J
Jia-Min Wang
Researcher at Chinese Academy of Sciences
Publications - 36
Citations - 1370
Jia-Min Wang is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Metamorphism & Zircon. The author has an hindex of 14, co-authored 30 publications receiving 799 citations. Previous affiliations of Jia-Min Wang include Ruhr University Bochum & Peking University.
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Highly fractionated granites: Recognition and research
TL;DR: In this article, the authors proposed that granites are an important sign indicating compositional maturity of the continental crust, and they are also closely related to the rare-elemental (metal) mineralization of W, Sn, Nb, Ta, Li, Be, Rb, Cs, REEs, etc.
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Highly fractionated Himalayan leucogranites and associated rare-metal mineralization
Fu-Yuan Wu,Xiao-Chi Liu,Zhi-Chao Liu,Rucheng Wang,Lei Xie,Jia-Min Wang,Wei-Qiang Ji,Lei Yang,Chen Liu,Gautam Prashad Khanal,Shao-Xiong He +10 more
TL;DR: The formation of the Himalaya was associated with the exhumation of high-grade metamorphosed rocks of the Higher Himalayan sequence (HHS) complex, which underwent amphibolite-, granulite- to eclogite-facies metamorphism and anatexis as discussed by the authors.
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Timing of Partial Melting and Cooling across the Greater Himalayan Crystalline Complex (Nyalam, Central Himalaya): In-sequence Thrusting and its Implications
TL;DR: In this article, the authors investigated the timing of crustal melting and cooling across the migmatites of the Greater Himalayan Crystalline Complex (GHC) in the Nyalam region, central Himalaya.
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Structural kinematics, metamorphic P–T profiles and zircon geochronology across the Greater Himalayan Crystalline Complex in south‐central Tibet: implication for a revised channel flow
TL;DR: In this paper, a revised channel flow model is proposed by considering the effect of heat advection and convection by melt and magma migration, which suggests that distributed processes like channel flow dominated during the growth of the Himalayan orogen, while discrete thrusting occurred in a later period as a secondary process.
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Initial subduction of the Paleo-Pacific Oceanic plate in NE China: Constraints from whole-rock geochemistry and zircon U–Pb and Lu–Hf isotopes of the Khanka Lake granitoids
Kai Liu,Kai Liu,Jinjiang Zhang,Simon A. Wilde,Jian-Bo Zhou,Meng Wang,Maohui Ge,Jia-Min Wang,Yi-Yun Ling +8 more