A study of flow path in Yuquanshan area of western Beijing based on integrated geophysical technology
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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。
Abstract: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 km2 in area with 3670 measurement points. On the basis of the explanation of gravity anomaly, 5.1km 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.
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Key words:
- gravity anomaly /
- microtremor survey /
- flow path /
- Yuquanshan /
- integrated geophysics
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图 3 AA'剖面综合分析图(平面位置见图 2a)
Figure 3.
图 4 BB'剖面综合分析图(平面位置见图 2a)
Figure 4.
表 1 研究区地层物性特征统计
Table 1. Statistics of petrophysical properties of strata in the study area
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