文章摘要
靳妙杰,贠孟超,赵跃鹏,孙海亮.山西平陆县东部铝土矿床水文地质条件[J].矿产勘查,2019,(2):392-398
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
投稿时间:2018-12-17  
DOI:
中文关键词: 平陆县东部  地下水类型  铝土矿  岩溶水  山西
英文关键词: eastern Pinglu county, groundwater type, bauxite, karst water,Shanxi
基金项目: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。
作者单位
靳妙杰 山西省地球物理化学勘查院,运城 044000 
贠孟超 山西省地球物理化学勘查院,运城 044000 
赵跃鹏 山西省地球物理化学勘查院,运城 044000 
孙海亮 山西省地球物理化学勘查院,运城 044000 
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中文摘要:
      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。
英文摘要:
      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.
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