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 compositi...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.展开更多
BACKGROUND A spectrum of strategically critical metals, such as gallium(Ga), germanium(Ge) and indium(In), with promising applications in green and high-tech fields, are produced as byproducts of zinc ores in a variet...BACKGROUND A spectrum of strategically critical metals, such as gallium(Ga), germanium(Ge) and indium(In), with promising applications in green and high-tech fields, are produced as byproducts of zinc ores in a variety of Pb-Zn deposits, such as magmatic-hydrothermal porphyry-skarn-vein type.展开更多
文摘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.
基金jointly funded by the National Key Research and Development Program of China (No.2021YFC2900300)the National Natural Science Foundation of China (No.42022020)。
文摘BACKGROUND A spectrum of strategically critical metals, such as gallium(Ga), germanium(Ge) and indium(In), with promising applications in green and high-tech fields, are produced as byproducts of zinc ores in a variety of Pb-Zn deposits, such as magmatic-hydrothermal porphyry-skarn-vein type.
