE trending mineralized veins, plus smaller secondary veins, within a very tight area, and hints of other major veins have also been drilled. We are observing higher-grade silver and cobalt mineralization focused near flexed vein intersections, defining steep, cigar shaped mineralized shoots, and there is potential at each of these major vein intersections for additional mineralized shoots. The remaining six drill holes were designed to follow up on the main Angus Vein intersection but also include one hole testing the Airgiod property at depth and all intersected visible silver and/or cobalt mineralization. Both the Campbell-Crawford and Airgiod areas remain extremely promising and high-priority exploration targets for Kuya Silver."
勘探副總裁戴維·劉易斯評論說:“當我們在2023年3月首次鑽探安格斯礦脈時,毫無疑問,坎貝爾-克勞福德地產蘊藏着新的經濟礦牀的潛力。現在,我們已經開始在非常狹窄的區域內定義至少六條東北和西北偏向礦化礦脈,以及較小的次生礦脈,並且還鑽探了其他主要礦脈的線索。我們正在觀察到更高品位的銀和鈷礦化聚焦在彎曲的礦脈交叉點附近,形成了陡峭的雪茄形礦化枝條,並且這些主要礦脈交叉點都有可能出現額外的礦化枝條。其餘六個鑽孔旨在跟蹤安格斯礦脈的主要交叉點,但也包括一個深度測試Airgiod特性的鑽孔,以及所有相交的可見銀和/或鈷礦化。坎貝爾-克勞福德和艾爾吉德地區仍然是Kuya Silver極具前景和高度優先的勘探目標。”
Hole ID | From | To | Length | Ag | Co | AgEq* (g/t) | Interpreted Mineralization |
(m) | (m) | (m) | g/t | % | Ag, Co only | ||
23-SK-14 | 285.47 | 285.87 | 0.40 | 70 | 0.81 | 371 | Toms Vein |
23-SK-15 | 286.77 | 287.17 | 0.40 | 11 | 0.26 | 108 | Toms Vein |
23-SK-19 (BMZ) | 283.00 | 283.83 | 0.83 | 143 | 0.23 | 228 | New NW Vein, 0.24% copper, 0.61% lead |
23-SK-19 (BMZ) | 287.52 | 287.92 | 0.40 | 174 | 0.60 | 399 | New NW Vein |
23-SK-19 (BMZ) | 289.00 | 289.40 | 0.40 | 13 | 0.39 | 158 | New NW Vein |
23-SK-20 | 182.50 | 183.33 | 0.83 | 1 | 0.42 | 159 | New E-W Vein (Diabase hosted) |
23-SK-20 (BMZ) | 302.00 | 303.00 | 1.00 | 98 | 0.25 | 190 | Angus Vein zone, 2% copper, 1% lead, 1% zinc |
23-SK-20 (BMZ) | 316.35 | 316.80 | 0.45 | 24 | 0.85 | 342 | Angus Vein |
23-SK-24 (BMZ) | 258.72 | 259.12 | 0.40 | 220 | 0.01 | 225 | Jones 3 Vein |
23-SK-25 (BMZ) | 287.70 | 288.10 | 0.40 | 27 | 0.30 | 138 | New NW Vein |
23-SK-25 | 319.80 | 320.40 | 0.60 | 422 | 0.01 | 426 | Angus Vein |
23-SK-26 | 253.00 | 260.00 | 7.00 | 199* | 0.02 | 208 | Toms Vein zone |
Including | 253.00 | 254.00 | 1.00 | 296 | 0.00 | 297 | Toms Vein zone |
Including | 257.60 | 258.00 | 0.40 | 2180* | 0.36 | 2,315 | Toms Vein |
Hole ID | 來自 | 到 | 長度 | Ag | 有限公司 | ageQ* (g/t) | 解讀礦化 |
(m) | (m) | (m) | g/t | % | 僅限 Ag、Co | ||
23-SK-14 | 285.47 | 285.87 | 0.40 | 70 | 0.81 | 371 | Toms Vein |
23-SK-15 | 286.77 | 287.17 | 0.40 | 11 | 0.26 | 108 | Toms Vein |
23-SK-19 (BMZ) | 283.00 | 283.83 | 0.83 | 143 | 0.23 | 228 | 全新 NW Vein,0.24% 銅,0.61% 鉛 |
23-SK-19 (BMZ) | 287.52 | 287.92 | 0.40 | 174 | 0.60 | 399 | 全新 NW Vein |
23-SK-19 (BMZ) | 289.00 | 289.40 | 0.40 | 13 | 0.39 | 158 | 全新 NW Vein |
23-SK-20 | 182.50 | 183.33 | 0.83 | 1 | 0.42 | 159 | 新的 E-W Vein(由 Diabase 託管) |
23-SK-20 (BMZ) | 302.00 | 303.00 | 1.00 | 98 | 0.25 | 190 | 安格斯靜脈區,2% 銅,1% 鉛,1% 鋅 |
23-SK-20 (BMZ) | 316.35 | 316.80 | 0.45 | 24 | 0.85 | 342 | 安格斯·維恩 |
23-SK-24 (BMZ) | 258.72 | 259.12 | 0.40 | 220 | 0.01 | 225 | 瓊斯 3 Vein |
23-SK-25 (BMZ) | 287.70 | 288.10 | 0.40 | 27 | 0.30 | 138 | 全新 NW Vein |
23-SK-25 | 319.80 | 320.40 | 0.60 | 422 | 0.01 | 426 | 安格斯·維恩 |
23-SK-26 | 253.00 | 260.00 | 7.00 | 199* | 0.02 | 208 | 湯姆斯靜脈區 |
包括 | 253.00 | 254.00 | 1.00 | 296 | 0.00 | 297 | 湯姆斯靜脈區 |
包括 | 257.60 | 258.00 | 0.40 | 2180* | 0.36 | 2,315 | Toms Vein |
Table 1: Significant silver and cobalt mineralization intersected in the Phase 2 2023 drill program at the Campbell-Crawford target area. Results from the first twelve drill holes (23-SK-14 to -26) are presented, with the remaining six pending. AgEq* (silver equivalent) grades were calculated using $23.69 USD / oz silver and $28,500 USD / tonne cobalt, with metal prices captured on January 2, 2024. Mineralized drilling intervals do not reflect true interval length. "BMZ" refers to mineralization within a Broader Mineralized Zone. *Assaying by Screened Metallics was conducted on high-grade, visually identified silver mineralization in hole 23-SK-26 between 256.80 m to 258.80 m. See Appendix A for full significant and anomalous assay results.
