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Application research of high density resistivity method to karst geological exploration in mining area

机译:高密度电阻率法在矿区岩溶地质勘查中的应用研究

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The karst collapse is a common karst geological hazard,which greatly endangers local people's life and property safety.Hazard geological survey provides necessary basic geological data for hazard treatment in karst area,and it is also the precondition of preventing and decreasing hazard work.As a new geological prospecting method,the high density resistivity method can be applied in geological hazard survey and engineering survey extensively.It is an effective method of karst survey,which can reflect the section electrical change caused by karst development and the basic form of karst electrical abnormal body.The status of karst development,the main geological structure and fault structure of Rucheng tungsten mine area are studied by using high density resistivity method in this paper.They have got a good geological effect,and preliminary studied the cause of karst geological hazard occurred in mining area.The result provides a solid geophysical basis for the further comprehensive treatment in this area.
机译:岩溶塌陷是一种常见的岩溶地质灾害,极大地危害了当地人民的生命和财产安全。灾害地质调查为岩溶地区的灾害治理提供了必要的基础地质资料,也是预防和减少灾害工作的前提。高密度电阻率法是一种新型的地质勘探方法,可广泛应用于地质灾害调查和工程勘察中。它是一种有效的岩溶勘查方法,可反映因岩溶发育引起的断层电气变化和岩溶异常电气的基本形式。本文采用高密度电阻率法研究了汝城钨矿区的岩溶发育状况,主要地质构造和断层构造,取得了良好的地质效果,并初步研究了岩溶发生地质灾害的成因。结果为进一步综合处理提供了坚实的地球物理基础在这方面。

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