北京西郊玉泉山地区岩溶水强径流路径地球物理分析
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摘要
为研究北京西郊玉泉山地区岩溶水径流路径,需查明区内地层结构和断裂构造发育情况,故在玉泉山周边地区开展了综合地球物理勘查工作。完成1∶25000面积性重力测量3670点,在重力数据解释推断成果基础上,有针对性地布设可控源音频大地电磁测深(CSAMT)剖面测量5.1 km及微动测深点4个。综合研究了基岩起伏形态和构造展布特征,新解释推断了10条可能存在的断裂构造。结合区域水文地质资料,对主要断裂的水文地质意义进行了分析,形成了玉泉山地区岩溶水强径流路径新的认识,部分成果与最新的同位素水化学研究成果一致。本研究为玉泉山泉恢复确定合理的回灌方案提供了地球物理依据。
In order to investigate the features of strata configuration and fault structure and study the karst water flow path in Yuquanshan area of western Beijing, the authors carried out integrated geophysical survey in the surrounding area of Yuquanshan and completed regional gravity survey 107 km~2 in area with 3670 measurement points. On the basis of the explanation of gravity anomaly, 5.1 km controlled source audio-frequency magnetotellurics(CSAMT) profiles and 4 microtremor measurement points were carried out. According to these geophysical data, the basement relief and structure distribution were comprehensively studied,and 10 possible faults were interpreted and deduced. Combined with regional hydrogeological data, the hydrogeological significance of the main faults was studied. Then a new understanding of the strong karst water flow path in Yuquanshan area was obtained,which is consistent with the result of the latest isotope and hydrochemistry studies. This study provides the geophysical support for determining a reasonable recharge program for the restoration of Yuquanshan spring.
In order to investigate the features of strata configuration and fault structure and study the karst water flow path in Yuquanshan area of western Beijing, the authors carried out integrated geophysical survey in the surrounding area of Yuquanshan and completed regional gravity survey 107 km~2 in area with 3670 measurement points. On the basis of the explanation of gravity anomaly, 5.1 km controlled source audio-frequency magnetotellurics(CSAMT) profiles and 4 microtremor measurement points were carried out. According to these geophysical data, the basement relief and structure distribution were comprehensively studied,and 10 possible faults were interpreted and deduced. Combined with regional hydrogeological data, the hydrogeological significance of the main faults was studied. Then a new understanding of the strong karst water flow path in Yuquanshan area was obtained,which is consistent with the result of the latest isotope and hydrochemistry studies. This study provides the geophysical support for determining a reasonable recharge program for the restoration of Yuquanshan spring.
引文
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Cao Chuanghua,Liu Jianxin,Tong Xiaozhong,Xiewei,Tong Gangtie,Gao Dawei.2013.Discussion and application of CSAMT method with progressively inversion technology[J].The Chinese Journal of Nonferrous Metals,23(9):2340-2350(in Chinese with English abstract).
Cai Yuemei,Wang Wenxiang,Zhang Mingjiang,Yin Xiulan,Cai Wutian,Wang Ruijiu,Li Wenpeng.2016.An analysis of the groundwater flow system based on environmental isotopes in Turpan basin[J].Geology in China,43(4):1439-1445(in Chinese with English abstract).
Dong Jian,Chen Lei,Zhang Guili.2018.Characteristics of geophysical fields around gold deposits in the Xiadian region,Shandong Province[J].Geology and Exploration,54(1):138-147(in Chinese with English abstract).
Feng Juan,Meng Xiaohong,Chen Zhaoxi,Zhang Sheng.2014.Review of the gravity density interface inversion[J].Progress in Geophysics,29(1):223-228(in Chinese with English abstract).
Liang Yongping,Zhao Chunhong,Tang Chunlei,Wang Weitai,Shen Haoyong.2015.Progress of hydrogeology and environmental geology survey in karst area of northern China:An example from western hills of Beijing[J].Geological Survey of China,29(1):223-228(in Chinese with English abstract).
Li Jinghe,He Zhanxiang,Xiong Bin.2018.Fast 2D forward modeling and inversion of CSEM with topography in the frequency domain[J].Geology and Exploration,54(2):325-331(in Chinese with English abstract).
Ma Zhiyuan,Niu Guangliang,Liu Fang,Hou Guangcai,Dang Xueya,Su Yan.2006.Isotope evidence of strong runoff zones of karst groundwater in eastern Weibei,Shaanxi,China,and its renewability evaluation[J].Geological Bulletin of China,25(6):756-761(in Chinese with English abstract).
Qin D J,Zhao Z F,Guo Y,Liu W C.2017.Using hydrochemical,stable isotope,and river water recharge data to identify groundwater flow paths in a deeply buried karst system[J].Hydrological Processes,31:4297-4314.
Qin Dajun,Sun Jie,Guo Yi,Li Lu,Mohammed Haji,Wang Dongdong,Liu Wencai.2019.Impacts of yongding river on the Xishan karst aquifer and Yuquan spring in Beijing,China[J].Journal of Engineering Geology,25(6):756-761(in Chinese with English abstract).
Ran Weiyan,Wang Zhendong.1994.Then long-wave microtremors method and its advances[J].Geophysical and Geochemical Exploration,18(1):28-34(in Chinese with English abstract).
Satoh T,Kawase H,Matsushima S.2001.Estimation of S-Wave velocity structures in and around the Sendai Basin,Japan,using array records of microtremors[J].Bulletin of the Seismological Society of America,91(2):206-218.