表 1:在坎貝爾-克勞福德目標區域的 2023 年第二階段鑽探計劃中,顯著的銀和鈷礦化相交。提供了前十二個鑽孔(23-SK-14 至 -26)的結果,其餘六個待定。AgeQ*(白銀當量)等級是使用23.69美元/盎司白銀和28,500美元/噸鈷計算得出的,金屬價格是在2024年1月2日公佈的。礦化鑽探間隔不能反映真實的間隔長度。“BMZ” 是指更廣泛的礦化區內的礦化。*Screened Metallics 的化驗是在 256.80 m 至 258.80 m 之間的 23-SK-26 孔中對高品位的、目視識別的銀礦化層進行的。有關完整的顯著和異常分析結果,請參閱附錄 A。
Figure 1: Plan map of the 2023 Phase 2 diamond drilling at the Campbell-Crawford and Airgiod target areas, Silver Kings Project.
圖 1:銀王項目在 Campbell-Crawford 和 Airgiod 目標區域進行的 2023 年第二階段鑽石鑽探計劃圖。
Campbell-Crawford Drilling Expanded
坎貝爾-克勞福德鑽探範圍擴大
Drilling at the Campbell-Crawford target area has successfully identified at least six steeply-dipping silver-cobalt mineralized veins with significant lateral and vertical extent at depth, as well as a variety of secondary mineralized veins (Table 1; Figure 1). The veins cut both the basal Archean volcano-sedimentary rocks and the overlying Nipissing Diabase sill (exposed on surface to 200+ m depth), but the mineralization increases dramatically below this rock contact. These steep silver-cobalt veins include the previously-recognized E-W trending Angus and McNamara veins, as well as four newly-identified NW-SE trending veins, including the Toms, Jones 1, Jones 2 and Jones 3 veins. A significant number of secondary mineralized veins, typically drilled near flexures or intersections of the major veins, were also intersected.
在Campbell-Crawford目標區域的鑽探成功地發現了至少六條陡峭的銀鈷礦化礦脈,這些礦脈深度具有顯著的橫向和垂直範圍,以及各種次生礦化礦脈(表1;圖1)。這些礦脈既切斷了太古代火山沉積岩的底層,也切開了上覆的尼皮辛輝綠岩基岩(暴露在地表深度超過200米),但礦化作用在岩石接觸下方急劇增加。這些陡峭的銀鈷礦脈包括先前認可的E-W趨勢安格斯和麥克納馬拉靜脈,以及四條新發現的NW-SE趨勢靜脈,包括湯姆斯、瓊斯1號、瓊斯2號和瓊斯3號靜脈。大量次生礦化礦脈也相交,這些礦脈通常鑽探在主要礦脈的彎曲處或交叉點附近。
High-grade silver and cobalt mineralization is largely restricted to the mineralized veins, but minor haloed intervals can also occur in the surrounding wall rock. Based on the initial six drill holes from the early 2023 drill program (23-SK-07 to -13), mineralization was interpreted to follow the shallowly-dipping lower diabase contact; further drilling now shows that mineralization plunges steeply in both E-W and NW-SE veins. Currently, high-grade zones are known near vein intersections and in vein flexures, only one of which has now been properly tested, and the basal Archean rock geometry also likely affects veining. Historically, in the Cobalt mining camp, clusters of closely-spaced mineralized vein structures with different orientations have the potential to host larger (i.e. >5 million ounce silver plus cobalt) deposits.
高品位的銀和鈷礦化在很大程度上僅限於礦化礦脈,但周圍的壁巖中也可能出現細微的光暈間隔。根據2023年初鑽探計劃(23-SK-07 至 -13)中最初的六個鑽孔,礦化被解釋爲沿着淺層的低輝綠岩接觸;現在的進一步鑽探表明,東北和西北-SE礦脈的礦化作用急劇下降。目前,已知在靜脈交叉點附近和靜脈彎曲處有高等級區域,目前只有一個區域經過了適當的測試,基礎太古代岩石的幾何形狀也可能會影響脈脈。從歷史上看,在 Cobalt 採礦營地中,間隔緊密、方向不同的礦化礦脈結構群有可能容納更大的(即 >500 萬盎司的銀(加鈷)礦牀。
The basal Archean rocks, located beneath the Nipissing Diabase sheet, consist of mafic volcanic, volcaniclastic, interflow sedimentary, and felsic intrusive rocks. The sedimentary rocks, which are traceable between drillholes, are highly enriched in base metal sulphides, and mineralized silver-cobalt veins are clearly influenced by these interflow sulphide zones. The sulphides, which locally grade up to several percent copper, lead and/or zinc, are also locally enriched in arsenic, silver and cobalt. The silver-cobalt veins frequently cut these interflow sedimentary rocks, but the relationship between the veins and sulphidized sedimentary rocks remains unclear.
