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

Previous Articles     Next Articles

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)

PDF (PC)

84

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
[1] Darnault C J G. Karst Aquifers:Hydrogeology and Exploitation[J]. Nato Security Through Science,2011:203-226.
[2] Andreo B. Introductory Editorial:Advances in Karst Hydrogeology[J]. Environment Earth Science,2012,65(8):2219-2220.
[3] 韩行瑞.岩溶水文地质学[M].北京:科学出版社,2015. Han Xingrui. Karst Hydrogeology[M]. Beijing:Science Press,2015.
[4] 梁永平,王维泰,赵春红,等.中国北方岩溶水变化特征及其环境问题[J]. 中国岩溶,2013, 32(1):34-42. Liang Yongping, Wang Weitai, Zhao Chunhong, et al. Variations of Karst Water and Environmental Problems in North China[J]. Carsologica Sinica, 2013,32(1):34-42.
[5] 于丽莎,潘晓东,曾洁,等.鲁中南泰莱盆地岩溶地下水赋存特征和找水规律[J]. 地质与勘探, 2019,55(1):170-179. Yu Lisha, Pan Xiaodong, Zeng Jie,et al. Occurrence Characteristic of Karst Groundwater and the Rule of Water Search in the Tailai Basin, Central-Southern Shandong Province[J]. Geology and Exploration, 2019,55(1):170-179.
[6] White W B. Conceptual Models for Karstic Aquifers[J]. Speleogenesis & Evolution of Karst Aquifers, 2003,1(1):11-16.
[7] Bakalowicz M. Karst Groundwater:A Challenge for New Resources[J]. Hydrogeology Journal,2005,13(1):148- 160.
[8] 阎长虹,王玉英,罗国煜,等.压性构造对岩溶发育的控制作用:以贵州普定地区为例[J]. 地质论评, 2008, 54(3):343-347. Yan Changhong, Wang Yuying, Luo Guoyu,et al. Compressive Structure's Control on the Karst Development[J]. Geological Review,2008,54(3):343-347.
[9] 刘元晴,周乐,李伟,等.鲁中山区下寒武统朱砂洞组似层状含水层成因分析[J].地质论评, 2019,65(3):653-663. Liu Yuanqing, Zhou Le, Li Wei, et al. Genetic Analysis of Lower Cambrian Zhushadong Formation Layered Aquifer in the Central Mountain Area of Shandong Province[J]. Geological Review,2019,65(3):653-663.
[10] 叶定衡,王新政,赵玉敏.中国新构造运动基本特征[J].中国地质科学院地质力学研究所所刊,1995(16):77-84. Ye Dingheng, Wang Xinzheng, Zhao Yumin. Neotectonics in China[J]. Bulletin of the Institute of Geomechnics CAGS, 1995(16):77-84.
[11] 肖楠森,高明.论新构造运动对地下水资源分布的控制作用[J].工程勘察,1982,10(4):1-6. Xiao Nansen, Gao Ming. Controlling Effect of Neotectonic Movement on Distribution of Groundwater Resources[J]. Geotechnical Investigation & Surveying,1982,10(4):1-6.
[12] 陈兰,尹海生,木合塔尔.新疆柴窝堡盆地新构造运动对地下水的影响[J].成都理工学院学报,2002,29(5):555-560. Chen Lan, Yin Haisheng, Muhe Taer. Effect of Neotectonic Movement on Groundwater in the Chaiwobao Basin of Xinjiang[J]. Journal of Chengdu University of Technology,2002,29(5):555-560.
[13] 吕金波,卢耀如,郑桂森,等.北京西山岩溶洞系的形成及其与新构造运动的关系[J].地质通报,2010,29(4):503-509. Lü Jinbo, Lu Yaoru, Zheng Guisen, et al. Formation of Karst Cave System and Its Relationship with Neotectonic Movement in Beijing Western Hills, Beijing, China.[J]. Geological Bulletin of China,2010,29(4):503-509.
[14] 周乐,刘元晴,李伟,等.山东大汶河流域中上游古近系含水岩组水文地质特征[J].中国地质,2019,46(2):316-327. Zhou Le, Liu Yuanqing, Li Wei, et al. Characteristics of the Paleogene Waterbearing Formation in the Middle and Upper Reaches of the Dawenhe River Basin, Shandong Province[J]. Geology in China,2019, 46(2):316-327.
[15] 张增奇,张成基,王世进,等.山东省地层侵入岩构造单元划分对比意见[J].山东国土资源,2014,30(3):1-23. Zhang Zengqi, Zhang Chengji, Wang Shijin, et al. Views on Classification and Contrast of Tectonic Units in Strata in Shandong Province[J]. Land and Resources in Shandong Province, 2014,30(3):1-23.
