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应用地球物理  2025, Vol. 22 Issue (4): 1369-1379    DOI: 10.1007/s11770-024-1106-7
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大地电磁法揭示沂沭断裂带中深层电性结构和热学特征
杜文龙,周兴宇*,孙远彬,王士党,张大彬,王琛,张金伟,丁仁伟
1. 山东省煤田地质局第三勘探队,泰安,271000;2. 山东科技大学地球科学与工程学院,青岛, 266590
Three-dimensional geothermal reservoir model using the magnetotelluric method in medium and deep strata of Yishu fault zone, Rizhao Section
Du Wen-long, Zhou Xing-yu,*, Sun Yuan-bin, Wang Shi-dang, Zhang Dabin, Wang Chen, Zhang Jin-wei, Ding Ren-wei
1. The Third Exploration Team, Shandong Bureau of Coal Geology, Taian, 271000 2. College of Earth Science and Technology, Shandong University of Science and Technology, Qingdao, 266590
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摘要 沂沭断裂带具有良好的中高温地热储藏条件,但地热赋存模式和热储模型目前仍不清楚。鉴于深部热源和热通道对揭示中高温地热系统形成机制的重要性,本文在沂沭断裂带日照段开展大地电磁测量,获得了10条测线、119个可用测点。通过二维和三维非线性共轭梯度反演,获得了研究区深部电性结构,首次构建了研究区三维地热储层模型。研究结果表明,沂沭断裂带深部低阻异常体通过电阻率稍高的通道向上运移,在浅部形成相对低阻层和低阻层,分别对应于热源、导热通道、热储层和盖层。断裂构造主要控制区域地热异常,影响大气降水、地表水入渗和地下热水的上升通道。研究结果对研究沂沭断裂带中深部地热资源形成机制和分布规律具有一定的指导意义,为该区地热资源的勘探和评价提供了一定的参考价值。
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关键词沂沭断裂带   大地电磁测深   地热模型   热通道     
Abstract: The Yishu fault zone in Shandong Province, China, exhibits favorable conditions for medium- and high-temperature geothermal storage. However, its geothermal occurrence patterns and heat storage model remain unclear. Recognizing the importance of deep heat sources and heat channels in unraveling the formation mechanisms of medium- and high-temperature geothermal systems, we conducted a magnetotelluric survey along the Yishu fault zone, which contained 10 survey lines and 119 usable points. Using two-dimensional and three-dimensional nonlinear conjugate gradient inversion, the deep electrical structure was obtained, and the three-dimensional geothermal reservoir model in the study area was constructed for the first time. The results show that the deep low-resistance anomaly in the Yishu fault zone moves upward through the channel with slightly higher resistivity, forming a relatively low-resistance layer and a low-resistance layer in the shallow part, corresponding to the heat source, thermal conduction fault, heat reservoir, and overburden layer, respectively. The fault structure primarily controls regional geothermal anomalies, influencing atmospheric precipitation, surface water infiltration, and geothermal water migration pathways. The results of this study have a certain guiding signifi cance for the study of the formation mechanism and distribution law of geothermal resources in the middle and deep strata of the Yishu fault zone. Additionally, the results provide valuable insights for the exploration and assessment of geothermal resources in the area.
Key wordsYishu fault zone    magnetotelluric sounding    geothermal model    heat flow channel   
收稿日期: 2024-03-28;
基金资助:This work was supported by LUMEIDIKE202326
通讯作者: 周兴宇, zhouxingyu2006@126.com.     E-mail: zhouxingyu2006@126.com
作者简介: Zhou Xingyu, Senior engineer, graduated from China University of Geosciences (Wuhan) in Resource Exploration Engineering. He is currently a senior engineer in the Third Exploration Team of Shandong Coalfi eld Geological Bureau. His main interests are coal mine goaf exploration, geological disaster investigation and evaluation, geothermal investigation, and metal exploration.
引用本文:   
. 大地电磁法揭示沂沭断裂带中深层电性结构和热学特征[J]. 应用地球物理, 2025, 22(4): 1369-1379.
. Three-dimensional geothermal reservoir model using the magnetotelluric method in medium and deep strata of Yishu fault zone, Rizhao Section[J]. APPLIED GEOPHYSICS, 2025, 22(4): 1369-1379.
 
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