基底太古巖位於尼皮辛輝綠岩層之下,由鎂鐵質火山、火山碎片、間流沉積岩和長英質侵入岩組成。沉積岩可追溯到鑽孔之間,富含基本金屬硫化物,礦化的銀鈷礦脈顯然受到這些硫化物間流帶的影響。這些硫化物的局部品位高達百分之幾的銅、鉛和/或鋅,當地還富含砷、銀和鈷。銀鈷礦脈經常切割這些互流沉積岩,但這些礦脈與硫化沉積岩之間的關係仍不清楚。
Drill Program Details and Interpretations
演習計劃詳情和解釋
Hole ID | Drill Pad | Drill Targets | Drill Intersections | Depth | Sample width | Comments |
m | m | |||||
23-SK-14 | 23-SK-13 | McNamara, Angus Vein at diabase contact | McNamara Vein | 140.00 | 0.58 | Weakly mineralized in diabase |
Angus Vein | 218.45 | 0.45 | Weakly mineralized in diabase | |||
Toms Vein | 285.47 | 0.40 | Strong cobalt mineralization | |||
23-SK-15 | 23-SK-13 | McNamara, Angus Vein at diabase contact, Toms Vein | McNamara Vein | 154.40 | 0.40 | Weakly mineralized in diabase |
Angus Vein | 235.62 | 0.56 | Moderately mineralized in diabase | |||
Toms Vein | 286.77 | 0.40 | Moderate cobalt mineralization | |||
23-SK-16 | 25m W 23-SK-13 | McNamara, Angus veins | McNamara Vein | 156.77 | 0.40 | Weakly mineralized in diabase |
Toms Vein | 207.60 | 0.40 | Weakly mineralized in diabase | |||
Angus Vein (?) | 247.70 | 0.50 | Weakly mineralized in diabase | |||
23-SK-17 | 25m W 23-SK-13 | McNamara, Angus veins | McNamara Vein | 176.40 | N/A | Weakly mineralized in diabase |
23-SK-18 | 50m W 23-SK-13 | McNamara, Angus veins | Toms Vein | 132.63 | 0.42 | Anomalously mineralized in diabase |
23-SK-19 | 23-SK-13 | McNamara, Angus veins | McNamara Vein | 157.00 | 1.00 | Weakly mineralized in diabase |
Angus Vein | 203.98 | 0.40 | Weakly mineralized in diabase | |||
NW Vein 1 | 283.00 | 0.83 | Significantly mineralized | |||
NW Vein 2 | 286.00 | 1.00 | Anomalously mineralized 50 cm wide vein (estimated true thickness) | |||
NW Vein 3 | 287.52 | 0.40 | Significantly mineralized | |||
NW Vein 4 | 289.00 | 0.40 | Significantly mineralized | |||
NW Vein 5 | 320.85 | 0.45 | Significantly mineralized | |||
NW Vein 6 | 328.00 | 2.56 | Weakly mineralized, vein along core axis | |||
NW Vein 7 | 334.20 | 0.60 | Anomalously mineralized | |||
23-SK-20 | 50m N 23-SK-13 | McNamara, Angus veins | E-W Vein | 182.50 | 0.83 | Moderately mineralized in diabase |
McNamara Vein | 258.64 | 3.36 | Anomalously mineralized faulted zone | |||
Base metal | 302.00 | 1.00 | Blebby copper zone | |||
Angus Vein | 314.79 | 2.41 | Moderately mineralized | |||
23-SK-21 | 50m N 23-SK-13 | McNamara, Angus veins | McNamara Vein | 190.60 | 0.80 | Weakly mineralized in diabase |
Angus Vein | 253.93 | 0.42 | Weakly mineralized in diabase | |||
23-SK-22 | 25m W 23-SK-13 | Vein cluster in hole 23-SK-19 | McNamara Vein | 143.00 | 0.40 | Moderately mineralized in diabase |
Angus Vein | 154.30 | 0.40 | Weakly mineralized in diabase | |||
23-SK-23 | 25m E 23-SK-13 | Angus/Toms intersection | McNamara Vein | 249.15 | 0.40 | Anomalously mineralized, drilled north of intersection |
Toms Vein | 274.59 | 0.41 | Moderately mineralized, drilled north of intersection | |||
23-SK-24 | 200m ENE 23-SK-13 | Drill beneath diabase, transect zone | Jones 3 vein A | 255.17 | 0.40 | Moderately mineralized |
Jones 3 vein B | 257.35 | 0.40 | Moderately mineralized | |||
Jones 3 vein C | 258.72 | 0.40 | Significantly mineralized | |||
Jones 2 Vein | 271.28 | 0.40 | Anomalously mineralized | |||
McNamara Vein | 293.90 | 0.70 | Moderately mineralized | |||
23-SK-25 | 200m ENE 23-SK-13 | Drill beneath diabase, transect zone, target Angus/Toms intersection | Jones 3 Vein | 255.60 | 0.50 | Anomalously mineralized |
Jones 2 Vein | 287.70 | 0.40 | Moderately mineralized | |||
Jones 1 Vein | 297.40 | 0.40 | Moderately mineralized | |||
Angus Vein | 319.80 | 0.60 | Significantly mineralized | |||
23-SK-26 | 130 m E 23-SK-13 | Drill beneath diabase, transect zone, target Angus/Toms intersection | Jones 2 Vein | 189.35 | 0.40 | Anomalously mineralized |
Toms Vein | 257.60 | 0.40 | Highly mineralized |
Hole ID | 鑽墊 | 鑽探目標 | 鑽孔十字路口 | 深度 | 樣本寬度 | 評論意見 |
m | m | |||||
23-SK-14 | 23-SK-13 | 麥克納馬拉、安格斯·韋恩和輝綠岩接觸 | McNamara Vein | 140.00 | 0.58 | 輝綠岩中弱礦化 |
安格斯·維恩 | 218.45 | 0.45 | 輝綠岩中弱礦化 | |||
Toms Vein | 285.47 | 0.40 | 強烈的鈷礦化 | |||
23-SK-15 | 23-SK-13 | McNamara、Angus Vein 和 diabase 接觸處、Toms Vein | McNamara Vein | 154.40 | 0.40 | 輝綠岩中弱礦化 |
安格斯·維恩 | 235.62 | 0.56 | 輝綠岩中呈中度礦化 | |||
Toms Vein | 286.77 | 0.40 | 中度鈷礦化 | |||
