| 云南砚山红舍克原生及堆积型铝土矿 |
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| 引用本文： | 刘汉和.云南砚山红舍克原生及堆积型铝土矿[J].云南地质,2007,26(1):32-40. |
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| 作者姓名： | 刘汉和 |
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| 作者单位： | 云南省有色地质勘查院曲靖院,云南,曲靖,655000 |
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| 摘 要： | 红舍克铝土矿分为沉积和堆积型两类,受上二叠统(P2l)含矿层控制明显:沉积矿位于上段(P2l2)下部,堆积矿位于沉积铝土矿上覆层。
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| 关 键 词： | 铝土矿 沉积及堆积型 成因探讨 砚山云南 |
| 文章编号： | 1004-1885（2007）-032-09 |
| 收稿时间： | 2006-08-14 |
| 修稿时间： | 2006-08-14 |
HONGSHEKE ORIGINAL AND SECONDARY BAUXITE DEPOSITIN YANSHAN, YUNNAN |
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| LIU Han-he.HONGSHEKE ORIGINAL AND SECONDARY BAUXITE DEPOSITIN YANSHAN, YUNNAN[J].Yunnan Geology,2007,26(1):32-40. |
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| Authors: | LIU Han-he |
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| Institution: | Qujing Branch, Yunnan Nonferrous Geoexploration Institute, Qujing 655000 |
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| Abstract: | This bauxite deposit can be divided into 2 types of sedimentation and accumulation,which are controlled evidently by the Upper Permian(P2l) ore-bearing bed.The former type ore deposit is in the lower part of Upper Permian Upper Member(P2l2);the latter one is in the Quaternary accumula tion horizon near the sedimentary type bauxite deposit. |
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| Keywords: | Bauxite Sedimentation and Accumulation Types Genesis Discussion Yanshan Yunnan |
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