supported by the National Natural Science Foundation of China (Grant No. 41273053);the National Key Basic Research Program of China (Grant No. 2012CB416702);the Sino-French Cai Yuanpei Program of China Scholarship Council
The Middle-Late Jurassic Cu-Pb-Zn-bearing and W-bearing granites in the Nanling Range have distinctly different mineralogical and geochemical signatures. The Cu-Pb-Zn-bearing granites are dominated by metaluminous amp...
financially supported by the National Key Basic Research Program (Grant2012CB416704) from the Ministry of Science and Technology, China;grant No. 40772063 from the National Natural Science Foundation of China;the Program of Excellent Young Scientists from the Ministry of Land and Resources (200809);Geological Survey Program Grant 1212010561603-2 from the China Geological Survey
Previous studies have obtained some petrogenetic and metallogenic chronological data with SHRIMP (sensitive high-resolution ion microprobe) zircon U-Pb, zircon LA-ICPMS (laser-ablation-inductively coupled plasma ma...
supported by the National Key Basic Research Program(2012CB416700,2007CB411408),a special fund managed by the State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,and the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences in Wuhan
Mesozoic granitic intrusions are widely distributed in the Nanling region, South China. Yanshanian granites are closely connected with the formation of tungsten deposits. The Xihuashan granite is a typical representat...
funded by the National Natural Science Foundation of China (No 40471139);National Basic Research Program of China (No 2004CB 720206);the State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sci-ences Foundation (No SKLLQG0309)
Layer LJ3 of Linjiang stratigraphic section in Dongjiang River valley in the south of the Nanling Mountains is a set of red sandy sediments.Measured by thermoluminescence(TL) dating,it was found to be formed in MIS2-9...
Supported by National Basic Research Program of China (Grant No. 2007CB411403);Knowledge Innovation Project of the Chinese Academy of Sci-ences (Grant No. KZCX1-YW-15-2);National Natural Science Foundation of China (Grant No. 40728002)
Although a number of petrographic observations and isotopic data suggest that magma mixing is common in genesis of many granite plutons, it is still controversial whether the mantle-derived magmas were involved in gra...
Supported by National Natural Science Foundation of China (Grant No.40471139);National Basic Research Program of China (Grant No.2004CB720206);the Special Fund of Scientific Research for Doctoral Subjects of Chinese Universities (Grant No. 20070574005);the RGC Grant of the HKSAR (HKU7243/04H)
The paleoenvironment indicated by the geochronology,major oxides——SiO2,Al2O3 and TOFE(Fe2O3 + FeO),and CIA(Chemical Index of Alteration) value of the red earth and brown-yellow silt primarily characterized by the Li...