Across the entire mantle we interpret 94 positive seismic wave-speed anomalies as
subducted lithosphere and associate these slabs with their geological record. We document …

The rapid development of provincial seismic networks and portable seismic arrays has
provided a good opportunity to image the detailed 3-D seismic structure of the upper mantle …

A new P wave tomographic model of the mantle was constructed using more than 10 million
travel times. The finite‐frequency effect of seismic rays was taken into account by calculating …

Abstract The Yadong-Gulu Rift, cutting across the Gangdese belt and Himalayan terranes, is
currently associated with a thermal anomaly in the mantle and crustal melting at 15–20 km …

We present a new whole mantle P wave tomographic model GAP_P4. We used two data
groups; short‐period data of more than 10 million picked‐up onset times and long‐period …

We present a new anisotropic tomographic model of the uppermost mantle around eastern
Tibet using Pn traveltime data from a newly deployed temporary seismic array and recent …

Understanding of postseismic deformation following great subduction zone earthquakes is
complicated by the combined effects of viscoelastic relaxation of earthquake‐induced …

A key issue in the Cenozoic evolution of the Tibetan plateau is the geodynamic drivers for
north‐trending rifting in southern Tibet. Recent studies have demonstrated an eastward …

Seismic anisotropy records past and present tectonic deformations and provides important
constraints for understanding the structure and dynamics of the Earth's interior. In this work …

Seismic tomography provides unique constraints on the morphology, the deformation, and
(indirectly) the rheology of subducting slabs. We use teleseismic double-difference P-wave …