Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications
D Hatzfeld, P Molnar - Reviews of Geophysics, 2010 - Wiley Online Library
We compare the geologic histories, the deep structures, and the present‐day kinematics of
deformation of the Himalaya and the adjacent Tibetan Plateau with those of the Zagros and …
deformation of the Himalaya and the adjacent Tibetan Plateau with those of the Zagros and …
[HTML][HTML] Seismic anisotropy in the southeastern margin of the Tibetan Plateau and its deep tectonic significances
G Yuan, S YuTao, W Qiong - Chinese Journal of Geophysics, 2020 - dzkx.org
The southeastern (SE) margin of the Tibetan Plateau is a channel of the eastward escaping
material flow of the Tibetan Plateau. In order to fully understand the complex lithosphere …
material flow of the Tibetan Plateau. In order to fully understand the complex lithosphere …
[HTML][HTML] 青藏高原东南缘地震各向异性及其深部构造意义
高原， 石玉涛， 王琼 - 地球物理学报, 2020 - html.rhhz.net
青藏东南缘是青藏高原物质东流的通道, 为了更全面了解复杂的岩石圈结构和强烈的变形特征,
本文介绍了青藏东南缘岩石圈各向异性的形态, 综合其他研究者得到的该区域壳幔各向异性结果 …
本文介绍了青藏东南缘岩石圈各向异性的形态, 综合其他研究者得到的该区域壳幔各向异性结果 …
Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions
Competing geodynamic models, such as rigid-block extrusion, continuous deformation, and
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …
[HTML][HTML] 青藏高原东北缘上地幔地震各向异性: 来自SKS, PKS 和SKKS 震相分裂的证据
王琼， 高原， 石玉涛， 吴晶 - 地球物理学报, 2013 - html.rhhz.net
基于青藏高原东北缘甘肃区域台网41 个宽频带地震台站的远震记录资料, 通过PKS, SKS
和SKKS 震相的剪切波分裂分析, 获取了台站下方介质的各向异性分裂参数 …
和SKKS 震相的剪切波分裂分析, 获取了台站下方介质的各向异性分裂参数 …
岩浆作用与青藏高原演化
莫宣学 - 高校地质学报, 2011 - geology.nju.edu.cn
岩浆作用与青藏高原演化 Page 1 高校地质学报 Geological Journal of China Universities 2011
年9 月,第17 卷,第3 期,351-367页 September 2011,Vol. 17, No.3, p. 351-367 岩浆作用与青藏 …
年9 月,第17 卷,第3 期,351-367页 September 2011,Vol. 17, No.3, p. 351-367 岩浆作用与青藏 …
2008 年汶川M_s8. 0 地震发生过程的动力学机制研究
朱守彪， 张培震 - 地球物理学报, 2009 - cqvip.com
2008 年5 月12 日汶川地震突发在现今并不活动的龙门山断裂带上, 该地震发生的动力学机制
问题引起广泛关注. 文中利用黏弹性接触问题的有限元方法, 考虑重力作用 …
问题引起广泛关注. 文中利用黏弹性接触问题的有限元方法, 考虑重力作用 …
The boundary between the Indian and Asian tectonic plates below Tibet
The fate of the colliding Indian and Asian tectonic plates below the Tibetan high plateau may
be visualized by, in addition to seismic tomography, mapping the deep seismic …
be visualized by, in addition to seismic tomography, mapping the deep seismic …
Teleseismic P‐wave tomography and mantle dynamics beneath Eastern Tibet
J Lei, D Zhao - Geochemistry, Geophysics, Geosystems, 2016 - Wiley Online Library
We determined a new 3‐DP‐wave velocity model of the upper mantle beneath eastern Tibet
using 112,613 high‐quality arrival‐time data collected from teleseismic seismograms …
using 112,613 high‐quality arrival‐time data collected from teleseismic seismograms …
Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography
H Yao, RD van Der Hilst… - Journal of Geophysical …, 2010 - Wiley Online Library
Understanding the geotectonic evolution of the southeastern Tibetan plateau requires
knowledge about the structure of the lithosphere. Using data from 77 broadband stations in …
knowledge about the structure of the lithosphere. Using data from 77 broadband stations in …