| 卡乌留克塔格铁磷矿区水文地质特征探析 |
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| 引用本文： | 郗国庆,梁中朋,杨煊.卡乌留克塔格铁磷矿区水文地质特征探析[J].化工矿产地质,2012(3):143-148. |
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| 作者姓名： | 郗国庆 梁中朋 杨煊 |
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| 作者单位： | 中化地质矿山总局地质研究院,河北涿州072754 |
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| 摘 要： | 通过对卡乌留克塔格矿区自然地理特征及地质特征的分析,认为矿区的地下水主要为第四系孔隙水和基岩裂隙水,其补给来源一是降雨,二是地表水,三是山区地下暗流。矿山开采后对水资源环境的影响主要会引起地面沉陷,地下水位下降。应采取先探后采.边采边探的生产安全措施。
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| 关 键 词： | 自然地理 水文地质 环境影响 卡乌留克塔格矿区 |
RESEARCH ON HYDROGEOLOGIC FEATURE OF KAWULIUKE TAG IRON-PHOSPHORITE DISTRICT |
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| Institution: | Xi Guoqing Liang Zhongpeng Geological Institute of China Chemical Geology and Mine Bureau, Zhuozhou, Hebei, 072754, China |
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| Abstract: | Based on the analysis of physiographic and geological features of Kawuliuke Tag district, ground water of this area are mainly quaternary pore water and bedrock fissure water .there are three sources of recharge which are rainfall, surface water and mountain underflow. Mining can influence Water resource environment, result in ground settlement and groundwater recession. Two measures for safe productionshould have been adopted, namely, mining flowing exploration and mining together with exploration. |
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| Keywords: | physiographic features hydrogeology environmental influences Kawuliuke Tag district |
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