吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (6): 1811-1822.doi: 10.13278/j.cnki.jjuese.20200052
刘元晴1, 周乐1, 李伟1, 王新峰1, 马雪梅1, 吕琳1, 尹凯2, 孟顺祥1
Liu Yuanqing1, Zhou Le1, Li Wei1, Wang Xinfeng1, Ma Xuemei1, Lü Lin1, Yin Kai2, Meng Shunxiang1
摘要: 为了掌握中生代构造运动以来鲁中山区岩溶地下水富集规律,以莱芜盆地为例,通过水文地质调查及数据统计分析、钻探施工、地质露头观测、碳酸盐岩可溶组分分析等方法,对中生代构造活动特征、岩浆活动特征,及其对岩溶地下水赋存规律的控制作用进行研究。结果表明:鲁中山区具有典型盆-山结构水文地质特征,盆地南北两侧水文地质特征不尽相同;区域滑脱构造形成的层间虚脱、空隙、碎裂岩带,使得鲁中山区下寒武统朱砂洞组含水层表现为"似层状"特征;热液混合岩溶作用形成的溶蚀裂隙、洞穴可成为岩溶地下水良好的赋存空间;由中生代滑脱构造及热液岩溶活动形成的岩溶介质环境受同期或后期层间溶蚀裂隙及断层沟通,形成立体的岩溶地下水网络。岩溶地下水沿该网络径流、富集,形成鲁中山区特有的岩溶地下水赋存特征。
中图分类号:
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