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Lithogeochemistry and Metamorphism of the Early Proterozoic Xingzi Group of Lu Shan Area, Jiangxi Province
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    Abstract:

    The early Proterozoic Xingzi Group was subjected to regional dynamothermal meta- morphism of Luliang period，dominated by low amphibolite facies with temperature 530-600 C and pressure 400一570 MPa. On the basis of its rock association and lithogeo chemistry，it is inferred that the Xingzi Group was formed in an epicontinental environment

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金文山,赵风清,甘晓春,王祖伟,1996,江西庐山地区早元古代星子群变质作用和岩石地球化学特征[J].岩石矿物学杂志,15(1):1~9. Jin Wenshan, Zhao Fengqing, Gan Xiaochun, Wang Zuwei,1996,Lithogeochemistry and Metamorphism of the Early Proterozoic Xingzi Group of Lu Shan Area, Jiangxi Province[J]. Acta Petrologica et Mineralogica,15(1):1~9.

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