青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义
Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai
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摘要: 热水沉积成因层矽卡岩在青海省肯德可克金矿区非常发育。其产出特征、结构、构造及与岩体的关系等与接触交代型矽卡岩都有显著的区别。层矽卡岩是该区金矿化主要控矿因素之一,同时也是重要区域找矿标志。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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Keywords:
- Hydr othermal fluid sediment /
- stratiform skarns /
- Kendekoke gold deposit /
- Qinhai
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