financially supported by the National Natural Science Foundation of China (Grant Nos.U1403292, 41472196, 41502085, and 41902214);the National Key Technology Research and Development Program of the Ministry of Science and Technology of China (2015BAB05B04, 2018YFC0604005);the China Geological Survey Bureau (JYYWF20183702, JYYWF20180602)
The Baleigong granites, located in the western part of the southwestern Tianshan Orogen(Kokshanyan region, China), records late Paleozoic magmatism during the late stages of convergence between the Tarim Block and the...
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...
supported by the China Geological Survey under grants No.1212011120185 and 1212011221111;the Ministry of Land and Resources of China under a grant Sinoprobe-02;the Ministry of Science and Technology of China under a grant 2006DFB21330
Selected geological data on Early Cretaceous strata, structures, magmatic plutons and volcanic rocks from the Kunlun to Himalaya Mountains reveal a new view of the Early Cretaceous paleo-tectonics and the related geod...
supported by the National Basic Research Program of China(Grant No.2012CB416701);National Natural Science Foundation of China(Grant Nos.41330208;41572200);National Science and Technology Support Program(Grant No.2011BAB04B02);the Jiangxi Geological Exploration Fund(Grant No.20100112);Jiangxi Science and Technology Project(Grant No.20122BBG70068)
The Zhuxi ore deposit is a super-large scheelite(copper) polymetallic deposit discovered in recent years. It grew above copper/tungsten-rich Neoproterozoic argilloarenaceous basement rocks and was formed in the contac...
part of the ongoing project "Superimposed tectonic activities and large-scale oreforming processes of the Hinggan-Mongolia Orogenic Belt";financially supported by the State Basic Research Program of China(2013CB429805)
The Hashitu molybdenum deposit is located in the southern part of the Great Hinggan Range, NE China. Molybdenum mineralization is hosted by and genetically associated with monzogranite and porphyritic syenogranite. Sr...
financially supported by the National Science and Technology Major Project(No. 2011ZX05008-001);the National Natural Science Foundation of China(No.40739906);the Chinese State 973 Project(No. 2011CB201100)
New whole-rock major and trace elements, and zircon U Pb and Hf-Nd isotope compositions are reported for the Karamay dikes, enclaves, and host granites in the West Junggar, NW China. Zircon U -Pb dating of the l(aram...
financially supported by the National Key Basic Research Program of China (Nos. 2013CB429802 and 2013CB429803);the National Natural Science Foundation of China (No. 41272077);by the Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan (No. GPMR201104)
Zircon U-Pb ages, Hf isotope data and whole-rock major and trace element data for the Middle to Late Ordovician gabbros and granites in the Erguna Massif, NE China were presented in this paper. The petrogenesis of the...
supported by National Natural Science Foundation of China (Grant Nos. 41190073, 41372198 and 40825009);National Basic Research Program of China (Grant No. 2014CB440901);State Key Laboratory of Ore Deport Geochemistry, Chinese Academy of Sciences (Grant No. 201301);Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (Grant No. GIGCAS-135-Y234 151001)
High εNd(t)-εHf(t) granites are robust evidence for crustal growth. In this paper we report results of petrologic, geochronological and geochemical investigations on the Huashiban granites from the Ailaoshan tec...
Supported by the National Natural Science Foundation of China (40972198);the National Key Basic Research and Development Program of China(2010CB732001)
Weathered troughs are frequently encountered in granites. They can cause problems to tunneling in the rocks and have to be properly addressed. The structures or spatial shapes of weathered troughs were seldom clarifie...
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...