普里亚穆耶锑汞成矿中的金含量

Vitaliy Stepanov
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摘要

介绍了普里亚穆尔斯基金矿的地质构造位置、交代岩组成、矿石组成和锑汞矿床及产状的含金量。人们确定,其中许多矿石含有天然黄金,其浓度达到商业价值。有些含金锑和汞矿床是金砂矿形成的来源。从矿石、近矿交代岩和天然金样品的组成来看,与这些矿床和产状相似的是雅库特-萨拉克的金锑组和九州的金汞组金矿。建议对Priamursky省的一些汞和锑矿床和金矿进行审计。因此,它有望识别金锑矿床和金汞矿床。此外,锑和汞的出现可能表明基岩中存在硫化金地层矿床,类似于Mayskoye (Chukotka)的大型矿床。
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On the gold content in the antimony and mercury mineralization in Priamurye
The data on the geological and structural position, composition of metasomatites, ores, and gold content of antimony and mercury deposits and occurrences of the Priamursky gold-bearing area are presented. It was established that the ores of many of them contain native gold, whose concentration reaches commercial values. Some of the gold-bearing antimony and mercury deposits serve as sources of the formation of gold placers. By the composition of ores, near-ore metasomatites and samples of native gold, the analogues of these deposits and occurrences are the famous gold deposits of Yakutia - Sarylakh of the gold-antimony formation and Kyuchus of the gold-mercury formation. It is recommended to audit a number of mercury and antimony deposits and occurrences in the Priamursky province for gold. As a result, it is expected to identify deposits of gold-antimony and gold-and-mercury formation. In addition, occurrences of antimony and mercury may be indicative of the presence of gold-sulfide formation deposits in the bedrock, similar to a large deposit Mayskoye (Chukotka).
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