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

    • Institute of Geology, Chinese Northwest Geoexploration Norferrous Bureau, Xi'an 710054, China

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    • Received Date: August 06, 2000
    • Revised Date: May 05, 2001
    • Published Date: June 04, 2001
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      • Abstract
    • 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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      • References (5)
    • 高章鉴,罗才让,郭健,等.青海省柴达木盆地周边地区早古生代大地构造背景及成矿意义的初探[J].西北金属矿产地质,1998,1(2).
      祁思敬,李英.秦岭热水沉积型铅锌(铜)矿床[M].北京:地质出版社,1993.
      李福东,张汉文,等.鄂拉山地区热水成矿模式--以铜为主多金属[M].西安:西北大学出版社,1993.
      Stanton R L.Constitutional features and some exploration implications of three zinc-bearing stratiform skarns of eastern Australia[C].Trans Instn Min Metall (Sect B:Appl Earth Sci).1986,96:B37-B57.
      Einaudi M T. Skans deposits[J].Economic Geology Seventy-Fifth Anniversary Volume,1981.
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