| 河南淅川寨沟钒矿床地质特征与矿床成因研究 |
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| 引用本文： | 卢清月.河南淅川寨沟钒矿床地质特征与矿床成因研究[J].四川地质学报,2013(2):158-161. |
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| 作者姓名： | 卢清月 |
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| 作者单位： | 河南省地质矿产勘查开发局第一地质勘查院,河南南阳473000 |
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| 摘 要： | 首次对寨沟钒矿成矿地质背景、矿体特征、矿石特征及矿床成因进行了系统研究,研究结果表明,该矿床产于寒武系水沟口组硅质岩、泥岩中,空间分布严格受地层及背斜构造双重控制,矿体呈隐伏—半隐伏状态,呈现鞍状、层状分布于背斜的转折端及两翼;成矿时间为寒武纪早期,钒主要来源于前寒武系地层,矿床形成于滨海至浅海环境中,矿床属滨海至浅海沉积型层控矿床。
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| 关 键 词： | 钒矿 地质特征 矿床成因 淅川寨沟 |
Geological Features and Ore Genesis of the Zhaigou Vanadium Deposit in Xichuan,Henan |
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| LU Qing-yue.Geological Features and Ore Genesis of the Zhaigou Vanadium Deposit in Xichuan,Henan[J].Acta Geologica Sichuan,2013(2):158-161. |
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| Authors: | LU Qing-yue |
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| Institution: | LU Qing-yue (No. 1 Geological Exploration Institute, Henan Bureau of Geology and Exploration and Development of Mineral Resources, Nanyang, Henan 473000) |
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| Abstract: | The Zhaigou V deposit is hosted in siliceous rock and mudstone of the Cambrian Shuigoukou Formation and controlled by stratigraphical horizon and anticline structure. The orebodies occur as saddle and stratified form in limbs and turning end of the Jiangjunzhai anticline. The deposit was formed in the Early Cambrian coastal and neritic environment, V was derived from Precambrian strata. The deposit is a coast~tl and early Cambrian sedimentary one. |
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| Keywords: | V deposit geological feature ore genesis Zhaigou Xichuan |
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