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尾波干涉原理及其应用研究进展综述

肖卓 高原

地震学报Issue(3):516-526,11.
地震学报Issue(3):516-526,11.DOI:10.11939/jass.2015.03.014

尾波干涉原理及其应用研究进展综述

A review on the theory of coda wave interferometry and its research progress

肖卓 1高原1

作者信息

  • 1. 中国北京 100036 中国地震局地震预测研究所
  • 折叠

摘要

Abstract

This review first presents the basic theory of coda wave interferome-try (CWI),and then introduces the application and research progress of CWI in source location variation and scatter moving status.Finally the advantages and the disadvantages as well as development direction of the CWI in monitoring velocity variation of underground media are discussed by using repeating earth-quakes,active sources and ambient noise cross-correlation function.Due to the characteristics of multiple scattering waves,CWI can be used to extract source locations and monitor subtle variations of media.The temporal change of media may provide us ideas and guidances of preparation and development of earth-quakes or volcanoes.

关键词

尾波干涉/震源相对位置/散射体运移/波速变化

Key words

coda wave interferometry/relative source location/scatter moving/velocity variation

分类

天文与地球科学

引用本文复制引用

肖卓,高原..尾波干涉原理及其应用研究进展综述[J].地震学报,2015,(3):516-526,11.

基金项目

国家自然科学基金重点项目(41230210)和中国地震局中日韩国际合作专项(ZRH2013-03,ZRH2014-05)联合资助. ()

地震学报

OA北大核心CSCDCSTPCD

0253-3782

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