论文部分内容阅读
通过对东刘家地区金矿床地质特征的分析研究 ,认为该区金矿床受层间滑动构造系统控制 ,赋存于古元古代荆山群或侵入其中的二长花岗岩之中 ,其矿床成因为多源多期中低温热液型。
Based on the analysis of the geological characteristics of the gold deposits in Dongliujia area, the gold deposits in the area are controlled by interlaminar sliding tectonics system and occur in the monzonitic granite in the Paleoproterozoic Jingshan Group or intruded into them. The ore deposits are multi-source Multi-stage low temperature hydrothermal type.