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The Material Sourece of a New Type of Copper Deposits—Evidence from Stable Isotopes
引用本文:颜文 甫为民 等. The Material Sourece of a New Type of Copper Deposits—Evidence from Stable Isotopes[J]. 中国地球化学学报, 1995, 14(2): 168-178. DOI: 10.1007/BF02873300
作者姓名:颜文 甫为民 等
作者单位:OpenLaboratoryofOreDepositGeochemistry,InstituteofGeochemistry,ChineseAcademyofSciences,Guiyang550002
摘    要:The new type of copper deposits concerned with in this paper are vein copper deposits found in the Lanping-Simao Rift Basin, Yunnan,China. As is indicated by H,O,C,S,Pb and Sr isotopes, water and mineralizers in the ore-forming fluids were derived from heated meteoric water and mantle, respectively.The metallic elements(Cu,Ag,Pb,Zn,As,Sb,Fe,REE,etc.)are characterized by a mixed source from the crust and the mantle.

关 键 词:铜矿床 物质来源 云南 稳定同位素 稀土元素 地质特征

The material source of a new type of copper deposits—Evidence from stable isotopes
Yan Wen,Li Chaoyang,Fu Weimin,Li Feng. The material source of a new type of copper deposits—Evidence from stable isotopes[J]. Chinese Journal of Geochemistry, 1995, 14(2): 168-178. DOI: 10.1007/BF02873300
Authors:Yan Wen  Li Chaoyang  Fu Weimin  Li Feng
Affiliation:(1) Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 550002 Guiyang;(2) Department of Territory, Kunming Engineering College, 650093 Kunming;(3) Present address: Shenyang University of Agriculture, Shenyang, China
Abstract:The new type of copper deposits concerned with in this paper are vein copper deposits found in the Lanping-Simao Rift Basin, Yunnan, China. As is indicated by H, O, C, S, Pb and Sr isotopes, water and mineralizers in the ore-forming fluids were derived from heated meteoric water and mantle, respectively. The metallic elements (Cu, Ag, Pb, Zn, As, Sb, Fe, REE, etc.) are characterized by a mixed source from the crust and the mantle. This project was granted by the Lab of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences.
Keywords:copper deposits of a new type  material source  stable isotope  Lanping-Simao Basin  Yunnan
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