| 东坪金矿床充水因素探讨 |
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| 引用本文： | 吕作刚,穆生莉.东坪金矿床充水因素探讨[J].地质找矿论丛,1997,12(4):73-79. |
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| 作者姓名： | 吕作刚 穆生莉 |
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| 作者单位： | 武警黄金第八支队!河北遵化，064200 |
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| 摘 要： | 东坪金矿赋存偏碱必杂岩体中，所处水文地质单元为低山分水岭近侧的基岩裂隙水区，东坪沟是矿区唯一的地表水体，地上水有第四系孔隙水和基岩裂隙水，矿床充水因素主要为地表水和第四系也隙水，其次为基岩裂隙水，基岩裂隙水直接渗漏到矿坑，地表水和第四系孔隙水通过基岩裂隙渗漏到矿坑，东坪金矿床属以基岩裂隙水直接充水，地表水和和纱孔隙之间接充水的水文地质条件中等类型的矿床。
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| 关 键 词： | 含水层 充水因素 金矿床 水文地质 |
| 收稿时间： | 1997/8/11 0:00:00 |
| 修稿时间： | 1997/9/22 0:00:00 |
DISCUSSION ON WATER-FILLING FACTORS IN DONGPING GOLD MINE, HEBEI PROVINCE |
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| L&#;Zhuogang and Mu Shengli.DISCUSSION ON WATER-FILLING FACTORS IN DONGPING GOLD MINE, HEBEI PROVINCE[J].Contributions to Geology and Mineral Resources Research,1997,12(4):73-79. |
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| Authors: | L&#;Zhuogang and Mu Shengli |
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| Institution: | the 8th branch of Plice Army |
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| Abstract: | ongping gold mine is located in a sub-alkline complex which occurs near the medium-lowmountain watershed. Hydrogeologically the mining area is of porous water domain of basement.Dongpinfggou rber is the only one surface water body. Underground water consists of Quaternaryporous water and the basement fractural water- The surface water and Quaternary Porous watesare the main factors for water-flow-in in the mine then is the basement fractural water The for-mer two permeate to the later and flow in drifts eventually. |
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| Keywords: | Dongping aquifer Water-filling factor |
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