Germanium isotope geochemistry: analysis, fractionation mechanisms and geochemical tracing
来源期刊：矿物学报2015年第S1期
论文作者：戚华文 Olivier Rouxel Yu-Miao Meng Rui-Zhong Hu
文章页码：1129 - 1130
摘 要：<正>Introduction Since Ge isotope is a new nontraditional isotope,the accumulated Ge isotope literatures are quite limited.The available researches mainly focused on two aspects:（1）the measurement of Ge isotopic compositions of geological and extraterrestrial materials,such as igneous rocks,marine sediments,seafloor hydrothermal fluids,hydrothermal Fe-oxyhydroxides,terrestrial high-temperature geothermal fluids,sphalerite,and iron meteorites;and（2）theoretical prediction of germanium isotope fractionation.
戚华文1，Olivier Rouxel2，Yu-Miao Meng1，Rui-Zhong Hu1
1. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences2. IFREMER, Centre de Brest, Dept.Géosciences Marines
摘 要：<正>Introduction Since Ge isotope is a new nontraditional isotope,the accumulated Ge isotope literatures are quite limited.The available researches mainly focused on two aspects:（1）the measurement of Ge isotopic compositions of geological and extraterrestrial materials,such as igneous rocks,marine sediments,seafloor hydrothermal fluids,hydrothermal Fe-oxyhydroxides,terrestrial high-temperature geothermal fluids,sphalerite,and iron meteorites;and（2）theoretical prediction of germanium isotope fractionation.
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