Earth Science Frontiers ›› 2010, Vol. 17 ›› Issue (2): 396-403.

• Article • Previous Articles     Next Articles

 Characteristics of isotopic geochemistry of Shuiyindong superlarge Carlin gold deposit in Guizhou.

WANG  Cheng-Hui, WANG  De-Gong, LIU  Jian-Zhong, DENG  Yi-Meng, LIU  Chuan-Qi, LI  Jian-Kang, CHEN  Fa-En   

  1. 1Graduate School, Chinese Academy of Geological Science, Beijing 100037, China
    2Institute of Mineral Resource, Chinese Academy of Geological Science, Beijing 100037, China
    3Guizhou Zijin Mining Limited Company, Zhenfeng 562200, China
    4No105 Team of Guizhou Bureau of Geological Exploration and Exploitation of Mineral Resources, Guiyang 550000, China
  • Received:2009-10-19 Revised:2009-10-28 Online:2010-03-15 Published:2010-04-05

Abstract:

 The Shuiyindong deposit is a superlarge gold deposit in Southwest Guizhou Province, which is famous for its high grade and super largescale. The geochemical study of isotopes such as S, Pb, C and O shows that the oreforming material may come from juvenile fluids and crustal rocks. Some isotopic data from other carlin deposits in YunnanGuizhouGuangxi area indicate that the mineralization of gold deposits in this area may closely relate to the evolution of juvenile fluids and some rocks that may be concealed under this area.

Key words: Shuiyindong gold deposit, geochemistry, isotope, sources of oreforming materials

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