黄铁绢英岩金矿主要赋存在以胶东群为交代基体的重熔花岗岩或交代花岗岩的构造蚀变带中心。
Pyritic phyllic alteration gold deposits are mainly located in the center of structure altered zone of anatexiS granite or metasomatism granite.
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
The tectonic setting of granitoids of Yanshanian Stage in the south of Anhui Province and the northeast of Jiangxi Province in Jiangnan Uplift is studied.
本区内的金矿断裂构造即花岗岩与太古代胶东群变质岩呈构造接触带。
The faults related to the gold deposits in the area often follow the contact between granites and metamorphic rocks of the Achaean Jiaodong Group.
哀牢山—金沙江构造带糜棱状花岗岩位于哀牢山深变质带中部。
Mylonitized granite in the AilaoshanJinshajiang tectonic zone is hosted in the center of the Ailaoshan high grade metamorphic belt.
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
Rare Earths of Magmatic Rocks of Yanshanian Stage in Adjacent Region of Anhui and Jiangxi Province, Jiangnan Uplift;
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
Rare Earths of Magmatic Rocks of Yanshanian Stage in Adjacent Region of Anhui and Jiangxi Province, Jiangnan Uplift;
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