摘要
大庙山金矿床产于震旦纪灯影组中段地层中,是多种成矿作用叠加改造的产物,成矿物质来 自于岩浆期后热液和灯影组碎屑岩。黄-破断裂是其主要的导矿构造,其次级低序次NNE向断裂带是 主要的容矿构造。
The Damiaoshan gold deposit occurred in the middle member of the Sinian Dengying Formation. It is resulted from polymetallogenic reworking and sourced from post - magmatic hydrothermal solution and the detrital rock of the Dengying Formation. The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host.
引文
①安徽省地矿局327队,安徽区调所,滁州-庐江-带铜、金、铅、锌等找矿研究,1996
[1]栾世伟,等.金矿床地质及找矿方法.成都:四川科技出版社,1987
[2]安徽省地质矿产局.安徽省区域地质志. 北京:地质出版社,1987
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