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  • 內華達金在亞特蘭大北延伸目標上鑽探多處厚度超過1克/噸黃金的礦脈，特別是2900萬克中的1.95克/噸黃金以及610萬克中的6.6克/噸黃金。

NEVADA KING DRILLS MULTIPLE THICK +1 G/T GOLD INTERCEPTS HIGHLIGHTED BY 1.95 G/T AU OVER 29.0M INCLUDING 6.6 G/T AU OVER 6.1M AT NORTH EXTENSION TARGET AT ATLANTA

NEVADA KING DRILLS MULTIPLE THICK +1 G/T GOLD INTERCEPTS HIGHLIGHTED BY 1.95 G/T AU OVER 29.0M INCLUDING 6.6 G/T AU OVER 6.1M AT NORTH EXTENSION TARGET AT ATLANTA

內華達金在亞特蘭大北延伸目標上鑽探多處厚度超過1克/噸黃金的礦脈，特別是2900萬克中的1.95克/噸黃金以及610萬克中的6.6克/噸黃金。
PR Newswire ·  2024/12/09 19:30

VANCOUVER, BC, Dec. 9, 2024 /PRNewswire/ - Nevada King Gold Corp. (TSXV: NKG) (OTC: NKGFF) ("Nevada King" or the "Company") is pleased to announce results from 20 vertical, reverse circulation ("RC") holes and one diamond core drill hole completed in the North Extension Target ("NET") (Tables 1 and 2) together with 14 RC holes drilled in the East Ridge Target ("ERT") (Table 5) at its 12,000 hectare (120km2), 100% owned Atlanta Gold Mine Project, located in the prolific Battle Mountain Trend 264km northeast of Las Vegas, Nevada. These holes were completed as part of the Company's Phase II drill program.

溫哥華，BC，2024年12月9日 /PRNewswire/ - 內華達國王黃金公司 (tsxv: NKG) (場外交易: NKGFF) （「內華達國王」或「公司」）欣然宣佈在其12000公頃（120km²）100%擁有的亞特蘭大黃金礦項目中完成的20個垂直反循環（「RC」）孔和一個金剛石核心鑽孔的結果，該項目位於內華達州拉斯維加斯以東北264公里的巴特爾山趨勢中。這些孔是公司第二階段鑽探計劃的一部分。

Table 1. Highlight holes released today. Mineralization occurs along near-horizontal horizons with true mineralized thickness in vertical holes estimated to be 85% to 95% of reported drill intercept length. *Denotes holes bottoming in mineralization. (CNW Group/Nevada King Gold Corp.)
表1. 今天發佈的重點孔。礦化沿近水平地平線發生，垂直孔中的真實礦化厚度估計爲報告鑽孔截長的85%至95%。*標示出底部爲礦化的孔。(CNW Group/內華達國王黃金公司)
Figure 2. Location map for holes reported in today's news release along 10 sections shown below in figures 3-11. In addition to the holes released along the NET sections, the remaining holes of the East Ridge Target CSAMT test holes are also reported in today's release. (CNW Group/Nevada King Gold Corp.)
圖2. 今日新聞稿中報告的孔位置圖，沿下圖3-11所示的10個剖面。此外，今天的發佈中還報告了東脊目標CSAMt測試孔的其餘孔。(CNW Group/內華達國王黃金公司)
Figure 3. Section 22-31N(2) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖3. 22-31N(2)剖面，向北看通過AMFZ。礦化沿着一個緩慢西傾的硅化地平面發生，該地平面在基底寒武紀時代的白雲岩和覆蓋的第三紀火山岩之間的非整合接觸處發展。垂直孔中真實礦化厚度估計爲報告鑽孔截長的85%至95%。(CNW Group/內華達國王黃金公司)
Figure 4. Section 22-30N(3) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖4. 22-30N(3)剖面，向北看通過AMFZ。礦化沿着一個緩慢西傾的硅化地平面發生，該地平面在基底寒武紀時代的白雲岩和覆蓋的第三紀火山岩之間的非整合接觸處發展。垂直孔中真實礦化厚度估計爲報告鑽孔截長的85%至95%。(CNW Group/內華達國王黃金公司)
Figure 5. Section 22-29N(3) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖5. 視圖22-29N(3)朝北看AMFZ。礦化沿着一個輕微西傾的硅化地層分佈，形成於基底奧陶紀的白雲岩與上覆的第三紀火山岩之間的不整合接觸面上。真正的礦化厚度估計爲垂直鑽孔報告的交 intercept長度的85%至95%。(CNW集團/內華達國王黃金corp.)
Figure 6. Section 22-28N(3) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖6. 視圖22-28N(3)朝北看AMFZ。礦化沿着一個輕微西傾的硅化地層分佈，形成於基底奧陶紀的白雲岩與上覆的第三紀火山岩之間的不整合接觸面上。真正的礦化厚度估計爲垂直鑽孔報告的交 intercept長度的85%至95%。(CNW集團/內華達國王黃金corp.)
Figure 7. Section 22-27N(3) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖7. 視圖22-27N(3)朝北看AMFZ。礦化沿着一個輕微西傾的硅化地層分佈，形成於基底奧陶紀的白雲岩與上覆的第三紀火山岩之間的不整合接觸面上。真正的礦化厚度估計爲垂直鑽孔報告的交 intercept長度的85%至95%。(CNW集團/內華達國王黃金corp.)
Figure 8. Section 22-26N(2) looking north across the AMFZ. Mineralization occurs along a gently west-dipping, silicified horizon developed at the unconformable contact between basal Ordovician age dolomite and overlying Tertiary age volcanics. True mineralized thickness estimated to be 85% to 95% of reported drill intercept length in vertical holes. (CNW Group/Nevada King Gold Corp.)
圖8. 視圖22-26N(2)朝北看AMFZ。礦化沿着一個輕微西傾的硅化地層分佈，形成於基底奧陶紀的白雲岩與上覆的第三紀火山岩之間的不整合接觸面上。真正的礦化厚度估計爲垂直鑽孔報告的交 intercept長度的85%至95%。(CNW集團/內華達國王黃金corp.)

譯文內容由第三人軟體翻譯。


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