supported jointly by National Basic Research Program of China (Grant No. 2007CB411401);Special Fund of State Key Laboratory of Ore Deposit Geochemistry and National Natural Science Foundation of China (Grant No. 40773035)
Ore minerals in the sedimentary-type Cu deposits in the Xuanwei Formation overlying the Emeishan basalt are dominated by copper sulfides and native copper. As the ores mostly exhibit concretionary structure, previous ...
Supported by National Natural Science Foundation of China (Grant Nos. 40572051, 40830317, 40873023, 40672044);National Basic Research Program of China (Grant No. 2009CB421002), Chinese "111" Project (Grant No. B07011);Programme of the Integrated Study of Basic Geology of Qinghai-Tibetan Plateau of the China Geological Survey
The Cretaceous granitoids in the middle and northern Gangdese, Tibet are generally interpreted as the products of anatexis of thickened deep crust genetically associated with the Lhasa-Qiangtang collision. This paper ...
The wave velocity for two types of granitoids was measured using the analytic method of full-wave vibration at high pressure and high temperature. The laws of velocity changes for them differ with the pressure hoost a...