东昆仑阿斯哈金矿胶状黄铁矿成因及其成矿意义
Genesis of Colloidal Pyrite and Its Metallogenic Significance in Asiha Gold Deposit，East Kunlun
1.第四系；2.侏罗系；3.三叠系；4.二叠系；5.石炭系；6.奥陶—志留系；7.印支期花岗岩；8.印支期闪长岩；9.华力西期花岗闪长岩；10.华力西期闪长岩；11.华力西期超基性岩；12.加里东期花岗岩；13.加里东期闪长岩；14.岩脉；15.断层
东昆仑阿斯哈金矿胶状黄铁矿成因及其成矿意义 |
| 梁改忠,杨奎锋,范宏瑞,李兴辉 |
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Genesis of Colloidal Pyrite and Its Metallogenic Significance in Asiha Gold Deposit，East Kunlun |
| Gaizhong LIANG,Kuifeng YANG,Hongrui FAN,Xinghui LI |
| 图1 东昆仑造山带构造简图（a）［据 1.第四系；2.侏罗系；3.三叠系；4.二叠系；5.石炭系；6.奥陶—志留系；7.印支期花岗岩；8.印支期闪长岩；9.华力西期花岗闪长岩；10.华力西期闪长岩；11.华力西期超基性岩；12.加里东期花岗岩；13.加里东期闪长岩；14.岩脉；15.断层 |
| Fig.1 Structural sketch of East Kunlun orogenic belt（a）［modified after |
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