| 安化县大溶溪白钨矿床地质特征及成因 |
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| 引用本文： | 王峰.安化县大溶溪白钨矿床地质特征及成因[J].湖南地质,1993,12(3):182-184. |
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| 作者姓名： | 王峰 |
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| 作者单位： | 湖南省湘安钨矿 安化 |
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| 摘 要： | 大溶澳白钨矿床,赋存于震旦系南沱砂岩中,为层状、似层状矿床,含矿4层,具开采价值的为上部I矿层,白钨矿为矿石中单一的有用矿物,平均WO_3为0.486％,成矿作用与大神山花岗岩侵入作用有关,属沉积一改造型层控白钨矿床。
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| 关 键 词： | 白钨矿床 地质特征 矿床成因论 |
Genesis and Geological Characteristic of Scheelite Deposit in Darongxi,Anhua |
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| Wang Feng.Genesis and Geological Characteristic of Scheelite Deposit in Darongxi,Anhua[J].Hunan Geology,1993,12(3):182-184. |
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| Authors: | Wang Feng |
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| Institution: | Xiangan tungsten mine of Hunan |
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| Abstract: | Darongxi scheelite deposit occur in sand of lento formation, Sinian system. Orebody presents bed or stratotd, having four beds orebodies, Upper I orebed is valule for mining, Scheelite is only usable mineral, Av-erage content of WO_3:0.486%. Metallogenesis closely relates with intrusion of Dacheng mountain granite. It be-longs to sedimentary-reformation type strata-bound scheelite deposit. |
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| Keywords: | Scheelite deposit Geological characteristic Deposit genesis |
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