Lowermost mantle shear velocity anisotropy beneath Siberia

被引：0
|
作者：
杨凤琴
刘斌
倪四道
曾祥方
戴志阳
吕彦
机构：
[1] Hefei 230026 China
[2] School of Earth and Space Science University of Science and Technology of China
[3] School of Earth and Space Science University of Science and Technology of China
来源：
Earthquake Science | 2008年 / 02期
基金：
中国国家自然科学基金;
关键词：
anisotropy; shear wave splitting; D’; region; lowermost mantle; Siberia;
D O I：
暂无
中图分类号：
P315.31 [];
学科分类号：
070801 ;
摘要：
Introduction D’’ layer plays an important role in geodynamic process. And seismological research indicates that D’’ layer has large scale seismic anisotropy, however, most research concentrated on areas such as Northern Pacific, Central Pacific, Caribbean, Central America, Alaska etc. (Wookey et al, 2005; Garnero and Lay, 2003; Matzel et al, 1996
引用
收藏
页码：213 / 216 +220
页数：5
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