A review of the current understanding of seismic shear-wave splitting in the Earth's crust and common fallacies in interpretation

被引:204
作者
Crampin, Stuart [1 ,2 ,3 ]
Peacock, Sheila [4 ]
机构
[1] Univ Edinburgh, Sch Geosci, Edinburgh EH9 3JW, Midlothian, Scotland
[2] British Geol Survey, Edinburgh Anisotropy Project, Edinburgh EH9 3LA, Midlothian, Scotland
[3] China Earthquake Adm, Inst Earthquake Sci, Beijing 100036, Peoples R China
[4] AWE Blacknest, Reading RG7 4RS, Berks, England
基金
英国自然环境研究理事会;
关键词
fallacies in interpretation; new geophysics; new understanding of fluid/rock deformation; shear-wave splitting;
D O I
10.1016/j.wavemoti.2008.01.003
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
Azimuthally-aligned shear-wave splitting is widely observed in the Earth's crust. The splitting is diagnostic of some form of seismic anisotropy, although the cause of this anisotropy has been sometimes disputed. The evidence in this review unquestionably indicates cracks, specifically stress-aligned fluid-saturated microcracks, as the predominant cause of the azimuthally-aligned shear-wave splitting in the crust. Although, in principle, shear-wave splitting is simple in concept and easy to interpret in terms of systems of anisotropic symmetry, in practice there are subtle differences from isotropic propagation that make it easy to make errors in interpretation. Unless authors are aware of these differences, misinterpretations are likely which has led to incorrect conclusions and charges of controversy where only misinterpretations exist. As a consequence, stress-aligned fluid-saturated microcracks as the cause of azimuthally-aligned shear-wave splitting in the crust is still not universally accepted despite there being distinguishing features that directly indicate crack-induced anisotropy. This paper reviews observations and interpretations of crack-induced shear-wave splitting and demonstrates that claims for aligned crystals and other sources of shear-wave splitting are due to fallacies in interpretation. This review shows how previous contrary interpretations are resolved and discusses common fallacies and misinterpretations. It is suggested that this new interpretation of shear-wave splitting has such fundamental implications for almost all solid-earth geoscience that it amounts to a New Geophysics with applications to particularly exploration and earthquake geoscience but also to almost to all other branches of solid Earth geoscience. Crown copyright (C) 2008 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:675 / 722
页数:48
相关论文
共 142 条
[1]  
ALEXANDROV KS, 1961, B ACAD SCI USSR GEOP, V12, P871
[2]  
Alford R. M., 1986, 56 ANN INT M SOC EXP, P379
[3]   S-WAVE ANISOTROPY IN THE UPPER MANTLE UNDER A VOLCANIC AREA IN JAPAN [J].
ANDO, M ;
ISHIKAWA, Y ;
WADA, H .
NATURE, 1980, 286 (5768) :43-46
[4]   Processing, modelling and predicting time-lapse effects of overpressured fluid-injection in a fractured reservoir [J].
Angerer, E ;
Crampin, S ;
Li, XY ;
Davis, TL .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2002, 149 (02) :267-280
[5]  
[Anonymous], [No title captured]
[6]  
ASTER RC, 1991, B SEISMOL SOC AM, V81, P1057
[7]   QUANTITATIVE MEASUREMENTS OF SHEAR-WAVE POLARIZATIONS AT THE ANZA SEISMIC NETWORK, SOUTHERN CALIFORNIA - IMPLICATIONS FOR SHEAR-WAVE SPLITTING AND EARTHQUAKE PREDICTION [J].
ASTER, RC ;
SHEARER, PM ;
BERGER, J .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B8) :12449-12473
[8]   COMMENT ON QUANTITATIVE MEASUREMENTS OF SHEAR-WAVE POLARIZATIONS AT THE ANZA SEISMIC NETWORK, SOUTHERN CALIFORNIA - IMPLICATIONS FOR SHEAR-WAVE SPLITTING AND EARTHQUAKE PREDICTION BY ASTER,RICHARD,C., SHEARER,PETER,M., BERGER,JON - REPLY [J].
ASTER, RC ;
SHEARER, PM ;
BERGER, J .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B4) :6415-6419
[9]   INITIAL SHEAR-WAVE PARTICLE MOTIONS AND STRESS CONSTRAINTS AT THE ANZA SEISMIC NETWORK [J].
ASTER, RC ;
SHEARER, PM .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1992, 108 (03) :740-748
[10]   Anisotropic structure under a back arc spreading region, the Taupo Volcanic Zone, New Zealand [J].
Audoine, E ;
Savage, MK ;
Gledhill, K .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2004, 109 (B11) :1-21