23-SK-16 | 25m W 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | McNamara Vein | 156.77 | 0.40 | 輝綠岩中弱礦化 |
Toms Vein | 207.60 | 0.40 | 輝綠岩中弱礦化 | |||
安格斯·維恩(?) | 247.70 | 0.50 | 輝綠岩中弱礦化 | |||
23-SK-17 | 25m W 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | McNamara Vein | 176.40 | 不適用 | 輝綠岩中弱礦化 |
23-SK-18 | 50m W 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | Toms Vein | 132.63 | 0.42 | 輝綠岩中異常礦化 |
23-SK-19 | 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | McNamara Vein | 157.00 | 1.00 | 輝綠岩中弱礦化 |
安格斯·維恩 | 203.98 | 0.40 | 輝綠岩中弱礦化 | |||
西北靜脈 1 | 283.00 | 0.83 | 顯著礦化 | |||
NW Vein 2 | 286.00 | 1.00 | 異常礦化 50 厘米寬的礦脈(估計的真實厚度) | |||
NW Vein 3 | 287.52 | 0.40 | 顯著礦化 | |||
NW Vein 4 | 289.00 | 0.40 | 顯著礦化 | |||
NW Vein 5 | 320.85 | 0.45 | 顯著礦化 | |||
NW Vein 6 | 328.00 | 2.56 | 弱礦化,沿着核心軸線的靜脈 | |||
NW Vein 7 | 334.20 | 0.60 | 異常礦化 | |||
23-SK-20 | 50m N 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | E-W 靜脈 | 182.50 | 0.83 | 輝綠岩中呈中度礦化 |
McNamara Vein | 258.64 | 3.36 | 異常礦化斷層帶 | |||
賤金屬 | 302.00 | 1.00 | Blebby 銅區 | |||
安格斯·維恩 | 314.79 | 2.41 | 中度礦化 | |||
23-SK-21 | 50m N 23-SK-13 | 麥克納馬拉,安格斯·維恩斯 | McNamara Vein | 190.60 | 0.80 | 輝綠岩中弱礦化 |
安格斯·維恩 | 253.93 | 0.42 | 輝綠岩中弱礦化 | |||
23-SK-22 | 25m W 23-SK-13 | 孔內靜脈群 23-SK-19 | McNamara Vein | 143.00 | 0.40 | 輝綠岩中呈中度礦化 |
安格斯·維恩 | 154.30 | 0.40 | 輝綠岩中弱礦化 | |||
23-SK-23 | 25m E 23-SK-13 | 安格斯/湯姆斯十字路口 | McNamara Vein | 249.15 | 0.40 | 異常礦化,在十字路口以北鑽探 |
Toms Vein | 274.59 | 0.41 | 中度礦化,在十字路口以北鑽探 | |||
23-SK-24 | 200m ENE 23-SK-13 | 在輝綠岩下鑽孔,橫斷區 | 瓊斯 3 靜脈 A | 255.17 | 0.40 | 中度礦化 |
瓊斯 3 靜脈 B | 257.35 | 0.40 | 中度礦化 | |||
瓊斯 3 靜脈 C | 258.72 | 0.40 | 顯著礦化 | |||
Jones 2 Vein | 271.28 | 0.40 | 異常礦化 | |||
McNamara Vein | 293.90 | 0.70 | 中度礦化 | |||
23-SK-25 | 200m ENE 23-SK-13 | 鑽探輝綠岩下方、橫斷區、目標安格斯/湯姆斯交叉點 | 瓊斯 3 Vein | 255.60 | 0.50 | 異常礦化 |
Jones 2 Vein | 287.70 | 0.40 | 中度礦化 | |||
瓊斯 1 Vein | 297.40 | 0.40 | 中度礦化 | |||
安格斯·維恩 | 319.80 | 0.60 | 顯著礦化 | |||
23-SK-26 | 130 m E 23-SK-13 | 鑽探輝綠岩下方、橫斷區、目標安格斯/湯姆斯交叉點 | Jones 2 Vein | 189.35 | 0.40 | 異常礦化 |
Toms Vein | 257.60 | 0.40 | 高度礦化 |
Table 2: Description of drill targeting and mineralized results for drill holes 23-SK-14 to 23-SK-26. Sample widths do not reflect true thickness of mineralization.
表 2:23-SK-14 至 23-SK-26 鑽孔的鑽探目標和礦化結果的描述。樣本寬度不能反映礦化的真實厚度。
The 2023 Phase 2 drill program was divided into several stages of work. Early drill holes (23-SK-14 to -20) were designed as step-out drill holes to the original major drilling intersections (23-SK-08 and -13; see Kuya Silver May 30, 2023 news release) in order to test vein continuity (both vertically and along trend). The first drill hole in the program, 23-SK-14, used the same pad as hole 23-SK-13, but the hole was drilled more shallowly. Drilling step-outs were designed to be on 25 m centers, both to the east and the west of this original pad, and multiple holes per pad were drilled with different dips. Later drill holes (23-SK-21 to -29) were designed to test vein intersections in progressively more detail. Hole 23-SK-30 was designed to test beneath Cyril Lake (Figure 1), an interpreted fault valley, and hole 23-SK-31, originally designed as a wedged hole from 23-SK-08, had to be drilled as an infill hole from surface when the wedge failed and jammed in hole 23-SK-08. A summary of drilling, including drill targets and results, is presented in Table 2 and drill hole coordinates and orientations are presented in Table 3.
2023 年第 2 階段的鑽探計劃分爲幾個工作階段。早期的鑽孔(23-SK-14 至 -20)被設計爲通往原始主要鑽探交叉點(23-SK-08 和 -13;參見 Kuya Silver 2023 年 5 月 30 日新聞稿)的階出式鑽孔,目的是測試礦脈連續性(垂直和沿趨勢)。程序中的第一個鑽孔 23-SK-14 使用了與 23-SK-13 孔相同的墊層,但鑽得更淺一些。鑽孔臺階設計在 25 米的中心位置,位於該原始鑽井平台的東部和西部,並且每個墊層鑽了多個具有不同傾角的孔。後來的鑽孔(23-SK-21 至 -29)被設計用於更詳細地測試靜脈交叉點。23-SK-30 孔設計用於在西里爾湖(圖 1)下進行測試,後者是一個經過解釋的斷層谷,而 23-SK-31 孔最初設計爲 23-SK-08 的楔形孔,當楔子失效並卡在孔 23-SK-08 中時,必須從地表鑽出填充孔。鑽探摘要,包括鑽探目標和結果,見表 2,鑽孔座標和方向,見表 3。
In the late stages of the drilling program, a borehole optical televiewer was used in five drill holes (23-SK-08, -18, -19, -29 and -31) to establish and/or verify vein orientations from the oriented drill core program. This work was performed by DGI Geoscience Inc. based in Toronto, Ontario. Currently, data from two drill holes (23-SK-08 and -19) has been returned.