Sun Linhua,Gui Herong,Chen Song.2009.Use of geochemical inversion to study deep groundwater pattern in northern Anhui mining areas[J].Coal Geology of China,21(1):35-38(in Chinese with English abstract).
Sun Houyun,Mao Qigui,Wei Xiaofeng,Zhang Huiqiong,Xi Yeze.2018.Hydrogeochemical characteristics and formation evolutionary mechanism of the groundwater system in the Hami basin[J].Geology in China,45(6):1128-1141(in Chinese with English abstract).
Tan Handong,Jiang Mei,Lin Changhong,Peng Miao,Wu Liangshi,Ma Huan,Wang Zhongkai,Li Jinjin,Tan Jiayan.2013.Characteristics of electrical structure of Tengchong volcanotectonic belt in Yunnan province[J].Geology in China,40(3):800-805(in Chinese with English abstract).
Tang Jingtian,Zhou Cong,Deng Xiaohong.2010.Identification and discrimination of the horizontal layered earth by usiong CSAMTapparent resistivity curves[J].Geology and Exploration,46(6):1079-1086(in Chinese with English abstract).
Tang Chunlei,Liang Yongping,Ji Tiequn,Wang Weitai,Zhao Chunhong,Shen Haoyong.2015.Hydrogeological significance of the Jiulongshan-Xiangyu syncline at Yuquanshan spring[J].Carsologica Sinica,34(5):431-437(in Chinese with English abstract).
Wang Qiang,Mou Huirong,Liu Taifu.1998.A primary study on the genesis and features of karst from Ordovician system in the Xishan hill of Beijing[J].Beijing Geology,(3):1-9(in Chinese with English abstract).
Wang Ruo,Wang Miaoyue.2003.Inversion method of controlled source audio-frequency magnetotelluric data[J].Progress in Geophysics,18(2):197-202(in Chinese with English abstract).
Wu Qianqian,Ren Jiaguo,Xu Mo.2008.Isotope features and supply sources of groundwater in the Yarkant river drainage area,Xinjiang[J].Geology in China,35(2):331-336(in Chinese with English abstract).
Wang Xiaohong,Liu Wencheng,Shen Yuanyuan,Liu Shicheng.2011.Analysis on the hydrogeology characteristics and exploitation potential of the emergency karst water source field in Xishan region,Beijing[J].Carsologica Sinica,30(2):216-221(in Chinese with English abstract).
Wang Lijiao,Zhang Youquan,Gong Huili,Yang Guoqing,Liu Jiurong,Sun Ying.2016.A study on recovery condition of Yuquanshan spring in Beijing[J].Hydrogeology and Engineering Geology,43(3):22-28(in Chinese with English abstract).
Wu Luping,Shi Kunfa,Li Yinhuai,Li Songhao.1996.Application of CSAMT to the search for groundwater[J].Acta Geophysica Sinica,43(3):22-28(in Chinese with English abstract).
Wu Le,Zhang Youquan,Gong Huili,Ye Chao,Shen Yuanyuan,Wang Rong.2016.Numerical simulation of groundwater flow for Xishan area in Beijing[J].Hydrogeology and Engineering Geology,43(3):29-36(in Chinese with English abstract).
Xu Guanghui,Huang Lijun,Liu Ruide.2005.The application of controllable source audio frequency magetotelluric sounding to hydrogeological exploration in Beijing[J].Geophsical and Geochemical Exploration,43(3):29-36(in Chinese with English abstract).
Xu Peifen,Li Chuanjin,Ling Suqun,Zhang Yinbin,Hou Chao,Sun Yongjun.2009.Mapping collapsed colums in coal mines utilizing Microtremor survey methods[J].Chinese Journal of Geophysics,52(7):29-36(in Chinese with English abstract).
Yang Ping,Hou Jingyan,Gao Ruihua.1984.The supply source of Yuquanshan spring-runoff characteristics of Ordovician karst water in front of Xishan region,Beijing[J].Hydrogeology and Engineering Geology,2(6):15-19(in Chinese).
Yan Jiayong,Lv Qingtian,Chen Mingchun,Deng Zhen,Qi Guang,Zhang Kun,Liu Zhendong,Liu Yan.2015.Identification and extraction of geological structure information based on multi-acale edgy detection of gravity and magnetic fields:An example of the Tongling ore concentration area[J].Chinese Journal of Geophysics,58(12):4450-4464(in Chinese with English abstract).
Zhu Liming,Wang Shuiqiang,Lei Wenmin.2012.Boundary detection of magnetic field source based on Canny theory[J].Chinese Journal of Engineering Geophysics,9(1):44-48(in Chinese with English abstract).
Zhang Baolong,Li Zhiwei,Bao Feng,Deng Yang,You Qingyu,Zhang Senqi.2016.Shallow shear-wave velocity structures under the Weishan volcanic cone in Wudalianchi volcano field by microtremor survey[J].Chinese Journal of Geophysics,59(10):3662-3673(in Chinese with English abstract).
Zhao Chunhong,Liang Yongping,Wang Weitai,Tang Chunlei,Shen Haoyong.2017.Discussion on the characteristics of karst water systems in the Xishan area of Beijing[J].Carsologica Sinica,36(5):641-647(in Chinese with English abstract).
程东兴,李延清,徐忠平,张泽红.2011.重力资料数据处理及解释概论[J].西部探矿工程,23(12):144-146.
曹创华,柳建新,童孝忠,谢维,佟钢铁,高大维.2013.CSAMT逐级反演技术的讨论及应用[J].中国有色金属学报,23(9):2340-2350.
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