[16] 李少俊,李三忠,李玺瑶,等.鲁西地块新生代断层体系活动性与深部动力机制[J].海洋地质与第四纪地质, 2018,38(4):123-134. Li Shaojun, Li Sanzhong, Li Xiyao, et al. Activity of Cenozoic Fault System in the Luxi Block and Deep Dynamics[J]. Marine Geology & Quaternary Geology,2018,38(4):123-134.
[17] 李守军,郑德顺,蔡进功,等.鲁北和鲁西南地区古近纪盆地沉积特征与控制因素探讨[J].地质论评,2003,49(3):225-232. Li Shoujun, Zheng Deshun, Cai Jingong, et al. Sedimentary Characteristics and Controlling Factors of Basins in the North Shandong and Southwest Shandong in Palaeogene[J]. Geological Review,2003,49(3):225-232.
[18] 刘元晴,周乐,李伟,等.山东莱芜盆地西北缘古近系半固结含水岩组的特征及其成因[J]. 地球学报,2018, 39(6):737-748. Liu Yuanqing, Zhou Le, Li Wei, et al. The Characteristics and Genetic Analysis of the Paleogene Semi-Consolidated Water-Bearing Formation on the Northwestern Margin of Laiwu Basin, Shandong Province[J]. Acta Geoscientica Sinica,2018, 39(6):737-748.
[19] 贺可强,刘炜金,邵长飞.鲁中南岩溶水资源综合类型及合理调蓄研究[J].地球学报,2002,23(4):369-374. He Keqiang, Liu Weijin, Shao Changfei. The Comprehensive Type Classification and Proper Adjustment of Karst Water Resource in the Central-South Region of Shandong Province[J]. Acta Geoscientica Sinica,2002,23(4):369-374.
[20] 康凤新,徐军祥,张中祥.山东省地下水资源及其潜力评价[J].山东国土资源,2010,26(8):4-12. Kang Fengxin, Xu Junxiang, Zhang Zhongxiang. Groundwater Resources and Its Potential in Shandong Province[J]. Land and Resources in Shandong Province, 2010,26(8):4-12.
[21] 李三忠,王金铎,刘建忠,等.鲁西地块中生代构造格局及其形成背景[J].地质学报,2005,79(4):487-497. Li Sanzhong, Wang Jinduo, Liu Jianzhong, et al. Mesozoic Structure and Its Tectonci Setting in the Western Shandong Block[J]. Acta Geologica Sinica,2005,79(4):487-497.
[22] 吴智平,侯旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399. Wu Zhiping, Hou Xubo, Li Wei. Disscussion on Mesozoic Basin Patterns and Evolution in the Eastern North China Block[J]. Geotectonica et Metallogenia,2007,31(4):385-399.
[23] 李勇,钟建华,温志峰,等.印支运动对济阳坳陷构造形态形成演化的影响[J].地质论评,2006,52(3):321-330. Li Yong, Zhong Jianhua, Wen Zhifeng, et al. Effects of Indosinian Movements on Tectonic Formation and Evolution, Jiyang Depression[J]. Geological Review,2006,52(3):321-330.
[24] 张宏仁,张永康,蔡向民,等.燕山运动的"绪动":燕山事件[J].地质学报,2013,87(12):1779-1790. Zhang Hongren, Zhang Yongkang, Cai Xiangmin, et al. The Triggering of Yanshan Movement:Yanshan Event[J]. Acta Geologica Sinica,2013,87(12):1779-1790.
[25] 王瑜,孙立新,周丽云,等.燕山运动与华北克拉通破坏关系的讨论[J].中国科学:地球科学,2018,48(5):521-535. Wang Yu, Sun Lixin, Zhou Liyun, et al. Discussion on the Relationship Between the Yanshanian Movement and Cratonic Destruction in North China[J]. Science China:Earth Science,2018, 48(5):521-535.
[26] 张剑,李三忠,李玺瑶,等.鲁西地区燕山期构造变形:古太平洋板块俯冲的构造相响应[J].地学前缘,2017,24(4):226-238. Zhang Jian, Li Sanzhong, Li Xiyao, et al. Yanshanian Deformation of Luxi Area:Tectonic Response to the Paleo-Pacifc Plate Subduction[J]. Earth Science Frontiers,2017,24(4):226-238.
