| 陕西省勉县白云寺铅锌矿床地质特征 |
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| 引用本文： | 陈智强,王创新,闫贺龙.陕西省勉县白云寺铅锌矿床地质特征[J].陕西地质,2010,28(1):30-33. |
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| 作者姓名： | 陈智强 王创新 闫贺龙 |
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| 作者单位： | 陕西省地矿局西安地质矿产勘查开发院,西安,710100 |
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| 摘 要： | 勉县白云寺铅锌矿床位于秦岭复合造山带勉略古岛弧隆起带之勉略蛇绿构造混杂岩带东段，由2条铅锌矿体组成，矿体呈规则脉状赋存于层内韧脆性断裂中，含矿地层为泥盆-石炭系金家河岩组。矿床类型为变质热液型。
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| 关 键 词： | 勉县白云寺 铅锌矿床 地质特征 |
METALLOGENESIS AND GEOLOGICAL FEATURES OF BAIYUNSI LEAD-ZINC DEPOSIT IN MIANXIAN COUNTY,SHAANXI PROVINCE |
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| Chen Zhi-qiang,Wang Chuan-gxin,Yan He-long.METALLOGENESIS AND GEOLOGICAL FEATURES OF BAIYUNSI LEAD-ZINC DEPOSIT IN MIANXIAN COUNTY,SHAANXI PROVINCE[J].Geology of Shaanxi,2010,28(1):30-33. |
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| Authors: | Chen Zhi-qiang Wang Chuan-gxin Yan He-long |
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| Institution: | Chen Zhi-qiang,Wang Chuan-gxin,Yan He-long(Xi'an Institute of Geology and Minerals,Shaanxi Bureau of Geology and Mineral Resources,Xi'an 710100) |
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| Abstract: | Tectonically, the Baiyunsi lead-zinc deposit is situated in the east part of the Mianlue structurally ophiolitic melange zone of the Mianlue old island-arc upheave zone within the Qinling combined orogenic belt. The deposit is composed of two lead-zinc orebodies, hosted in the ductile-brittle fault at vein-type. The host of mineralization is in the Jinjiahe Formation of the Devonian-Carboniferous system. The type of the deposit is attributed to hydrothermal metamorphism. |
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| Keywords: | Baiyusi in Mianxia lead-zinc deposit geological feature metallogenesis |
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