The work is supported by National Natural Science Foundation of China(NSFC)(Grants No.11574215,No.11575116,No.11274359,and No.11422428);H.M.W is also supported by the National 973 program of China(Grants No.2018YFA0305700 and No.2013CB921700);the“Strategic Priority Research Program(B)”of the Chinese Academy of Sciences(Grant No.XDB07020100).
Node line band-touchings protected by mirror symmetry(named as m-NLs),the product of inversion and time reversal symmetry S=PT(named as s-NLs),or nonsymmorphic symmetry are nontrivial topological objects of topologica...
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 ...