[27] 燕守勋,王桂梁,邵震杰,等.鲁西地壳隆升的伸展构造模式[J].地质学报,1996,70(1):1-11. Yan Shouxun, Wang Guiliang, Shao Zhenjie, et al. Extensional Tectonic Model of Crustal Elevation in Western Shandong[J]. Acta Geologica Sinica,1996,70(1):1-11.
[28] 牛树银,胡华斌,毛景文,等.鲁西地区地质构造特征及其形成机制[J].中国地质,2004,31(1):34-39. Niu Shuyin, Hu Huabin, Mao Jingwen,et al. Structure in Western Shandong and Its Genetic Mechanism[J]. Chinese Geology,2004,31(1):34-39.
[29] 张锡明,张岳桥,季玮.山东鲁西地块断层构造分布型式中生代沉积-岩浆-构造演化序列[J].地质力学学报,2007,13(2):163-172. Zhang Ximing, Zhang Yueqiao, Ji Wei. Fault Distribution Patterns of Luxi Block, Shandon, and Mesozoic Sedmentary-Magmatic-Structural Evolution Sequence[J]. Journal of Geomechanics,2007,13(2):163-172.
[30] 王世进,张成基,杨恩秀,等.鲁西地区中生代侵入岩期次划分[J].山东国土资源,2009,25(2):18-23. Wang Shijin, Zhang Chengji, Yang Enxiu, et al. Division of Mesozoic Intrusive Stages in Luxi Area[J]. Shandong Land and Resources, 2009,25(2):18-23.
[31] 李理,钟大赉,石秀朋,等.鲁西地区的滑脱构造及其形成的深部背景[J].自然科学进展,2008,18(6):651-660. Li Li, Zhong Dalai, Shi Xiupeng, et al. The Decollement Structure and Its Deep Background in Western Shandong Province[J]. Progress in Natural Science,2008,18(6):651-661.
[32] 申豪勇,梁永平,赵春红,等.古堆泉岩溶地下水系统特征及系统圈划[J]. 吉林大学学报(地球科学版), 2020,50(1):217-225. Shen Haoyong, Liang Yongping, Zhao Chunhong, et al. Hydro-Geological Characteristics and Demarcation of Gudui Spring Karst Groundwater System[J]. Journal of Jilin University(Earth Science Edition), 2020,50(1):217-225.
[33] 梁永平,王维泰.中国北方岩溶水系统划分与系统特征[J]. 地球学报,2010,31(6):860-868. Liang Yongping, Wang Weitai. The Division and Characteristics of Karst Water System in Northern China[J]. Acta Geoscientica Sinica,2010,31(6):860-868.
[34] White D E. Thermal Water of Volcanic Origin[J]. Bulletin of the Geological Society of America,1957,68:1637-1658.
[35] Langhrone B S, Graham R D. Structurally Controlled Hydrothermal Alteration of Carbonate Reservoirs:Introduction[J]. AAPG Bulletin, 2006,90(11):1635-1640.
[36] 李明诚.地壳中的热流体活动与油气运移[J]. 地学前缘,1995,2(3/4):155-161. Li Mingcheng. Hot Fluid Activity in Crust and Hydrocarbon Migration[J]. Earth Science Frontiers,1995,2(3/4):155-161.
[37] 金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J]. 地质学报, 2006, 80(2):245-253. Jin Zhijun, Zhu Dongya, Hu Wenxuan, et al. Geological and Geochemical Signatures of Hydrothermal Activity and Their Influence on Carbonate Reservoir Beds in the Tarim Basin[J]. Acta Geologica Sinica, 2006, 80(2):245-253.
[38] 朱东亚,孟庆强,解启来,等.塔里木盆地大理岩化储层发育特征[J].石油与天然气地质,2011,32(4):506-521. Zhu Dongya, Meng Qingqiang, Xie Qilai, et al. Characteristics of Marmorized Reservoirs in the Tarim Basin[J]. Oil &Gas Geology,2011,32(4):506-521.
[39] 刘元晴,周乐,李伟,等.山东莱芜盆地碳酸盐岩热液溶蚀特征及水文地质意义[J].现代地质,2020,34(1):199-206. Liu Yuanqing, Zhou Le, Li Wei, et al. Characteristics and Hydrogeological Siginificance of Hydrothermal Dissolution in Carbonate Rocks from Laiwu Basin, Shandong Province[J]. Geoscience, 2020,34(1):199-206.
[40] 胡海涛,许贵森.论构造体系与地下水网络[J].水文地质工程地质,1980(3):5-11. Hu Haitao, Xu Guisen. Discussion on Tectonic System and Groundwater Network[J]. Hydrogeology & Engineering Geology, 1980(3):5-11.
