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NEVADA KING MAKES AT-SURFACE OXIDE GOLD DISCOVERY AT EAST RIDGE ZONE, SHOWS POTENTIAL FOR LARGER MINERALIZED TARGETS IN NEW GEOLOGICAL SETTING AT ATLANTA

NEVADA KING MAKES AT-SURFACE OXIDE GOLD DISCOVERY AT EAST RIDGE ZONE, SHOWS POTENTIAL FOR LARGER MINERALIZED TARGETS IN NEW GEOLOGICAL SETTING AT ATLANTA

内华达金王在东岭区的表面氧化金发现点，展示了在亚特兰大的新的地质环境中更大矿化目标的潜力。
PR Newswire ·  07/16 07:30

VANCOUVER, BC, July 16, 2024 /PRNewswire/ - Nevada King Gold Corp. (TSXV: NKG) (OTCQX: NKGFF) ("Nevada King" or the "Company") is pleased to announce results for 15 reverse circulation ("RC") reconnaissance holes drilled in and around the East Ridge Target ("ERT") at its 5,166 hectare (51.7km2), 100%-owned Atlanta Gold Mine Project, located in the prolific Battle Mountain Trend 264km northeast of Las Vegas, Nevada. Drilling at the ERT commenced in June with five holes located to test coincident geophysical and geochemical anomalies. A fence of 10 holes were also drilled between the ERT and the Atlanta Resource Zone. The ERT covers a low resistivity zone that measures 100m-wide, strikes 1,000m north-south and is located 300m east of the historical Atlanta Pit and resource zone.

珍宝餐饮集团（TSXV：NKG）（OTCQX：NKGFF）很高兴宣布，其5166公顷（51.7平方公里），100％拥有的亚特兰大黄金矿项目位于内华达州拉斯维加斯东北部264公里的富有成效的巴特尔山趋势地带。探针开展于六月，共进行了15个反向循环（"RC"）侦察孔的钻探，并围绕东支脉目标（"ERT"）进行。其中五个孔位用于测试具有相互关联的地球物理和地球化学异常。此外，还钻探了10个孔位，介于ERT和亚特兰大资源区之间。ERT覆盖了一条低电阻区域，宽10,000米，南北走向10,000米，位于历史悠久的亚特兰大矿坑和资源区东部30000万处。

Figure 1. Plan view of ERZ showing locations of reported reconnaissance drill holes. The composited low resistivity CSAMT anomaly highlighted in orange trends NNW for about 1,000m and corresponds with intrusive dikes and associated decalcification in the surrounding dolomite that provided the plumbing system for gold mineralization. The trend of the anomaly is very similar to that of the main pit resource zone. (CNW Group/Nevada King Gold Corp.)
图1. ERZ（East Ridge Zone）平面图，显示了报道的侦察孔的位置。高亮显示的低电阻CSAMt异常向北北西延伸约100000米，对应于侵入岩墙以及周围白云石的解钙作用提供了含金矿化的管道系统。异常的趋势非常类似于主采区资源带。（CNW集团/Nevada King Gold Corp.）
Figure 2. Drill section A-A' across the central portion of the ERZ showing gold mineralization in relation to the silica breccia zone and high-angle intrusions. Oxidized Au mineralization is largely hosted within silicified and clay-altered rhyolitic intrusions and adjacent silicified dolomite. Depth of mineralization within the intrusive rocks is currently unknown. (CNW Group/Nevada King Gold Corp.)
图2. 穿过ERZ中部的A-A'钻孔剖面，显示了硅化英安岩带和高角度侵入物中的含金矿化作用。氧化金矿化作用主要寄存在硅化和粘土改性流纹岩侵入和相邻的硅化白云石中。目前尚不清楚岩浆侵入岩石中的矿化深度。（CNW集团/Nevada King Gold Corp.）
Figure 3. Looking north at CSAMT Line 10 with ERZ anomaly (orange), indicating low-resistivity rock types - silicified/argillized Tertiary intrusions & variably silicified and decalcified dolomite. Blue indicates highly resistive, unaltered Paleozoic carbonate basement rocks. Horn-shaped low resistivity zone at far right is potentially upper portion of large igneous mass intruding upward into carbonate sequence and could represent a mineralized zone similar to the ERZ, albeit on a larger scale. (CNW Group/Nevada King Gold Corp.)
图3. 向北看CSAMt Line 10，呈现出低电阻性岩石类型，即硅化/粘土化的第三纪侵入岩和可变硅化和解钙的白云石。蓝色表示高电阻性未改性的古生代碳酸盐基底岩石。右侧类似象形角的低电阻区域潜在是大型岩浆团体的上部，向上侵入碳酸盐系列并可能代表类似于ERZ的矿化带，尽管规模更大。（CNW集团/Nevada King Gold Corp.）
Figure 4. Looking north at CSAMT Line 12 with ERZ anomaly (green), indicating low-resistivity rock types - silicified/argillized Tertiary intrusions and decalcified dolomite. Blue indicates highly resistive, unaltered Paleozoic carbonate basement rocks. Red colors to east of ERZ in new Jumbo Target suggest large intrusive mass underneath Paleozoic carbonate cover with plumes intruding up through the carbonate carapace, similar to that seen in ERZ but on a much larger scale. (CNW Group/Nevada King Gold Corp.)
图4. 向北看CSAMt Line 12，呈现出低电阻性岩石类型，即硅化/粘土化的第三纪侵入岩和可变硅化和解钙的白云石。蓝色表示高电阻性未改性的古生代碳酸盐基底岩石。ERZ绿色异常以东的红色色带表明在古生代碳酸盐层盖下面，存在大型侵入体，且向上侵入碳酸盐层盖，类似于ERZ的矿化带，但规模更大。（CNW集团/Nevada King Gold Corp.）
Figure 5. Plan Map shows distribution of major structural features as indicated by deep CSAMT low resistivity responses in relation to exploration targets and drilling done to date (includes historical and NKG holes). Deep drill holes reveal these CSAMT anomalies to be igneous intrusions and associated alteration of adjacent carbonate basement rocks. The Atlanta resource zone occurs near a sharp flexure in the basement structure that is mimicked by the low resistivity zones to the west and east. (CNW Group/Nevada King Gold Corp.)
图5. 平面图显示了主要构造特征的分布，如深部CSAMt低电阻性响应所示，与迄今为止完成的勘探目标和钻探（包括历史和NKG孔）相关。深钻孔揭示了这些CSAMt异常体是岩浆侵入物并与相邻碳酸盐岩地基发生了改性。亚特兰大资源区位于地下构造的一个明显的弯曲处，并且该构造的低电阻性区域在西部和东部得到了模拟。（CNW集团/Nevada King Gold Corp.）
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