We report a new model of radially anisotropic crustal and upper mantle structure of the
western United States (WUS324) obtained from full waveform inversion of earthquake data …

Seismic tomography harnesses earthquake data to explore the inaccessible structure of the
Earth. Adjoint waveform tomography (AWT), a method of seismic tomography, updates the …

We present REVEAL, a global‐scale, transversely isotropic full‐waveform inversion model.
REVEAL builds upon the earlier construction of the long‐wavelength Earth (LOWE) model …

We present a new model of radially anisotropic seismic wavespeeds for the crust and upper
mantle of a broad region of the Middle East and Southwest Asia (MESWA) derived from …

We investigate the upper-crustal structure of the Rukwa–Tanganyika rift zone in East Africa,
where the Tanganyika rift interacts with the Rukwa and Mweru-Wantipa rift tips, evidenced …

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 …

Tectonic forces alone cannot drive rifting in old and thick continental lithosphere.
Geodynamic models suggest that thermal weakening is critical for lithospheric extension, yet …

Objectively exploring global variations in crust and upper mantle structure helps constrain
fundamental aspects of Earth's plate tectonic and convective processes. Here we adopted a …

The obduction of the Tethys oceanic lithosphere is documented by the Semail ophiolite
along the northeastern Arabian continental margin. Although the ophiolite is continuous and …

Nowadays, the most successful applications of full‐waveform inversion (FWI) involve marine
seismic data under acoustic approximations. Elastic FWI of land seismic data is still …