| 四川白玉连龙锡银多金属矿床地质特征及成因探讨 |
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| 引用本文： | 王显锋.四川白玉连龙锡银多金属矿床地质特征及成因探讨[J].四川地质学报,2008,28(3):204-207. |
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| 作者姓名： | 王显锋 |
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| 作者单位： | 四川省地质调查院,成都,610081 |
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| 摘 要： | 连龙锡银多金属矿床位于义敦岛孤带，是造山后岩浆作用形成的舍锡花岗岩带内一个重要中型矿床，共（伴）生有Cu、Pb、Zn等元素，并含有大量Bi矿物。该矿床赋存于“A”型花岗岩与富泥质的曲嘎寺组灰岩接触带，矿床类型为接触交代型多金属矿床。
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| 关 键 词： | 锡银多金属矿 地质特征 成因 四川白玉连龙 |
An Approach to the Geological Features and Genesis of the Lianlong Sn-Ag Polymetallic Deposit in Baiyu,Sichuan |
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| WANG Xian-feng.An Approach to the Geological Features and Genesis of the Lianlong Sn-Ag Polymetallic Deposit in Baiyu,Sichuan[J].Acta Geologica Sichuan,2008,28(3):204-207. |
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| Authors: | WANG Xian-feng |
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| Institution: | WANG Xian-feng ( Sichuan Geological Survey, Chengdu 610081 ) |
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| Abstract: | The Lianlong Sn-Ag polymetallic deposit is located in the Yidtm island arc belt. This is an important medium-sized deposit associated with Cu, Pb, Zn and Bi in the stanniferous granite belt formed by the post-orogenic magmatism. The deposit is a contact metasomatic one which is confined to contact between the A-type granite and politic-rich limestone of the Qugasi Formation. |
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| Keywords: | Sn-Ag polymetallic deposit geological features ore genesis Lianlong Baiyu Sichuan |
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