| 黔西林泉片区表层岩溶带发育特征及供水 |
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| 引用本文： | 王若帆.黔西林泉片区表层岩溶带发育特征及供水[J].四川地质学报,2014,34(3):433-436. |
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| 作者姓名： | 王若帆 |
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| 作者单位： | 贵州省地质矿产勘查开发局114地质大队,贵州 遵义,563000 |
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| 摘 要： | 贵州省黔西县林泉片区属于深切河谷斜坡地带,区内地下水位受乌江期隆升作用埋深大,不利于地下水的开发利用;且区内缺水人口分散分布于河谷斜坡地带,不利于集中供水。所以对区内表层岩溶带发育及表层带岩溶水分布特征的研究,是解决区内缺水问题的关键。
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| 关 键 词： | 表层岩溶带 深切河谷 地下水 林泉 |
Surface Karst Water Development and Water Supply in the Linquan Area,Qianxi, Guizhou |
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| WANG Ruo-fan.Surface Karst Water Development and Water Supply in the Linquan Area,Qianxi, Guizhou[J].Acta Geologica Sichuan,2014,34(3):433-436. |
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| Authors: | WANG Ruo-fan |
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| Institution: | WANG Ruo-fan (No. 114 Geological Team, Guizhou Bureau of Geology and Mineral Resources, Zunyi, Guizhou 563000) |
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| Abstract: | The Linquan area in Qianxi, Guizhou lies in an incised valley characterized by karst development. This has a discussion on surface karst water development and water supply in this region. |
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| Keywords: | surface karst zone slope zone of incised valley water supply Linquan |
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