Fault modeling of the 2012 Wutai, Taiwan earthquake and its tectonic implications
详细信息    查看全文
文摘

NW–SE trending seismogenic faults exist in a NW–SE compressional stress regime.

The low friction is inferred from the stress drop of the Wutai mainshock.

A rheology model is proposed using the transition of fault type and friction.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700