期刊
TECTONOPHYSICS
卷 431, 期 1-4, 页码 143-151出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/j.tecto.2006.05.043
关键词
GPS; 3D motion velocity; strain rate; seismicity; electromagnetic data; apparent resistivity
On the base of the GPS-measured velocity field referring to the recent crust movements over sizable terrestrial areas (Central Tien Shan), the strain rate tensor is evaluated as the tensor components are governed by space gradients of the velocity field. The areas of the extreme values of the strain rate tensor components are shown to coincide with the highest seismic activity areas. Also shown is the fact that, in the direction of the crust surface layer compression, the deep layer electric conductivity reaches its maximum. A simplest explanation of this phenomenon is proposed. (c) 2007 Published by Elsevier B.V.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据