| 四川木里梭罗沟金矿床特征 |
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| 引用本文： | 喻安光,卢玫瑰,宋晓华,刘文武.四川木里梭罗沟金矿床特征[J].四川地质学报,2014(4):514-516. |
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| 作者姓名： | 喻安光 卢玫瑰 宋晓华 刘文武 |
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| 作者单位： | 四川省地质矿产勘查开发局区域地质调查队,成都610213 |
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| 摘 要： | 四川木里梭罗沟金矿床位于甘孜—理塘构造成矿带的南段、唐央复式背斜南东倾伏端(或唐央穹窿南缘),目前已探明储量属大型岩金矿床。矿体产于上三叠统曲嘎寺组蚀变基性火山岩中,受近东西向断裂控制。矿床具多期成矿特点,属构造蚀变岩型—中低温热液型金矿床。
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| 关 键 词： | 金矿床 控矿断裂 多期成矿 梭罗沟 |
Geological Features of the Suoluogou Au Deposit in Muli,Sichuan |
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| YU Anguang,LU Meigui,SONG xiaohua,LIU Wenwu.Geological Features of the Suoluogou Au Deposit in Muli,Sichuan[J].Acta Geologica Sichuan,2014(4):514-516. |
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| Authors: | YU Anguang LU Meigui SONG xiaohua LIU Wenwu |
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| Institution: | (Regional Geological Surveying Team, BGEEMRSP, Chengdu 610213) |
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| Abstract: | The Suoluogou Au deposit in Muli, Sichuan lies on the southern margin of the Tangyang dome in the southern section of the Garze-Litang tectonic-metallogenic belt. The deposit is confined to the altered basic volcanic rock of the Upper Triassic Qugasi Formation and controlled by nearly EW-trending fracture zone The deposit is a structural altered rock type one which was formed by multiple ore-formation. |
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| Keywords: | Au deposit ore control fracture multiple ore-formation Suoshi Gulley |
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