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应用地球物理  2025, Vol. 22 Issue (1): 99-109    DOI: 10.1007/s11770-023-1026-y
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低阻覆盖区深层地热探测方法及应用实例
乔勇,张慧*
1. 长江大学 地球科学学院,武汉 430100;2. 华北水利水电大学 地球科学与工程学院,郑州 450000;3. 水利水电规划设计总院,北京 100120
SMethodology and Application of Deep Geothermal Sounding in Low-Resistance Cover Areas
Qiao Yong, and Zhang Hui*
1. College of Geosciences, Yangtze University, Wuhan, 430100, China 2. College of Geosciences and Engineering, North China University of Water Resources and Electric Power, Zhengzhou 450000, China 3. China Renewable Energy Engineering Institute, Beijing,100120, China
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摘要 本文以齐河地区为例,针对深层岩溶地热探测面临的城区施工、热储埋藏深、上覆巨厚“低阻屏蔽”层等问题,综合对比多种地球物理测深方法后,在研究区实施了可控源音频大地电磁法对深部地层结构进行探测。根据可控源音频大地电磁法的电阻率剖面,推测出3条断裂并圈定了区内1个低阻异常区。通过钻探验证,剖面解释成果与钻探揭露的地层界线吻合较好,低阻异常区与钻探结果基本吻合,证明了可控源音频大地电磁方法对低阻覆盖区下的深层地热勘探的有效性,可为类似地区的深部地热探测提供技术支持。
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关键词可控源音频大地电磁法   低阻屏蔽   奥陶系岩溶热储   断裂破碎带   全区视电阻率     
Abstract: Taking the Qihe area as an example, this paper compared various geophysical exploration methods in view of the problems of urban construction, deep thermal reservoir burial, and vast overlying low-resistance shield layer in deep karst geothermal exploration. A Controlled-source audio magnetotelluric (CSAMT) method was taken to overcome the problems and detect deep stratigraphic structures in the study area. The acquisition parameters of CSAMT were optimized to take into account the exploration depth and signal-to-noise ratio. The distortion of data in the near and transition zone was eliminated by the inversion of equivalent whole-region apparent resistivity, so as to achieve the purpose of deep sounding. Based on the resistivity profile resulting from the proposed CSAMT method, three faults were inferred and one low-resistance anomaly zone in the area was traced. The results of the profile interpretation were verified by drilling. The inferred stratigraphic boundaries and low-resistance anomaly zone were basically in agreement with the drilling results, thereby proving the effectiveness of the CSAMT method for deep geothermal exploration in low-resistance coverage areas. This method could provide technical support for deep geothermal exploration in similar areas.
Key wordsCSAMT    low-resistivity shielding    Ordovician karst geothermal reservoir    fracture zone    whole region apparent resistivity   
收稿日期: 2022-08-31;
基金资助:This research is supported by the National Natural Science Foundation of China (No 52174048).
通讯作者: 张慧 (Email: zhanghui@ncwu.edu.cn).     E-mail: zhanghui@ncwu.edu.cn
作者简介: Qiao Yong (1986 -), since 2019 he has been studying for his Ph.D. at College of Geosciences, Yangtze University, Wuhan. His main research direction is geothermal exploration and development, geothermal policy research. E-mail: 89561564@qq.com.
引用本文:   
. 低阻覆盖区深层地热探测方法及应用实例[J]. 应用地球物理, 2025, 22(1): 99-109.
. SMethodology and Application of Deep Geothermal Sounding in Low-Resistance Cover Areas[J]. APPLIED GEOPHYSICS, 2025, 22(1): 99-109.
 
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[5] 乔勇,张慧*. 低阻覆盖区深层地热探测方法及应用实例[J]. 应用地球物理, 0, (): 99-109.
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