Chen Bin
Professor
Earth and Space Sciences
South University of Science and Technology of China
China
Biography
professor. 1985 NianAnd 1988 in Changchun Institute of Geology (now Jilin University) were Bachelor (geology) and master's degree (petrology); in 1991 in Peking University Department of geology doctoral degree (petrology). 1991 onwards at Peking University to teach in 2014 in 9 monthly income of Hefei University of Technology to help build Isotope Laboratory, 2017 , joined the South University of Technology. Long engaged in geology, geochemistry teaching and research work, published more than 50 papers. Has presided over the National Outstanding Youth Fund, the National Natural Science Focus Fund, Ministry of Science and Technology 973 project two projects and other research projects more than 10 items. 2014-2016 Annual Elsevier high earth and planetary sciences cited scholars.
Research Interest
(1) magma origin, evolution and geodynamic background; (2) the mechanism of polymetallic mineralization related to granite; (3) isotope geochemical tracing, simulation; (4) the application of nonstandard stable isotopes in the field of magmatic-hydrothermal system evolution, continental weathering and marine depositional environments, and planetary science.
Publications
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Chen CJ, Chen B,Wang ZQ, Li Z, (2016) Important role of magma mixing in generating the Mesozoic monzodioritic-granodioritic intrusions related to Cu mineralization Tongling East China evidence from petrological and in situ Sr-Hf isotopic data. Lithos 248-251:80-93.
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Chen B, Chen W, Chen YJ, Sun KK, Sun H, (2017) Lithium isotope behaviour during partial melting of metulationiments from the Jiangnan orogeny, South China Implications for the origin of REE tetrad effect of F-rich granite And associated rare-metal mineralization.
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Chen B, Huang C, Sun KK, Gu HO, (2017) Lithium isotopic constraints on the origin of I- and A-type granites from East Junggar (NW China) of the Central Asian Orogenic Belt Implications for Li isotopic fractionation During crumbal anatexis.
