学术报告

固体地球物理学术报告通知-郑应才

报告人:郑应才

报告题目:Deep earthquakes in slab anisotropy - the role of subducted carbonates and testable ideas

报告时间:星期四,2020-06-04 10:00 - 11:30

报告地点:Zoom(ID:724-620-904)

Why deep earthquakes are in subducted oceanic slab? By studying the non-double-couple seismic radiations of deep earthquakes, Li et al. (2018 nature geoscience) found that deep earthquakes are, like shallow earthquakes shear dislocations, but in anisotropic laminated fabric. In this talk, I’ll review these findings and propose possible origin of the anisotropy. Predictive testable hypotheses will be put forward for people to test the anisotropy idea.

上一篇:下一篇:
  • 地址:

    安徽省合肥市金寨路96号中国科学技术大学东区教学行政楼

  • 电话:

    0551-63601848

  • 邮箱:

    essadmin@ustc.edu.cn

Copyright © 2025 All Rights Reserved 中国科学技术大学地球和空间科学学院 版权所有.        皖ICP备05002528号

网站地图 - 法律声明