[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 esca**
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 …
Seismic imaging: From classical to adjoint tomography
Q Liu, YJ Gu - Tectonophysics, 2012 - Elsevier
Seismic tomography has been a vital tool in probing the Earth's internal structure and
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …
A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion
Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
Eastward expansion of the Tibetan Plateau by crustal flow and strain partitioning across faults
The lateral expansion of the southeastern Tibetan Plateau causes devastating earthquakes,
but is poorly understood. In particular, the links between regional variations in surface …
but is poorly understood. In particular, the links between regional variations in surface …
The community velocity model V. 1.0 of southwest China, constructed from joint body‐and surface‐wave travel‐time tomography
Southwest China, located at the southeastern margin of the Tibetan plateau, plays an
important role for the plateau growth and its material extrusion. It has complicated tectonic …
important role for the plateau growth and its material extrusion. It has complicated tectonic …
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 …
Shear wave velocity structure of the crust and upper mantle in Southeastern Tibet and its geodynamic implications
Southeastern Tibet, which has complex topography and strong tectonic activity, is an
important area for studying the subsurface deformation of the Tibetan Plateau. Through the …
important area for studying the subsurface deformation of the Tibetan Plateau. Through the …
USTClitho2. 0: Updated unified seismic tomography models for Continental China lithosphere from joint inversion of body‐wave arrival times and surface‐wave …
Abstract presented 3D seismic velocity models (VP and VS) of crust and uppermost mantle
of continental China using seismic body‐wave travel‐time tomography, which are referred to …
of continental China using seismic body‐wave travel‐time tomography, which are referred to …
Direct inversion of surface wave dispersion for three-dimensional shallow crustal structure based on ray tracing: methodology and application
We propose a method to invert surface wave dispersion data directly for 3-D variations of
shear wave speed, that is, without the intermediate step of phase or group velocity maps …
shear wave speed, that is, without the intermediate step of phase or group velocity maps …
High-resolution lithospheric structure beneath Mainland China from ambient noise and earthquake surface-wave tomography
We present a new high-resolution shear-velocity model of the lithosphere (down to about
160 km) beneath China using Rayleigh-wave tomography. We combined ambient noise and …
160 km) beneath China using Rayleigh-wave tomography. We combined ambient noise and …