在鑽探計劃的後期階段,在五個鑽孔(23-SK-08、-18、-19、-29 和 -31)中使用了鑽孔光學電視監視器,以確定和/或驗證定向鑽芯計劃中的礦脈方向。這項工作由總部位於安大略省多倫多的DGI Geoscience Inc.完成。目前,來自兩個鑽孔(23-SK-08 和 -19)的數據已經返回。
Hole ID | Easting | Northing | Elevation (mASL) | Depth (m) | Azimuth | Dip |
23-SK-14 | 601853 | 5248957 | 340 | 291 | 185 | -66 |
23-SK-15 | 601853 | 5248964 | 340 | 303 | 185 | -66 |
23-SK-16 | 601827 | 5248953 | 340 | 264 | 185 | -70 |
23-SK-17 | 601827 | 5248953 | 340 | 306 | 185 | -72 |
23-SK-18 | 601801 | 5248956 | 338 | 315 | 185 | -72 |
23-SK-19 | 601852 | 5248965 | 341 | 339 | 165 | -68 |
23-SK-20 | 601856 | 5249010 | 339 | 330 | 185 | -65 |
23-SK-21 | 601856 | 5249010 | 339 | 315 | 182 | -56 |
23-SK-22 | 601827 | 5248951 | 340 | 348 | 152 | -66 |
23-SK-23 | 601875 | 5248971 | 337 | 300 | 206 | -68 |
23-SK-24 | 602041 | 5249027 | 273 | 396 | 239 | -40 |
23-SK-25 | 602041 | 5249026 | 273 | 384 | 230 | -40 |
23-SK-26 | 601973 | 5248980 | 293 | 321 | 230 | -46 |
23-SK-27 | 601973 | 5248980 | 293 | 300 | 228 | -48 |
23-SK-28 | 601974 | 5248980 | 293 | 285 | 235 | -48 |
23-SK-29 | 601974 | 5248981 | 293 | 327 | 221 | -52 |
23-SK-30 | 601609 | 5248859 | 306 | 450 | 350 | -69 |
23-SK-31 | 601832 | 5248787 | 338 | 257 | 4 | -70 |
Hole ID | 向東 | 北方 | 海拔 (masL) | 深度 (m) | 方位角 | 浸 |
23-SK-14 | 601853 | 5248957 | 340 | 291 | 185 | -66 |
23-SK-15 | 601853 | 5248964 | 340 | 303 | 185 | -66 |
23-SK-16 | 601827 | 5248953 | 340 | 264 | 185 | -70 |
23-SK-17 | 601827 | 5248953 | 340 | 306 | 185 | -72 |
23-SK-18 | 601801 | 5248956 | 338 | 315 | 185 | -72 |
23-SK-19 | 601852 | 5248965 | 341 | 339 | 165 | -68 |
23-SK-20 | 601856 | 5249010 | 339 | 330 | 185 | -65 |
23-SK-21 | 601856 | 5249010 | 339 | 315 | 182 | -56 |
23-SK-22 | 601827 | 5248951 | 340 | 348 | 152 | -66 |
23-SK-23 | 601875 | 5248971 | 337 | 300 | 206 | -68 |
23-SK-24 | 602041 | 5249027 | 273 | 396 | 239 | -40 |
23-SK-25 | 602041 | 5249026 | 273 | 384 | 230 | -40 |
23-SK-26 | 601973 | 5248980 | 293 | 321 | 230 | -46 |
23-SK-27 | 601973 | 5248980 | 293 | 300 | 228 | -48 |
23-SK-28 | 601974 | 5248980 | 293 | 285 | 235 | -48 |
23-SK-29 | 601974 | 5248981 | 293 | 327 | 221 | -52 |
23-SK-30 | 601609 | 5248859 | 306 | 450 | 350 | -69 |
23-SK-31 | 601832 | 5248787 | 338 | 257 | 4 | -70 |
Table 3: Collar coordinates and drill orientations from the 2023 Campbell-Crawford and Airgiod area Phase 2 drilling. All units are in meters and coordinates are presented in UTM NAD83 Zone 17N.
表 3:2023 年坎貝爾-克勞福德和艾爾吉德地區第二階段鑽探的環座標和鑽探方向。所有單位均以米爲單位,座標以 UTM NAD83 區域 17N 表示。
Quality Assurance and Quality Control
質量保證和質量控制
The drill core samples were logged and sampled with limestone blank material and standard reference material added in sample sequence and/or following visual identification of silver or cobalt mineralization. The samples were cut perpendicular to veining by core saw and were secured in labelled vinyl sample bags. Samples were shipped to AGAT Laboratories in Timmins, Ontario, where they were weighed, crushed and pulverized.
鑽芯樣本是在樣品序列中添加石灰石空白材料和標準參考材料和/或目視識別銀或鈷礦化後進行記錄和採樣的。樣品由芯鋸垂直於脈紋切割,並固定在貼有標籤的乙烯基樣品袋中。樣本被運往安大略省蒂明斯的AGAT實驗室,在那裏進行稱重、壓碎和粉碎。
At AGAT Labs (Calgary, Alberta), samples were digested by 4-acid and analyzed by ICP-OES (maximum undiluted detection limit of 500 g/t silver).
在AGAT實驗室(艾伯塔省卡爾加里),樣品經四酸消化,然後由ICP-OES進行分析(最大未稀釋檢出限爲500 g/t銀)。
At SGS Labs (Lakefield, Ontario), samples were processed by 500 g Screened Metallics. This method is suitable for coarse native metals (e.g. gold, silver, copper, palladium and platinum) with no upper detection limit. Samples were screened to 106 microns and fire assayed.
在 SGS 實驗室(安大略省萊克菲爾德),樣品由 500 g 篩選金屬進行處理。該方法適用於粗糙的原生金屬(例如金、銀、銅、鈀和鉑),沒有檢出上限。對樣本進行了篩查至106微米並進行了火災檢驗。
When samples were analyzed for silver by both ICP-AES and Screened Metallics, the Screened Metallics results are presented. A single QA/QC standard processed by Screened Metallics returned a value below two standard deviations for silver; all other QA/QC standards were acceptable and within two standard deviations of certified values.
當使用ICP-AES和篩選金屬對樣品進行銀分析時,會顯示篩選金屬的結果。Screened Metallics處理的單一質量保證/質量控制標準返回的值低於銀的兩個標準差;所有其他質量保證/質量控制標準均可接受,且在認證值的兩個標準差以內。
National Instrument 43-101 Disclosure
國家儀器 43-101 披露
The technical content of this news release has been reviewed and approved by Mr. David Lewis, P.Geo., Vice President Exploration of Kuya Silver and a Qualified Person as defined by National Instrument 43-101.
