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山西平陆县东部铝土矿床水文地质条件

Hydrogeological conditions of Bauxite deposit in the eastern Pinglu county,Shanxi Province

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【作者】 靳妙杰贠孟超赵跃鹏孙海亮

【Author】 JIN Miao-jie;YUN Meng-chao;ZHAO Yue-peng;SUN Hai-liang;Shanxi Geophysical and Chemical Exploration Institute;

【机构】 山西省地球物理化学勘查院

【摘要】 平陆县东部铝土矿床地下水类型分为:松散岩类孔隙水,碎屑岩类裂隙、孔隙水,碳酸盐岩裂隙岩溶水,变质岩和岩浆岩裂隙水等4种。其中碳酸盐岩裂隙岩溶水水量最为丰富,属于单斜顺置型岩溶水系统。由于地下岩溶水的补给量明显大于排泄量,故推测黄河水下具有尚未发现的岩溶泉存在,并为今后进一步对该区岩溶水的研究提供一定的帮助。

【Abstract】 Groundwater of bauxite deposits in eastern Pinglu County can be classified into four types: pore water in loose rocks,fractured-pore water in clastic rocks, carbonate fissure karst water, fractured water in metamorphic rock and magmatic rock. Among them, the carbonate fissure karst water is the most abundant and belongs to the monoclinic order type karst water system. Since the recharge of underground karst water is obviously greater than the discharge, it is presumed that there are undiscovered karst springs under the Yellow River, which will stimulate further study of karst water in this area in the future.

【基金】 山西省地质勘查基金管理中心两权价款项目(编号:晋国土资办函[2017]265号)资助
  • 【文献出处】 矿产勘查 ,Mineral Exploration , 编辑部邮箱 ,2019年02期
  • 【分类号】P641.463
  • 【被引频次】6
  • 【下载频次】36
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