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描述
该金矿位于哈萨克斯坦阿克莫拉州扎克辛斯基区境内。 研究区为哈萨克高原西郊，绝对海拔248～423 m，相对海拔50～70 m。 金矿点是1989年由国营企业“Stepgeology”的PSE-33和GRE-37联合进行的1:50000地质调查工作的结果发现的。
1992-94年，GRE-37在现场矿点进行了预索赔和评估工作。 由于资金终止，评价井钻探量为预计量的17.8%。 同样，由于同样的原因，大约 5000 个岩心样本仍未得到分析。
关键点
金矿床位于细长煤槽东侧附近，呈经向方向。 这种地质结构包括陆源地层、碳酸盐地层和陆源碳酸盐岩地层，其历史可以追溯到石炭纪时期。
该矿床区域夹在断层之间，明显具有强烈破碎和角砾化的区域。 它还具有一系列由煌斑岩和斑岩组成的堤坝。 发生了强烈的热液过程，导致了贝雷石型交代岩的形成和金矿石矿化的沉积。
在该领域内，已确定了三种热液交代地层：
Propylite（石英-绿泥石-绢云母-绿帘石交代岩） – 代表交代作用的亚碱性阶段。
Berezitic（贝雷兹石化岩石、石英绢云母交代岩或贝雷兹岩） – 表明交代作用的酸性阶段。
泥质岩（石英-碳酸盐-高岭石交代岩）——与交代作用的酸性阶段有关。
矿区描述
通过矿床内的勘探和评估工作，沿走向和倾角识别并追踪了四个矿带。 后者的长度从100米到850米不等，宽度从几米到130米不等。 矿床矿带总长1230米。
在这些区域的轮廓内，确定了 0.3 克/吨金的边界品位，并将其纳入八个矿体的储量计算中。
已发现的矿体从基底表面至深度14-18米至91-97米均经历过氧化作用。
风化壳矿石中最常见的矿物是石英与玉髓，风化壳氧化矿石中的原生矿石矿物是自然金。
矿体呈东南走向，平均入射角60～78度。
Basic Details
Business ID:
L#20240587
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