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 …
Magmatism within the northern margin of the South China Sea during the post-rift stage: An overview, and new insights into the geodynamics
Abstract The South China Sea, which is located to the southeast of Eurasian continent,
developed as the result of intra-continental rifting and seafloor spreading on the South …
developed as the result of intra-continental rifting and seafloor spreading on the South …
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 …
Transcurrent tectonic system and deep seismogenic mechanism in the southeastern Tibetan Plateau: A view from gravity and magnetic anomalies
Abstract The southeastern Tibetan Plateau margin (SETPM) is characterized by a series of
curved strike-slip faults around the eastern Himalayan Syntaxis. Influenced by the …
curved strike-slip faults around the eastern Himalayan Syntaxis. Influenced by the …
The high-resolution community velocity model V2. 0 of southwest China, constructed by joint body and surface wave tomography of data recorded at temporary dense …
Abstract The Sichuan-Yunnan area is located at the southeastern margin of the Tibetan
Plateau, where tectonic movement is strong with deep and large faults distributed in a …
Plateau, where tectonic movement is strong with deep and large faults distributed in a …
A new crustal shear-velocity model in Southwest China from joint seismological inversion and its implications for regional crustal dynamics
Southwest (SW) China is located in a transition site from the active Tibetan Plateau to the
stable Yangtze craton, which has complicated tectonic deformation and severe seismic …
stable Yangtze craton, which has complicated tectonic deformation and severe seismic …
Massive lithospheric delamination in southeastern Tibet facilitating continental extrusion
Significant left-lateral movement along the Ailao Shan-Red River fault accommodated a
substantial amount of the late Eocene to early Miocene India-Asia convergence. However …
substantial amount of the late Eocene to early Miocene India-Asia convergence. However …
P wave tomography and anisotropy beneath Southeast Asia: Insight into mantle dynamics
Southeast Asia is surrounded by subduction zones resulting from the interactions of several
lithospheric plates. Its evolution has been also influenced by active tectonics due to the Indo …
lithospheric plates. Its evolution has been also influenced by active tectonics due to the Indo …
The mechanism of deep material transport and seismogenic environment of the **aojiang fault system revealed by 3-D magnetotelluric study
The **aojiang fault system (XJFS), located to the southeast of the Tibetan Plateau, has a
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …
[HTML][HTML] Is there a big mantle wedge under eastern Tibet?
The big mantle wedge (BMW) model was originally proposed to explain the origin of the
intraplate Changbaishan volcano in NE China where the subducting Pacific slab becomes …
intraplate Changbaishan volcano in NE China where the subducting Pacific slab becomes …