吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 273-284.doi: 10.13278/j.cnki.jjuese.20190019
• 地球探测与信息技术 • 上一篇
林松1,2, 王薇1,2, 邓小虎2, 查雁鸿2, 周红伟2, 程邈1,2
Lin Song1,2, Wang Wei1,2, Deng Xiaohu2, Zha Yanhong2, Zhou Hongwei2, Cheng Miao1,2
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。
中图分类号:
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