Granitic pegmatites are commonly thought to form by fractional crystallization or by liquid immiscibility of granitic magma;however,these proposals are based ma
Late Paleozoic post-collisional granitoids are widespread in West Junggar,as well as northern Xinjiang.As a representative of those intrusions,the Jietebutiao g
Geochemical characteristics of the Chagande’ersi molybdenum deposit in Inner Mongolia and its genesis were analyzed in this study using rock mineralography and
The Binchuan area of Yunnan is located in the western part of the Emeishan large igneous province in the western margin of the Yangtze Block.In the present stud