| 三峡库区典型滑坡地质与地球物理电性特征 |
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| 引用本文： | 林松,王薇,邓小虎,查雁鸿,周红伟,程邈.三峡库区典型滑坡地质与地球物理电性特征[J].吉林大学学报(地球科学版),2020,50(1):273-284. |
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| 作者姓名： | 林松 王薇 邓小虎 查雁鸿 周红伟 程邈 |
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| 作者单位： | 1. 中国地震局地震研究所, 地震预警湖北省重点实验室, 武汉 430071;2. 武汉地震工程研究院有限公司, 武汉 430071 |
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| 基金项目： | 国家自然科学基金项目（41572354） |
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| 摘 要： | 滑坡属于地质灾害中的重要灾种之一，查明滑坡区的地质与地球物理特征，对分析滑坡形成机制、评价滑坡稳定性具有重要意义。鉴于此，本文将高密度电法引入三峡库区腹地万州区滑坡地质调查中，在区内四方碑滑坡、塘角1号滑坡和麻柳林滑坡进行地球物理探测工作，并结合钻孔资料对实测结果进行对比验证。实测结果表明：在地形复杂地区开展地球物理探测工作，通过数据反演与分析，可获取滑坡体地层结构及滑移面；结合相关地质资料，通过对比解译，可弥补单纯依靠钻孔信息来确定滑移面形态的不足；3个典型滑坡区地球物理实测资料揭露滑坡体和滑床地球物理电性特征表现为，由崩坡积物、第四系粉质黏土以及含水碎石块组成的滑坡体电阻率低于40 Ω·m，而由砂岩与泥岩组成的滑床电阻率高于40 Ω·m，高密度电法对基岩滑坡和土质滑坡都能获取较好的结果。
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| 关 键 词： | 三峡库区 滑坡 地球物理特征 地质特征 滑床 |
| 收稿时间： | 2019-01-28 |
Geological and Geophysical Electric Characteristics of Typical Landslides in Three Gorges Reservoir |
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| Lin Song,Wang Wei,Deng Xiaohu,Zha Yanhong,Zhou Hongwei,Cheng Miao.Geological and Geophysical Electric Characteristics of Typical Landslides in Three Gorges Reservoir[J].Journal of Jilin Unviersity:Earth Science Edition,2020,50(1):273-284. |
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| Authors: | Lin Song Wang Wei Deng Xiaohu Zha Yanhong Zhou Hongwei Cheng Miao |
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| Institution: | 1. Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China;2. Wuhan Institute of Earthquake Engineering Co. Ltd., Wuhan 430071, China |
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| Abstract: | Landslide is one of the most important types of geological hazards. It is of great significance to find out the geological and geophysical characteristics of a landslide area for analyzing the formation mechanism of a landslide and evaluating its stability. In view of this, the high-density resistivity method was first introduced into the landslide geological survey of Wanzhou area in the hinterland of the Three Gorges Reservoir area, and the geophysical exploration of Sifangbei landslide, Tangjiao No. 1 landslide, and Maliulin landslide was carried out in the area. The measured results were compared and verified with borehole data. Through data inversion and analysis, the stratum structure and slip surface of landslide bodies are obtained; By combining with the relevant geological data and comparative interpretation, it can make up for the deficiency of only relying on borehole information to determine the shape of slip surface; According to the measured data of the three typical landslide areas, the geophysical and electrical characteristics of landslide mass and sliding bed are as follows, resistivity of landslide mass composed of colluvium, quaternary silty clay and water bearing gravel block is less than 40 Ω·m, while resistivity of sliding bed composed of sandstone and mudstone is more than 40 Ω·m. It is proved that the high-density electrical method can get better results for both bedrock landslide and soil landslide. |
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| Keywords: | Three Gorges Reservoir landslide geophysical characteristics geological characteristics slide bed |
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