黑海北部地区的黄金潜力

Y. Shnyukov, M. Maslakov, U. Naumenko
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引用次数: 0

摘要

本文介绍了对黑海北部和克里米亚地区金矿的分析评价结果。本区含金量的增加主要与古岛弧和乌克兰结晶地块的岩浆作用和火山作用有关。通过对实地研究和实验室结果的分析,可以确定金矿化成因的主要因素。克里米亚山脉的岩浆活动形成了原生矿床和冲积矿床,从东部的卡拉达格到赫拉克利亚和罗蒙诺索夫地块依次延伸。细粒金矿的主要来源是乌克兰盾构岩的风化壳和冲积层的次生产物,这些次生产物在近代,特别是在冰期后,有大量的松散沉积物流出。作者指出,古水系在含金砂的聚集和众多小河流冲积层的潜在流出源的形成中都起着决定性作用。别列根斯基和苏尔斯基气候岩的冲积砂和冲积-冲积覆盖卵石因其含金量而特别令人感兴趣。它们在流域上形成覆盖层,填满了大河的古山谷。作者还研究了古第聂伯河和北亚速海地区其他主要河流在冰川融化期间的作用,当时大量的沙质粉质物质,包括细金和超细金,被长途运输。因此,确定影响金矿床位置、构造和组成的因素,对于确定黑海北部和克里米亚地区形成金矿床的潜在有利条件的预测标准具有重要意义。目前关于黑海地区含金量的数据还不充分。有必要对金矿床进行进一步的研究,以确定这一现象的科学和实际意义。到目前为止,只能说明金矿床的存在,为进一步的研究和找矿提供了基础。
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The gold potential of the northern Black Sea region
The article presents the results of the analysis and evaluation of gold occurrences of the Northern Black Sea and Crimea. The increased gold content of this region is associated primarily with magmatism and volcanism of the paleo
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