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Ore-forming fluid characteristics of the Damoqujia gold deposit in Zhaoping Fault Zone, Shandong province, China

机译:山东省昭平断裂带DAMOQUJIA金矿床的矿石流体特征

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摘要

The Damoqujia gold deposit, discovered recently and located in the north of Zhaoping Fault Zone, is a large altered rock type deposit. Metallogenic processs can be divided into Ⅰ, Ⅱ, Ⅲ and Ⅳ four stages which are charactered by coarse pyrite - milky quartz assemblage, ashy fine quartz - pyrite veins, auriferous poly-metallic sulfide and quartz-carbonate veins respectively.
机译:最近发现的Damoqujia金矿床,位于Zhoping断层区的北部,是一个大型改变的岩型矿床。可以将成矿过程分为Ⅰ,Ⅱ,Ⅲ和Ⅳ阶段,其特征在于粗硫铁矿 - 乳状石英组合,灰质细石英 - 硫化物静脉,纤维酸多金属硫化物和石英碳酸盐静脉。

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