The application of shallow seismic techniques in the study of active faults: The Atalanti normal fault, central Greece
详细信息查看全文 | 推荐本文 |
摘要
Shallow seismic surveys can constitute a useful tool in actively deforming regions by yielding precise information on the location of active faults, their geometry and cumulative displacement. Since the structures in these regions are rarely flat but always with sharp dips, 3D effects and side reflections can influence the results, thus the interpretation must be combined with geomorphological and geological data.

The application of shallow seismic techniques in the hanging wall area of the Atalanti normal fault, central Greece, provided new data on hanging wall deformation, the amount of crustal extension and the long-term slip distribution along the fault.

© 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