地震面波资料处理的基本方法

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英文篇名：Basic Method for Seismic Surface Wave Data Process 中文刊名：黑龙江水利科技 英文刊名：Heilongjiang Science and Technology of Water Conservancy 作者：代虎 英文作者：DAI Hu ; Guizhou Province Water Conservancy & Hydroelectric Power Investigation ; Design and Research Institute 中文关键词：地震勘探 ; 瑞雷面波 ; 基本原理 ; 瞬态 ; 稳态 ; 频散点 英文关键词：seismic exploration ; Rayleigh surface wave ; basic principle ; transient state ; static state ; dispersion point 出版日期：2013-09-30 机构：贵州省水利水电勘测设计研究院; 年：2013 期：09 出版单位：黑龙江水利科技

摘要

面波勘探是近几年发展起来的一种新的浅层地震勘探方法,具有简便、快捷、效率高等优点。该方法已在许多领域得到应用,并且取得良好效果。在天然地震面波中,瑞雷波是一种具有危害性较大的地震波;在人工地震勘探中,面波也是一种干扰波。但在工程勘探中,将面波视为有效波,并且在层状介质中,面波具有频散的特性,由此特性将面波应用在工程勘探中。近年来,面波勘探理论日趋成熟,应用范围越来越广,更多的人开始在工程勘察中使用面波。介绍了地震面波的发展历史、利用面波进行浅层地质勘探的基本原理及资料处理方法。
Surface wave is a new shallow seismic exploration method developed in recent years,characterizing by simplicity,convenience,high efficiency. The method is widely applied in different fields and achieves good results. In the natural seismic surface wave,Rayleigh wave is a seismic wave which has a more harmful effect. In artificial seismic exploration surface wave is a kind of interference wave. But surface wave is viewed as effective wave in engineering investigation,it has characteristic of dispersion points in the layered medium and the character is used in engineering investigation. In recent years surface wave exploration theory becomes more mature and application scope is widened greatly. Many engineers use it in engineering investigation. The development history of seismic surface wave,basic principle and data process method are introduced in the paper.

引文

[1]杨成林.瑞雷面波勘探[M].北京:地质出版社,1993.
    [2]张胜也,潘玉玲.应用地球物理学原理[M].北京:中国地质大学出版社,2000.
    [3]王振东.浅层地震勘探应用[M].北京:地质出版社,1988.