First time that left-lateral shear is clearly documented inside the Gulf of Evia rift.
Aftershock depths indicate a seismogenic (brittle) zone of about 15 km in depth for the Gulf of Evia rift.
The left-lateral kinematics indicates crustal strain partitioning because of E-W horizontal compression.
© 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 |