湖北郧县大柳钒矿地质特征及成因 |
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引用本文: | 门道改,伏雄.湖北郧县大柳钒矿地质特征及成因[J].科技信息,2011(27):422-423. |
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作者姓名: | 门道改 伏雄 |
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作者单位: | 河南省有色金属地质矿产局第三地质大队; |
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摘 要: | 从矿床产出特征、成矿物质来源、沉积环境、赋矿层位与含矿岩系及区域钒矿的对比等方面,对大柳钒矿成矿地质背景等特征进行研究。结果表明,大柳钒矿为赋存于早寒武世庄子沟组黑色岩系中沉积型钒矿,广泛分布于华北板块南缘的早寒武世庄子沟组黑色岩系中,具有良好的成矿条件和找矿前景。
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关 键 词: | 黑色岩系 钒矿 地质特征 矿床成因 大柳 |
The Geological Characterics and the Genesisof the Daliu Vanadium Deposit in Yunxian,Hubei Province |
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Abstract: | The authors studiedf the metallogenic background and geological characteristics of vanadium deposit in Daliu area in characteristics of occurrence,source of metallogenic material,sedimentary environment and lithofacies,and the comparison of ore-bearing horixon wirh one-bearing rock series and reginal vanadium deposits.The results showed that Daliu vanadium was a sedimintart one hosted in the black series of Lower Cambrian Zhuangzigou Formation,which was widely distributed in the southern edge of north china... |
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Keywords: | Black rock series Vanadium deposit Geological characteristics Genesis of deposit Daliu |
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