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。
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.
引文
陈平,柴东浩.1997.山西铝土矿地质学研究[M].太原:山西科学技术出版社,52.
韩颖,阎世龙,马汉田,等.2008.山西六大盆地地下水资源及其环境问题调查评价[M].北京:地质出版社,249-250.
蒋辉,郭训武.2007.专门水文地质学[M].北京:地质出版社.
靳妙杰,贠孟超,王凤宇,等.2017.山西省平陆县西窑矿区铝土矿补充勘探报告[R]山西省地球物理化学勘查院.
靳妙杰,赵跃鹏,李帅,等.2015.山西省平陆县黄土岭一带铝土矿勘探地质报告[R]山西省地球物理化学勘查院.
梁永平,韩行瑞.2013.中国北方岩溶地下水环境问题与保护[M].北京:地质出版社,53-63.
山西省地质勘查局.1972.运城三门峡1:20万区域地质调查报告[R].
山西省地质矿产局.1989.山西省区域地质志[M].北京:地质出版社,587.