Crustal radial anisotropy across eastern Tibet and the western Yangtze craton
Phase velocities across eastern Tibet and surrounding regions are mapped using Rayleigh
(8–65 s) and Love (8–44 s) wave ambient noise tomography based on data from more than …
(8–65 s) and Love (8–44 s) wave ambient noise tomography based on data from more than …
GPS determined coseismic slip of the 2021 Mw7.4 Maduo, China, earthquake and its tectonic implication
M Wang, F Wang, X Jiang, J Tian, Y Li… - Geophysical Journal …, 2022 - academic.oup.com
SUMMARY The 2021 M w7. 4 Maduo earthquake occurred on the Jiangcuo fault within the
Bayan Har block in eastern Tibet. It is a rather unique event and attests that large …
Bayan Har block in eastern Tibet. It is a rather unique event and attests that large …
Present-day crustal deformation and strain transfer in northeastern Tibetan Plateau
Y Li, M Liu, Q Wang, D Cui - Earth and Planetary Science Letters, 2018 - Elsevier
The three-dimensional present-day crustal deformation and strain partitioning in
northeastern Tibetan Plateau are analyzed using available GPS and precise leveling data …
northeastern Tibetan Plateau are analyzed using available GPS and precise leveling data …
Strong variability in the thermal structure of Tibetan Lithosphere
We present a model of thermal lithospheric thickness (the depth where the geotherm
reaches a temperature of 1300° C) and surface heat flow in Tibet and adjacent regions …
reaches a temperature of 1300° C) and surface heat flow in Tibet and adjacent regions …
Limited southward underthrusting of the Asian lithosphere and material extrusion beneath the northeastern margin of Tibet, inferred from teleseismic Rayleigh wave …
The northeastern margin of Tibet is of key importance in understanding the uplift and
expansion of Tibetan Plateau. In this research, we perform Rayleigh wave tomography from …
expansion of Tibetan Plateau. In this research, we perform Rayleigh wave tomography from …
Shear-velocity structure, radial anisotropy and dynamics of the Tibetan crust
Geophysical and geological data suggest that Tibetan middle crust is a partially molten,
mechanically weak layer, but it is debated whether this low-viscosity layer is present …
mechanically weak layer, but it is debated whether this low-viscosity layer is present …
Crustal layering in northeastern Tibet: A case study based on joint inversion of receiver functions and surface wave dispersion
Recently constructed models of crustal structure across Tibet based on surface wave data
display a prominent mid-crustal low velocity zone (LVZ) but are vertically smooth in the crust …
display a prominent mid-crustal low velocity zone (LVZ) but are vertically smooth in the crust …
[HTML][HTML] 基于2001年MW7.8可可西里地震震后形变模拟研究藏北地区岩石圈流变学结构
贺鹏超， 王敏， 王琪， 沈正康 - 地球物理学报, 2018 - html.rhhz.net
青藏高原岩石圈的流变学结构和形变机制是地学界长期争论的重大科学问题. 2001
年发生在东昆仑断裂带的MW 7.8 可可西里地震造成青藏高原北部地区岩石圈构造应力场的很大 …
年发生在东昆仑断裂带的MW 7.8 可可西里地震造成青藏高原北部地区岩石圈构造应力场的很大 …
Crustal structure of the Eratosthenes Seamount, Cyprus and S. Turkey from an amphibian wide-angle seismic profile
C Feld, J Mechie, C Hübscher, J Hall, S Nicolaides… - Tectonophysics, 2017 - Elsevier
Abstract In 2010, project CoCoCo (incipient COntinent-COntinent COllision) recorded a 650
km long amphibian NS wide-angle seismic profile, extending from the Anatolian plateau …
km long amphibian NS wide-angle seismic profile, extending from the Anatolian plateau …
Lithospheric structures of and tectonic implications for the central–east Tibetan plateau inferred from joint tomography of receiver functions and surface waves
M Feng, M An, J Mechie, W Zhao… - Geophysical Journal …, 2020 - academic.oup.com
We present an updated joint tomographic method to simultaneously invert receiver function
waveforms and surface wave dispersions for a 3-DS-wave velocity (Vs) model. By applying …
waveforms and surface wave dispersions for a 3-DS-wave velocity (Vs) model. By applying …