REE geochemistry of the Zhoutan Group metasedimentary rocks in central Jiangxi Province, Southeast China
Detailed REE and trace elements geochemical studies of the Zhoutan Group metasedimentary rocks in central Jiangxi Province, China, and rock-forming minerals such as garnet were conducted and the results showed that the REEs are partly present in the rock-forming minerals and are dominantly contained in the lattice of accessory minerals. In the process of metamorphism the REEs between garnet porphyroblast and rock and the partitioning of REEs between garnet and the host rock is obviously controlled by the chemical composition of the system. The REEs compositions of metamorphic veins and their minerals display remarked lanthanide tetrad effects and the element pairs Zr-Hf, Y-Ho, Pb-Nd and U-Th have also experienced a certain degree of fractionation with respect to the metasedimentary rocks and they can be used as discriminating indicators to some extent for the occurrence of fluid processes in the process of metamorphism of the Zhoutan Group.
作 者： HU Gongren LIU Congqiang YU Ruilian 作者单位： HU Gongren(Department of Environmental Science and Engineering, Huaqiao University, Quanzhou 362021, China;Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093,China)LIU Congqiang(Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China)
YU Ruilian(Department of Environmental Science and Engineering, Huaqiao University, Quanzhou 362021, China)
刊 名： 中国地球化学学报（英文版） 英文刊名： CHINESE JOURNAL OF GEOCHEMISTRY 年，卷(期)： 2009 28(2) 分类号： P59 关键词： REE garnet metasedimentary rock Zhoutan Group central Jiangxi Province