本新聞稿的技術內容已由P.Geo大衛·劉易斯先生、Kuya Silver勘探副總裁和National Instrument 43-101定義的合格人員的審查和批准。
About Kuya Silver Corporation
關於 Kuya Silver 公司
Kuya Silver is a Canadian‐based mineral exploration and development company with a focus on acquiring, exploring, and advancing precious metals assets in Peru and Canada.
Kuya Silver是一家總部位於加拿大的礦產勘探和開發公司,專注於收購、勘探和開發秘魯和加拿大的貴金屬資產。
For more information, please contact:
欲了解更多信息,請聯繫:
David Stein, President and Chief Executive Officer
Telephone: (604) 398‐4493
info@kuyasilver.com
大衛·斯坦,總裁兼首席執行官
電話:(604) 398-4493
info@kuyasilver.com
Reader Advisory
讀者諮詢
This news release contains statements that constitute "forward-looking information," including statements regarding the plans, intentions, beliefs, and current expectations of the Company, its directors, or its officers with respect to the future business activities of the Company. The words "may," "would," "could," "will," "intend," "plan," "anticipate," "believe," "estimate," "expect," "must," "next," "propose," "new," "potential," "prospective," "target," "future," "verge," "favourable," "implications," and "ongoing," and similar expressions, as they relate to the Company or its management, are intended to identify such forward-looking information. Investors are cautioned that statements including forward-looking information are not guarantees of future business activities and involve risks and uncertainties, and that the Company's future business activities may differ materially from those described in the forward-looking information as a result of various factors, including but not limited to fluctuations in market prices, successes of the operations of the Company, continued availability of capital and financing, and general economic, market, and business conditions. There can be no assurances that such forward-looking information will prove accurate, and therefore, readers are advised to rely on their own evaluation of the risks and uncertainties. The Company does not assume any obligation to update any forward-looking information except as required under the applicable securities laws.
本新聞稿包含構成 “前瞻性信息” 的陳述,包括有關公司、其董事或高級管理人員對公司未來業務活動的計劃、意圖、信念和當前預期的陳述。“可能”、“將”、“可能”、“將”、“打算”、“計劃”、“預測”、“相信”、“估計”、“期望”、“必須”、“下一步”、“提議”、“新”、“潛在”、“目標”、“未來”、“邊緣”、“有利”、“影響” 和 “持續” 等詞語以及類似的表述,與公司或其管理層有關的,旨在識別此類前瞻性信息。投資者請注意,包括前瞻性信息在內的陳述不能保證未來的業務活動,涉及風險和不確定性,由於各種因素,包括但不限於市場價格的波動、公司經營的成功、資本和融資的持續可用性以及總體經濟、市場和業務狀況,公司的未來業務活動可能與前瞻性信息中描述的業務活動存在重大差異。無法保證此類前瞻性信息會被證明是準確的,因此,建議讀者依靠自己對風險和不確定性的評估。除非適用的證券法要求,否則公司不承擔任何更新任何前瞻性信息的義務。
Neither the Canadian Securities Exchange nor the Investment Industry Regulatory Organization of Canada accepts responsibility for the adequacy or accuracy of this release.
加拿大證券交易所和加拿大投資行業監管組織均不對本新聞稿的充分性或準確性承擔責任。
Hole ID | From | To | Length | Ag | Co | AgEq* (g/t) | Cu | Ni | Pb | Zn | Interpreted Mineralization | |
(m) | (m) | (m) | g/t | % | Ag, Co only | % | % | % | % | |||
Significant Mineralization | ||||||||||||
23-SK-14 | 285.47 | 285.87 | 0.40 | 70 | 0.81 | 371 | 0.12 | 0.01 | 0.14 | 0.08 | Toms Vein | |
23-SK-15 | 286.77 | 287.17 | 0.40 | 11 | 0.26 | 108 | 0.08 | 0.03 | 0.05 | 0.05 | Toms Vein | |
23-SK-19 (BMZ) | 283.00 | 283.83 | 0.83 | 143 | 0.23 | 228 | 0.24 | 0.04 | 0.61 | 0.38 | New NW Vein | |
23-SK-19 (BMZ) | 287.52 | 287.92 | 0.40 | 174 | 0.60 | 399 | 0.12 | 0.08 | 0.24 | 0.01 | New NW Vein | |
23-SK-19 (BMZ) | 289.00 | 289.40 | 0.40 | 13 | 0.39 | 158 | 0.01 | 0.02 | 0.03 | 0.26 | New NW Vein | |
23-SK-20 | 182.50 | 183.33 | 0.83 | 1 | 0.42 | 159 | 0.07 | 0.03 | 0.00 | 0.00 | New E-W Vein (Diabase hosted) | |
23-SK-20 (BMZ) | 302.00 | 303.00 | 1.00 | 98 | 0.25 | 190 | 2.02 | 0.03 | 0.87 | 1.25 | Angus Vein zone | |
23-SK-20 (BMZ) | 316.35 | 316.80 | 0.45 | 24 | 0.85 | 342 | 0.07 | 0.11 | 0.08 | 0.01 | Angus Vein | |