[1] Shen Haoyong, Liang Yongping, Zhao Chunhong, Tang Chunlei, Wang Zhiheng. Hydro-Geological Characteristics and Demarcation of Gudui Spring Karst Groundwater System [J]. Journal of Jilin University(Earth Science Edition), 2020, 50(1): 217-225.
[2] Lu Lijuan, Cai Zhourong, Huang Qiangtai, Yao Yongjian, Liu Hailing. Characteristics and Controlling Factors of Neotectonic Movement in South China Sea (SCS) and the Adjacent Areas [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 206-217.
[3] Ma Rong, Shi Jiansheng, Liu Jichao. Application of Artificial Endocrine Network Model in Studying of Hydrogeology Parameter [J]. Journal of Jilin University(Earth Science Edition), 2013, 43(3): 914-921.
[4] KANG De-jiang, ZHANG Bin-chi. Tectonic Movement of Buried Hill and Hydrocarbon Accumulation--An Example from Beier Depression in Hailaer Basin [J]. J4, 2009, 39(5): 767-772.
[5] CAO Qiang, YE Jia-ren, GUO Fei-fei, FENG Yong. Pressure Evolution in the Moliqing Fault-Depression, Yitong Basin [J]. J4, 2009, 39(4): 642-649.
[6] LIN Xue-yu. Historical Change and Prospect of Discipline Development of “Groundwater Science and Engineering” [J]. J4, 2007, 37(2): 209-0215.
[7] CUI Xue-hui，CHEN Hong-han,CHEN Hong-kun,QIN Yan-jun,LIU Da-wei. Regional Hydrogeology GIS System and AccessorialDesign for Engineering Based on ActiceX [J]. J4, 2006, 36(01): 91-0095.
[8] LIANG Xiu-juan, LIN Xue-yu, YU Jun. Application of Virtual Reality Technology in Hydrogeological Research [J]. J4, 2005, 35(05): 636-640.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] CHENG Li-ren, ZHANG Yu-jie, ZHANG Yi-chun. Ordovician Nautiloid Fossils of Xainza Region,Tibet[J]. J4, 2005, 35(03): 273 -0282 .
[2] LI Bing-cheng. Preliminary Studies on Holocene Climatic In Fuping,Shaanxi Province[J]. J4, 2005, 35(03): 291 -0295 .
[3] HE Zhong-hua，YANG De-ming，WANG Tian-wu，ZHENG Chang-qing. SHRIMP U[CD*2]Pb Dating of Zircons from Two-Mica Granite in Baga Area in Gangdise Belt[J]. J4, 2005, 35(03): 302 -0307 .
[4] CHEN Li， NIE Lei， WANG Xiu-fan， LI Jin. Seismic Risk Analysis of Some Electric Power Equipment Station in Suizhong[J]. J4, 2005, 35(05): 641 -645 .
[5] JI Hong-jin,SUN Feng-yue2,CHEN Man,HU Da-qian,SHI Yan-xiang,PAN Xiang-qing. Geochemical Evaluation for Uncovered GoldBearing Structures in Jiaodong Area[J]. J4, 2005, 35(03): 308 -0312 .
[6] CHU Feng-you, SUN Guo-sheng,LI Xiao-min,MA Wei-lin, ZHAO Hong-qiao. The Growth Habit and Controlling Factors of the CobaltRich Crusts in Seamount of the Central Pacific[J]. J4, 2005, 35(03): 320 -0325 .
[7] LI Bin, MENG Zi-fang， LI Xiang-bo, LU Hong-xuan, ZHENG Min. The Structural Features and Depositional Systems of the Early Tertiary in the Biyang Depression[J]. J4, 2005, 35(03): 332 -0339 .
[8] LI Tao, WU Sheng-jun, CAI Shu-ming, XUE Huai-ping, YASUNORI Nakayama. Simulation Analysis of the Storage Capacity Based on DEM Before and After Connecting to Yangtze River in Zhangdu Lake[J]. J4, 2005, 35(03): 351 -0355 .
[9] KUANG Li-xiong,GUO Jian-hua, MEI Lian-fu, TONG Xiao-lan, YANG Li. Study on the Upheaval of the Bogeda Mountain Block from Angle of Oil and Gas Exploration[J]. J4, 2005, 35(03): 346 -0350 .
[10] ZHANG Guang-xin, DENG Wei, HE Yan, RAMSIS Salama. An Application of Hydrological Response Units in Assessment of Soil Salinization Risks[J]. J4, 2005, 35(03): 356 -0360 .
Copyright © Journal of Jilin University(Earth Science Edition), All Rights Reserved.
Tel: +86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
Powered by Beijing Magtech Co. Ltd