Focal mechanisms and seismotectonic stress in North Central Taiwan in relation with the Chi-Chi earthquake

被引:3
|
作者
Mozziconacci, Laetitia [1 ,2 ]
Angelier, Jacques [1 ,2 ]
Delouis, Bertrand [1 ,2 ]
Rau, Ruey-Juin [3 ]
Bethoux, Nicole [1 ,2 ]
Huang, Bor-Shouh [4 ]
机构
[1] Observ Oceanol Villefranche, F-06235 Villefranche Sur Mer, France
[2] Univ Nice Sophia Antipolis, CNRS, F-06560 Valbonne, France
[3] Natl Cheng Kung Univ, Dept Earth Sci, Tainan 70101, Taiwan
[4] Acad Sinica, Inst Earth Sci, Taipei 115, Taiwan
关键词
Seismotectonics; Focal mechanisms; Stress tensor; North Central Taiwan; LONGITUDINAL VALLEY; TENSOR INVERSION; FAULT PLANE; SEQUENCE; BELT; IDENTIFICATION; RELOCATION; CHIHSHANG; EVOLUTION; COLLISION;
D O I
10.1016/j.tecto.2007.11.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The aftershock sequence of the 1999 Chi-Chi earthquake (M-w=7.6) provided a large number of focal mechanisms recorded with BATS Centroide Moment Tensors (CMT) which allowed us to perform reliable stress tensor inversions in North Central Taiwan. These inversions were done for three time-periods corresponding to the post-seismic phase of the 1999 Chi-Chi earthquake (M-w 7.6). In the last period the 2003 Chengkung earthquake (M-w=6.5) occurred on the vicinity of our study area and its influence is also examined. For comparison between seismotectonic regimes of the pre- and post- Chi-Chi periods, we also carried out stress inversion using published focal mech of the pre Chi-Chi period. For each period, we delineated seismogenic domains with relatively homogeneous stress regimes in agreement with the local structures. The boundaries of these domains vary during the whole post Chi-Chi period as seismic activity decays. A 25 degrees clockwise rotation of the main compressive stress sigma(1) is observed between the pre and the post Chi-Chi periods in the domain located near the northern termination of the Chi-Chi rupture. A stress perturbation related to the Chengkung earthquake could be detected in the eastern part of the Central Range. We present an interpretation of the determined stress regimes in terms of changes in mechanical behaviour of the Sanyi-Puli transfer zone. (c) 2007 Elsevier B.V. All rights reserved.
引用
收藏
页码:409 / 426
页数:18
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