financially supported by the Major Research Project of National Natural Science Foundation of China(NSFC Project;Grant Nos.92162215 and 92155305);National Key Basic Research Development Program of China(973 Program;Grant Nos.2015CB452602 and 2015CB452606);111 Plan under the Ministry of Education of China and the State Administration of Foreign Experts Affairs,China(Grant No.B07011)。
Magmatic-hydrothermal Sn deposits are commonly associated with high silica magmas,but why most global high silica granites do not bear economic Sn ore grades remains unclear.Two crucial factors controlling magmatic-hy...
financially supported by the National Natural Science Foundation of China(No.41372102);the National Basic Research Program of China(No.2014CB440803);the China Geological Survey(No.DD20160071)
The Xiangshan mafic-ultramafic complex is one of the major Early Permian maficultramafic intrusions in eastern Tianshan (Xinjiang, NW China), and consists of two major intrusive phases. The first intrusive phase is ...
financially supported by the National Basic Research Program(973 Program)of China(No.2013CB29702);the China Ocean Mineral Resources Research and Development Association(DY125-11-R-05,DY125-12-R-03)
Pumice,the most widely distributed volcanic rock in Okinawa Trough,is loose and porous.Since its formation,it has definitely suffered from the denudation of the sea to different degrees.In order to truly reveal the ge...
supported by the National Key Basic Research Program of China(2012CB416800);the Key International Science and Technology Cooperation project(2007DFA21230)
The Ningzhen region in Jiangsu Province represents the easternmost magmatic region in the middle-lower Yangtze River belt.The formation of the polymetallic deposits has close genetic relationships with Early Cretaceou...
supported by 973 Program(2007CB411408);National Natural Science Foundation of China(NSFC) projects (40730420 and 40973038);Chinese Academy of Sciences(KZCX2-YW-Q04)
The three most crucial factors for the formation of large and super-large magmatic sulfide deposits are: (1) a large volume of mantle-derived mafic-ultramafic magmas that participated in the formation of the deposi...
supported by the National Science Foundation of China (project 40872147/40472119);the basic outlay of scientific research work from the Ministry of Science and Technology of China(project 2006BAB01A11);the Geological Survey Project of China(project 12120100782003-13)
The Taohekou Formation is a volcanic-sedimentary terrane formed in the early Silurian in the northern Daba Mountains, China. The volcanic rocks, with dominant alkali basalts and minor mantle xenoliths, are enriched in...
Mianning-Dechang Himalayan REE Metallogenetic Belt in Sichuan Province lies along the western margin of the Yangtze Craton. We have conducted detailed mineralogical studies on ore minerals collected from Maoniuping an...
the grants of the National Key Project for Basic Research of China(No.2002CB412600);the National Natural Science Foundation of China(Nos.40172025,40103003,49802005,49772107,40473020);the key project on the Tibetan Plateau of the Ministryof Land and Resources of China(No.20010102401).
Abundant mafic microgranular enclaves (MMEs) extensively distribute in granitoids in the Gangdise giant magmatic belt, within which the Qüxü batholith is the most typical MME-bearing pluton. Systematic sampling for ...
supported by NSFC(Grant Nos.40072037,40273025);NKBRSF Project(Grant No.G1999043200)
Primitive mantle normalized Platinum group elements (PGE) concentration patterns for the Zhengziyanwo intrusion and Dashibao Formation basalts are of positive slope, similar to most of the world class magmatic Ni Cu P...