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高原冻土区三分量地震探测方法试验

刘建勋 徐明才 王小江 张保卫

物探与化探Issue(2):327-333,7.
物探与化探Issue(2):327-333,7.DOI:10.11720/wtyht.2015.2.19

高原冻土区三分量地震探测方法试验

A study of three-component seismic exploration in plateau permafrost region

刘建勋 1徐明才 1王小江 1张保卫1

作者信息

  • 1. 中国地质科学院 地球物理地球化学勘查研究所,河北 廊坊 065000
  • 折叠

摘要

Abstract

Three⁃component seismic exploration is an effective method for the utilization of P⁃wave and converted⁃wave to detect fine structures.With this method,converted⁃wave imaging profiles have high resolution,and small geological structures such as small faults and small structures can be identified.In this paper,based on the application experiments of three⁃component seismic exploration tech⁃nology in Qiangtang basin of Tibet,the authors investigated the three⁃component seismic data acquisition method,converted⁃wave data processing technology and comparative interpretation method,and the results achieved prove the effectiveness of this method.This paper has certain reference value for the application and study of multi⁃component seismic exploration technology in plateau permafrost area in the future.

关键词

高原冻土区/三分量地震勘探/转换波/数据采集/处理解释

Key words

plateau permafrost region/three-component seismic exploration/converted-wave/data acquisition/processing and interpre-tation

分类

天文与地球科学

引用本文复制引用

刘建勋,徐明才,王小江,张保卫..高原冻土区三分量地震探测方法试验[J].物探与化探,2015,(2):327-333,7.

基金项目

公益性行业科研专项经费项目(201111019);中国地质调查局天然气水合物勘查与试采专项项目 ()

物探与化探

OACSCDCSTPCD

1000-8918

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