23-SK-24 (BMZ) | 258.72 | 259.12 | 0.40 | 220 | 0.01 | 225 | 0.04 | 0.01 | 0.04 | 0.05 | Jones 3 Vein | |
23-SK-25 (BMZ) | 287.70 | 288.10 | 0.40 | 27 | 0.30 | 138 | 0.04 | 0.02 | 0.00 | 0.00 | New NW Vein | |
23-SK-25 | 319.80 | 320.40 | 0.60 | 422 | 0.01 | 426 | 0.01 | 0.00 | 0.01 | 0.03 | Angus Vein | |
23-SK-26 | 253.00 | 260.00 | 7.00 | 199* | 0.02 | 208 | 0.02 | 0.01 | 0.04 | 0.02 | Toms Vein zone | |
Including | 253.00 | 254.00 | 1.00 | 296 | 0.00 | 297 | 0.01 | 0.01 | 0.03 | 0.03 | Toms Vein zone | |
Including | 257.60 | 258.00 | 0.40 | 2180* | 0.36 | 2,315 | 0.03 | 0.05 | 0.00 | 0.01 | Toms Vein | |
Anomalous Mineralization | ||||||||||||
23-SK-15 | 235.62 | 236.18 | 0.56 | 26 | 0.08 | 57 | 0.07 | 0.03 | 0.39 | 0.05 | Angus Vein (Diabase hosted) | |
23-SK-17 | 267.19 | 270.00 | 2.81 | 9 | 0.01 | 14 | 0.11 | 0.01 | 0.07 | 0.10 | Base metal zone | |
23-SK-17 | 272.00 | 282.96 | 10.96 | 19 | 0.00 | 20 | 0.18 | 0.00 | 0.55 | 0.31 | Base metal zone | |
23-SK-18 | 132.63 | 133.05 | 0.42 | 4 | 0.07 | 31 | 0.09 | 0.02 | 0.01 | 0.06 | Toms Vein (Diabase hosted) | |
23-SK-18 | 258.00 | 266.00 | 8.00 | 2 | 0.00 | 3 | 0.01 | 0.00 | 0.21 | 0.34 | Base metal zone | |
23-SK-18 | 289.00 | 315.00 | 26.00 | 6 | 0.00 | 8 | 0.07 | 0.00 | 0.35 | 0.40 | Base metal zone | |
23-SK-19 | 281.00 | 289.40 | 8.40 | 36 | 0.09 | 68 | 0.17 | 0.01 | 0.16 | 0.51 | New Vein zone | |
23-SK-19 | 320.85 | 321.30 | 0.45 | 81 | 0.01 | 83 | 0.47 | 0.01 | 3.01 | 1.29 | New E-W vein | |
23-SK-20 | 300.00 | 306.00 | 6.00 | 24 | 0.05 | 41 | 0.50 | 0.01 | 0.44 | 1.11 | Base metal zone | |
23-SK-20 | 314.79 | 317.20 | 2.41 | 9 | 0.26 | 108 | 0.04 | 0.06 | 0.03 | 0.02 | Angus Vein zone | |
Including | 315.65 | 316.35 | 0.70 | 6 | 0.25 | 98 | 0.01 | 0.04 | 0.01 | 0.01 | Angus Vein zone | |
23-SK-22 | 143.00 | 143.40 | 0.40 | 0 | 0.13 | 50 | 0.00 | 0.02 | 0.00 | 0.00 | McNamara Vein (Diabase hosted) | |
23-SK-22 | 335.60 | 336.50 | 0.90 | 30 | 0.01 | 33 | 0.08 | 0.01 | 1.55 | 0.59 | Base metal zone | |
23-SK-23 | 274.59 | 275.00 | 0.41 | 2 | 0.13 | 49 | 0.02 | 0.00 | 0.01 | 0.01 | Toms Vein | |
23-SK-23 | 281.60 | 285.00 | 3.40 | 6 | 0.00 | 7 | 0.04 | 0.00 | 0.31 | 0.31 | Base metal zone | |
23-SK-24 | 255.17 | 255.57 | 0.40 | 39 | 0.11 | 81 | 0.10 | 0.15 | 0.40 | 0.11 | New NW Vein | |
23-SK-24 | 256.95 | 259.12 | 2.17 | 76 | 0.01 | 81 | 0.05 | 0.01 | 0.03 | 0.04 | New NW Vein | |
23-SK-24 | 293.90 | 294.60 | 0.70 | 2 | 0.34 | 129 | 0.00 | 0.03 | 0.00 | 0.00 | McNamara Vein | |
23-SK-25 | 255.60 | 256.10 | 0.50 | 20 | 0.03 | 31 | 0.01 | 0.01 | 0.12 | 0.17 | New NW Vein | |
23-SK-25 | 266.00 | 267.00 | 1.00 | 20 | 0.08 | 49 | 0.00 | 0.04 | 0.19 | 0.03 | New NW Vein | |
23-SK-25 | 287.00 | 310.40 | 23.40 | 8 | 0.01 | 12 | 0.05 | 0.00 | 0.16 | 0.07 | Broad vein zone | |
Including | 297.40 | 297.80 | 0.40 | 12 | 0.12 | 55 | 0.03 | 0.01 | 0.08 | 0.15 | Ag/Co vein |
Hole ID | 來自 | 到 | 長度 | Ag | 有限公司 | ageQ* (g/t) | 銅 | Ni | 鉛 | 鋅 | 解讀礦化 | |
(m) | (m) | (m) | g/t | % | 僅限 Ag、Co | % | % | % | % | |||
顯著的礦化 | ||||||||||||
23-SK-14 | 285.47 | 285.87 | 0.40 | 70 | 0.81 | 371 | 0.12 | 0.01 | 0.14 | 0.08 | Toms Vein | |
23-SK-15 | 286.77 | 287.17 | 0.40 | 11 | 0.26 | 108 | 0.08 | 0.03 | 0.05 | 0.05 | Toms Vein | |
23-SK-19 (BMZ) | 283.00 | 283.83 | 0.83 | 143 | 0.23 | 228 | 0.24 | 0.04 | 0.61 | 0.38 | 全新 NW Vein | |
23-SK-19 (BMZ) | 287.52 | 287.92 | 0.40 | 174 | 0.60 | 399 | 0.12 | 0.08 | 0.24 | 0.01 | 全新 NW Vein | |
23-SK-19 (BMZ) | 289.00 | 289.40 | 0.40 | 13 | 0.39 | 158 | 0.01 | 0.02 | 0.03 | 0.26 | 全新 NW Vein | |
23-SK-20 | 182.50 | 183.33 | 0.83 | 1 | 0.42 | 159 | 0.07 | 0.03 | 0.00 | 0.00 | 新的 E-W Vein(由 Diabase 託管) | |
23-SK-20 (BMZ) | 302.00 | 303.00 | 1.00 | 98 | 0.25 | 190 | 2.02 | 0.03 | 0.87 | 1.25 | 安格斯靜脈區域 | |
