阿穆尔州索洛维约夫斯基金矿中心金矿床时代的地质和同位素参考点

Vitali Stepanov, Anton Melnikov
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摘要

报告提供了阿穆尔州索洛维约夫斯基金矿中心金矿床的地质和同位素年龄数据,这些矿床被归类为金多金属、金硫化物石英和金石英形成类型。研究表明,根据地质数据,金多金属(Berezitovoe)和金硫化物石英(Kirovskoe)类型的高产矿床的地质和同位素年龄为早白垩世,而根据同位素测定,其地质和同位素年龄为巴雷姆世(1.31-1.25 亿年)。由于母岩多为前寒武纪的片麻岩和水晶页岩,因此很难确定金-石英型贫矿床的地质年代。Snezhninka 和 Zolotaya gora 金石英矿床的同位素形成年龄分别为晚三叠世(2.12 亿年)和晚侏罗世(1.55 亿年)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological and isotopic reference points of the age of gold deposits of the Solovyovsky gold ore center in the Amur province
The data are presented on the geological and isotopic age of gold deposits of the Solovyovsky gold ore center in the Amur province, assigned to the gold-polymetallic, gold-sulfide-quartz, and goldquartz formation types. It is demonstrated that the geological and isotopic age of the most productive ore deposits of the gold-polymetallic (Berezitovoe) and gold-sulfide-quartz (Kirovskoe) types is Early Cretaceous according to geological data and Barremian (in the range of 131–125 million years) according to isotopic determinations. The geological age of poorly productive ore deposits of the gold-quartz type is difficult to determine due to the fact that the host rocks are most often represented by gneisses and crystal shales of Precambrian age. The isotopic age of formation of the Snezhninka and Zolotaya gora gold-quartz deposits is, respectively, Late Triassic (212 million years) and Late Jurassic (155 million years).
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