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物探与化探  2020, Vol. 44 Issue (4): 727-733    DOI: 10.11720/wtyht.2020.1413
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
多种非震方法在山东齐河地热勘查中的应用
章惠1,2(), 隋少强1(), 钱烙然3, 汪新伟1
1.中石化新星石油公司新能源研究院,北京 100083
2.中石化石油物探技术研究院,江苏 南京 211103
3.中石化石油勘探开发研究院,北京 100083
The application of multiple non-seismic methods to geothermal exploration in Qihe, Shandong Province
Hui ZHANG1,2(), Shao-Qiang SUI1(), Luo-Ran QIAN3, Xin-Wei WANG1
1. New Energy Research Institute,Sinopec Star Petroleum Co. Ltd.,Beijing 100083,China
2. Sinopec Geophysical Research Institute,Nanjing 211103,China
3. Sinopec Petroleum Exploration and Development Research Institute,Beijing 100083,China
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摘要 

非震地球物理勘探方法是目前地热勘查的有效手段。本文以山东齐河荣盛温泉小镇为例,针对该区断裂较为发育,地层横向变化大,地质条件复杂的难点问题,综合考虑地层电性和地层速度差异特征,采取“两步走”方式进行地热勘查。第一步利用电磁方法查明研究区断裂构造位置和热储埋深,初步圈定有利的富水区域;第二步通过地微动方法验证断裂和地层的展布特征,缩小目标靶区,为地热井布设提供充实的依据。经钻井表明,多种非震方法相结合具有较好的应用效果,为今后复杂地质条件的地热勘探提供了有利的参考价值和重要的借鉴意义。

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章惠
隋少强
钱烙然
汪新伟
关键词 可控源大地电磁方法地微动探测方法地热勘查山东齐河    
Abstract

Non-seismic methods have been proved to be effective in geothermal exploration.This paper describes a two-step method for investigating the geothermal potential in Fountain Village,Rongsheng,Qihe,Shandong Province.The geological background of the target area is very complicated;for instance,many complex faults are developed and the formations usually have strong horizontal anisotropic property,which enhances the difficulty of exploration.The two-step method put forward by the authors utilizes the electrical and elastic features in different formations to solve these difficulties.The first step is to investigate the location of huge fault structure and the depth of resources by using electromagnetic method,which can locate the water-rich regions.The second step focuses on the more precise features of faults based on microtremors method. This method can help locate the sweet spot area more accurately and bring constructive suggestions to well location determination.Drilling results have testified the feasibility and applicability of this two-step method,which opens up a new path in complex geothermal exploration.

Key wordsCSAMT    microtremors survey    geothermal exploration    Qihe in Shandong Province
收稿日期: 2019-09-02      出版日期: 2020-08-28
:  P631.4  
基金资助:中石化科技部项目“渤海湾盆地重点地区地热资源评价与开发技术政策”(JP19002-1)
通讯作者: 隋少强
作者简介: 章惠(1987-),女,工程师,硕士,主要从事地热地球物理勘探工作。Email:zhanghui714@126.com
引用本文:   
章惠, 隋少强, 钱烙然, 汪新伟. 多种非震方法在山东齐河地热勘查中的应用[J]. 物探与化探, 2020, 44(4): 727-733.
Hui ZHANG, Shao-Qiang SUI, Luo-Ran QIAN, Xin-Wei WANG. The application of multiple non-seismic methods to geothermal exploration in Qihe, Shandong Province. Geophysical and Geochemical Exploration, 2020, 44(4): 727-733.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2020.1413      或      https://www.wutanyuhuatan.com/CN/Y2020/V44/I4/727
Fig.1  齐河地区构造地质简图
地层 主要岩性 电阻率/(Ω·m) 横波速度/(m·s-1)
第四系—新近系 黏土、泥岩、粉砂岩、中细砂岩 0~60(低阻) 0~1600(低速)
侏罗系—二叠系—石炭系 砂泥岩、页岩夹煤层、薄层灰岩 60~200(中阻) 1600~2000(中速)
奥陶系—寒武系 灰岩 200以上(高阻) 2000以上(高速)
Table 1  研究区地层物性参数
Fig.2  CSAMT方法L11线(左)、L20线(右)反演电阻率剖面及解释图
Fig.3  垂直电测深电阻率等值线断面图及解释图
Fig.4  CSAMT方法反演电阻率切片图及解释图
Fig.5  微动探测DWD1线反演横波速度剖面及解释图
Fig.6  研究区综合物探解释成果平面图
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