| 小柳沟铜钨多金属矿区地质特征 |
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| 引用本文： | 张胜业,李杰,等.小柳沟铜钨多金属矿区地质特征[J].地质与勘探,2002,38(4):33-35,40. |
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| 作者姓名： | 张胜业 李杰 |
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| 作者单位： | 甘肃有色地质勘查局四队,张掖,734012 |
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| 摘 要： | 小柳沟铜钨矿矿床成因类型属层控改造型，在其形成过程中，各种地质因素相互配合，相互作用，共同制约着矿体的分布特征，形状产状，规模，品位及其矿物组合。在诸多的控矿地质因素中，有利的地层是成矿的前提基础，适宜的岩石构造环境是成矿的必要场所，充分的岩浆岩条件是成矿的动力源泉。
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| 关 键 词： | 铜钨矿床 控矿地质因素 层控改造型 形态产状 品位 构造环境 |
| 文章编号： | 0495-5331(2002)04-0033-04 |
THE GEOLOGICAL CHARACTERS OF XIAOLIUGOU Cu-W DEPOSIT |
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| ZHANG Sheng-ye,LI Jie,ZHOU Ji-qiang,ZHANG Quan.THE GEOLOGICAL CHARACTERS OF XIAOLIUGOU Cu-W DEPOSIT[J].Geology and Prospecting,2002,38(4):33-35,40. |
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| Authors: | ZHANG Sheng-ye LI Jie ZHOU Ji-qiang ZHANG Quan |
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| Abstract: | The Xiaoliugou Cu-W deposit is controlled by strata and has been rebuilt in late time. During forming stage, various geological factors controlled ore distribution, forming-scale, grade and mineral assemblages. In the all geological factors, the stratum cell was precondition of mineralization. Suitable petrology-structure environments were essential condition. Magmatic activities were dynamic sources for mineralization. |
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| Keywords: | Xiaoliugou Cu-W deposit geological factors stratum structure magma |
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