Transient fault slip in Guerrero, southern Mexico

被引：157

作者：

Lowry, AR ^{[1
]}

Larson, KM

Kostoglodov, V

Bilham, R

机构：

[1] Univ Colorado, Dept Phys, Boulder, CO 80309 USA

[2] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA

[3] Univ Colorado, Dept Aerosp Engn, Boulder, CO 80309 USA

[4] Natl Autonomous Univ Mexico, Inst Geofis, Mexico City 04510, DF, Mexico

来源：

GEOPHYSICAL RESEARCH LETTERS | 2001年 / 28卷 / 19期

关键词：

D O I：

10.1029/2001GL013238

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Guerrero region of southern Mexico has accumulated more than 5 m of relative plate motion since the last major earthquake. In early 1998, a continuous CPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along-strike of the subduction megathrust. Campaign GPS and leveling data corroborate the model. The moment release was equivalent to an M(w)greater than or equal to6.5 earthquake. No M >5 earthquakes accompanied the event, indicating the frictional regime is velocity-strengthening at the location of slip.

引用

页码：3753 / 3756

页数：4

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