V. Stepanov
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摘要

本文论述了阿穆尔省Unya-Bom地区的Witwatersrand古砂矿和现今的高汞金砂矿及其成因。威特沃特斯兰德矿床含细金,汞含量显著。原始的来源是未知的。在Unya-Bom地区,在矿体被破坏和高品位汞金转变为砂矿期间,其成分被保留下来,但砂矿中形成的高品位外壳除外:由于电化学腐蚀,银和汞被从中除去。当在砂矿中运输25公里时,金颗粒中心部分的高汞含量相当于矿石金。对威特沃特斯兰德古砂矿中碎裂成因金的一种可能来源进行了分类。可能为金-石英矿化,含高汞金,与阿穆尔河地区乌尼亚-博姆地区相似。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
О коренных источниках палеороссыпей Витватерсранда (Южная Африка)
The article discusses Witwatersrand paleoplacers as well as current high-mercury gold placers and sources of their formation in the Unya-Bom district of the Amur province. The Witwatersrand deposits contain fine gold with significant mercury content. The original sources are unknown there. In the Unya-Bom district, during the destruction of ore bodies and the transition of high-grade mercuric gold into placers, its composition is preserved, with the exception of the high-grade shell formed in placers: silver and mercury are removed from it due to electrochemical corrosion. When transported in placers up to 25 km, the high content of mercury in the central part of gold particles corresponds to ore gold. An attempt was made to typify one of the possible sources of clastogenic gold in Witwatersrand paleoplacers. It might have been gold-quartz mineralization with high- mercury gold, similar to that common in the Unya-Bom district of the Amur region.
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