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GAO Zhang-jian, LUO Cai-rang, JING Ji-feng. Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai[J]. Northwestern Geology, 2001, 34(2): 50-53.
Citation: GAO Zhang-jian, LUO Cai-rang, JING Ji-feng. Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai[J]. Northwestern Geology, 2001, 34(2): 50-53.

Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai

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  • Received Date: August 06, 2000
  • Revised Date: May 05, 2001
  • Published Date: June 04, 2001
  • The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in Kendekoke gold deposit,Qinhai province.And their development features,textures,structures and the relation with magma intrusion are obviously different from the skarns of contact metasometic origin type.The stratiform skarn is a major factor of gold mineralization control and the regional ore-searching criteria.
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