用户名: 密码: 验证码:
Geodynamic background of the 2008 Wenchuan earthquake based on 3D visco-elastic numerical modelling
详细信息    查看全文
文摘

Stress concentration in the fault zone is responsible for the Wenchuan earthquake.

Stress concentration is controlled by the crust rheological structure.

Large horizontal viscosity variation accelerates the stress concentration.

Fast moving lower crustal flow accelerates the stress concentration.

The along-strike stress distribution explains the fault motion during the earthquake.

© 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