Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (6): 1811-1822.doi: 10.13278/j.cnki.jjuese.20200052

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Controlling Effect of Mesozoic Tectonic Activities on Present Karst Groundwater Occurrence in Central Mountain Area of Shandong Province

Liu Yuanqing1, Zhou Le1, Li Wei1, Wang Xinfeng1, Ma Xuemei1, Lü Lin1, Yin Kai2, Meng Shunxiang1   

  1. 1. Center for Hydrogeology and Environmental Geology Survey, China Geological Survey, Baoding 071051, Hebei, China;
    2. Shandong Zhongcheng Geotechnial Engineering Limited Company, Yantai 264000, Shandong, China
  • Received:2020-03-03 Online:2021-11-26 Published:2021-11-24
  • Supported by:
    Supported by the Project of China Geological Survey (DD20190259,DD20160289,12120114010802,12120114010801)

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Abstract: Influenced by the Mesozoic tectonic movement, faults, and folds occurred in the central mountain area of Shandong, the strata tilted, strata, and forming a series of graben-semi-graben basins with extensional detachment and Yanshanian magmatic intrusion. By taking Laiwu basin as an example, the influence of Mesozoic tectonic activities on the present karst groundwater occurrence was studied by means of hydrogeological survey, data statistics, drilling construction, geological outcrop observation, and analysis of soluble components of carbonate rocks. The results show that it has typical hydrogeological characteristics of basin-mountain structure in the central mountain area of Shandong. The hydrogeological characteristics of the south and north sides of the basin are different. The interlayer collapse, voids, and fractured rock zones formed by the regional decollement structure make the Lower Cambrian Zhushadong Formation aquifer show "stratiform". The dissolution fissures and caves formed by the hydrothermal mixed karstification are good space for the occurrence of karst groundwater. The interlayer corrosion fissures and faults formed by Mesozoic detachment structure and hydrothermal karst activity are connected in the same period or later, forming a three-dimensional karst groundwater network. The karst groundwater flows and accumulates along the network, and forms the unique characteristics of karst groundwater occurrence in the central mountain area of Shandong.

Key words: hydrogeology, decollement structure, hydrothermal dissolution, central mountain area of Shandong Province, tectonic movement, karst groundwater

CLC Number: 

  • P641.6
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