23-SK-20 (BMZ) | 316.35 | 316.80 | 0.45 | 24 | 0.85 | 342 | 0.07 | 0.11 | 0.08 | 0.01 | 安格斯·維恩 | |
23-SK-24 (BMZ) | 258.72 | 259.12 | 0.40 | 220 | 0.01 | 225 | 0.04 | 0.01 | 0.04 | 0.05 | 瓊斯 3 Vein | |
23-SK-25 (BMZ) | 287.70 | 288.10 | 0.40 | 27 | 0.30 | 138 | 0.04 | 0.02 | 0.00 | 0.00 | 全新 NW Vein | |
23-SK-25 | 319.80 | 320.40 | 0.60 | 422 | 0.01 | 426 | 0.01 | 0.00 | 0.01 | 0.03 | 安格斯·維恩 | |
23-SK-26 | 253.00 | 260.00 | 7.00 | 199* | 0.02 | 208 | 0.02 | 0.01 | 0.04 | 0.02 | 湯姆斯靜脈區 | |
包括 | 253.00 | 254.00 | 1.00 | 296 | 0.00 | 297 | 0.01 | 0.01 | 0.03 | 0.03 | 湯姆斯靜脈區 | |
包括 | 257.60 | 258.00 | 0.40 | 2180* | 0.36 | 2,315 | 0.03 | 0.05 | 0.00 | 0.01 | Toms Vein | |
異常礦化 | ||||||||||||
23-SK-15 | 235.62 | 236.18 | 0.56 | 26 | 0.08 | 57 | 0.07 | 0.03 | 0.39 | 0.05 | Angus Vein(Diabase 託管) | |
23-SK-17 | 267.19 | 270.00 | 2.81 | 9 | 0.01 | 14 | 0.11 | 0.01 | 0.07 | 0.10 | 賤金屬區 | |
23-SK-17 | 272.00 | 282.96 | 10.96 | 19 | 0.00 | 20 | 0.18 | 0.00 | 0.55 | 0.31 | 賤金屬區 | |
23-SK-18 | 132.63 | 133.05 | 0.42 | 4 | 0.07 | 31 | 0.09 | 0.02 | 0.01 | 0.06 | Toms Vein(Diabase 託管) | |
23-SK-18 | 258.00 | 266.00 | 8.00 | 2 | 0.00 | 3 | 0.01 | 0.00 | 0.21 | 0.34 | 賤金屬區 | |
23-SK-18 | 289.00 | 315.00 | 26.00 | 6 | 0.00 | 8 | 0.07 | 0.00 | 0.35 | 0.40 | 賤金屬區 | |
23-SK-19 | 281.00 | 289.40 | 8.40 | 36 | 0.09 | 68 | 0.17 | 0.01 | 0.16 | 0.51 | 新靜脈區 | |
23-SK-19 | 320.85 | 321.30 | 0.45 | 81 | 0.01 | 83 | 0.47 | 0.01 | 3.01 | 1.29 | 新的 E-W 靜脈 | |
23-SK-20 | 300.00 | 306.00 | 6.00 | 24 | 0.05 | 41 | 0.50 | 0.01 | 0.44 | 1.11 | 賤金屬區 | |
23-SK-20 | 314.79 | 317.20 | 2.41 | 9 | 0.26 | 108 | 0.04 | 0.06 | 0.03 | 0.02 | 安格斯靜脈區域 | |
包括 | 315.65 | 316.35 | 0.70 | 6 | 0.25 | 98 | 0.01 | 0.04 | 0.01 | 0.01 | 安格斯靜脈區域 | |
23-SK-22 | 143.00 | 143.40 | 0.40 | 0 | 0.13 | 50 | 0.00 | 0.02 | 0.00 | 0.00 | McNamara Vein(Diabase 託管) | |
23-SK-22 | 335.60 | 336.50 | 0.90 | 30 | 0.01 | 33 | 0.08 | 0.01 | 1.55 | 0.59 | 賤金屬區 | |
23-SK-23 | 274.59 | 275.00 | 0.41 | 2 | 0.13 | 49 | 0.02 | 0.00 | 0.01 | 0.01 | Toms Vein | |
23-SK-23 | 281.60 | 285.00 | 3.40 | 6 | 0.00 | 7 | 0.04 | 0.00 | 0.31 | 0.31 | 賤金屬區 | |
23-SK-24 | 255.17 | 255.57 | 0.40 | 39 | 0.11 | 81 | 0.10 | 0.15 | 0.40 | 0.11 | 全新 NW Vein | |
23-SK-24 | 256.95 | 259.12 | 2.17 | 76 | 0.01 | 81 | 0.05 | 0.01 | 0.03 | 0.04 | 全新 NW Vein | |
23-SK-24 | 293.90 | 294.60 | 0.70 | 2 | 0.34 | 129 | 0.00 | 0.03 | 0.00 | 0.00 | McNamara Vein | |
23-SK-25 | 255.60 | 256.10 | 0.50 | 20 | 0.03 | 31 | 0.01 | 0.01 | 0.12 | 0.17 | 全新 NW Vein | |
23-SK-25 | 266.00 | 267.00 | 1.00 | 20 | 0.08 | 49 | 0.00 | 0.04 | 0.19 | 0.03 | 全新 NW Vein | |
23-SK-25 | 287.00 | 310.40 | 23.40 | 8 | 0.01 | 12 | 0.05 | 0.00 | 0.16 | 0.07 | 寬闊的靜脈區 | |
包括 | 297.40 | 297.80 | 0.40 | 12 | 0.12 | 55 | 0.03 | 0.01 | 0.08 | 0.15 | Ag/Co 靜脈 |
Appendix A: Significant and anomalous silver, cobalt and base metal mineralization intersected in the Phase 2 2023 drill program at the Campbell-Crawford target area. Results from the first twelve drill holes (23-SK-14 to -26) are presented, with the remaining six pending. AgEq* (silver equivalent) grades were calculated using $23.69 USD / oz silver and $28,500 USD / tonne cobalt, with metal prices captured on January 2, 2024. Mineralized drilling intervals do not reflect true interval length. "BMZ" refers to mineralization within a Broader Mineralized Zone. *Assaying by Screened Metallics was conducted on high-grade, visually identified silver mineralization in hole 23-SK-26 between 256.80 m to 258.80 m.
附錄A:在坎貝爾-克勞福德目標區域的2023年第二階段鑽探計劃中,出現了重要的異常銀、鈷和賤金屬礦化。提供了前十二個鑽孔(23-SK-14 至 -26)的結果,其餘六個待定。AgeQ*(白銀當量)等級是使用23.69美元/盎司白銀和28,500美元/噸鈷計算得出的,金屬價格是在2024年1月2日公佈的。礦化鑽探間隔不能反映真實的間隔長度。“BMZ” 是指更廣泛的礦化區內的礦化。*Screened Metallics 對位於 256.80 m 至 258.80 m 之間的 23-SK-26 洞中經過視覺識別的高品位銀礦化進行了檢測。
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