We present a new global thermochemical model of the lithosphere and underlying upper
mantle constrained by state of the art seismic waveform inversion, satellite gravity (geoid …

Surface wave tomography using dispersion data to obtain isotropic and anisotropic shear
wave velocity structures is a very efficient approach to study regional and global tectonics …

The Tethyan evolution depicts the continuous process of landmasses separating from the
Gondwana continent in the south, drifting northwards, and subsequently colliding with the …

Mantle shear velocity (Vs) structure beneath the Transportable Array (TA) in Alaska and
northwestern Canada is imaged by joint inversion of Rayleigh wave dispersion and …

Understanding the distribution and mobility of crystal mushes within modern magmatic
systems is crucial to volcanic hazard assessments as distinct pockets of mobile magma may …

We present a high-resolution 3-D crustal model of southeastern Tibetan Plateau (SE Tibet)
by joint inversion of local earthquake P-wave travel-times and Bouguer gravity anomalies …

Seismic wave speed is controlled by a number of factors, including temperature and
chemical composition, as well as the presence of volatiles and partial melt. Tomography …

Variations in temperature within the Earth are of great interest because they indicate the
thickness and, consequently, mechanical strength of the lithosphere and density variations …

The eastern margin of North America has been shaped by a series of tectonic events
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …

We presented two high‐resolution, three‐dimensional (3D) global P‐and joint S‐wave
velocity models of the whole mantle with a particular focus on the North Pacific realm using …