In seismological full waveform inversion, the choice of misfit functions plays a critical role in
quantifying the discrepancy between observed and synthetic data, affecting convergence …

We present a novel hybrid method to simulate wave propagation through remote regional
models. By reviewing and refining the two main existing hybrid categories, the multiple point …

The dehydration of subducting slabs expels a massive amount of water into the forearc and
backarc mantle which is responsible for the serpentinization of the mantle wedge, as well as …

A new technique for P‐wave receiver function (PRF) inversion, within the framework of wave
equation‐based adjoint tomography and referred to as receiver function adjoint tomography …

We propose a novel framework for teleseismic traveltime tomography that requires no ray
tracing. The tomographic inverse problem is formulated as an Eikonal equation‐constrained …

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 …

Teleseismic waveforms contain abundant interpretable information about Earth's properties.
They can be used to explore the refined structure of Earth's interior, especially in the regions …

Receiver functions have been used for decades to study the Earth's major discontinuities by
focusing on converted waves. Deconvolution, which is the mathematical backbone of the …

Teleseismic receiver functions are widely used to map the depth and topography of various
major discontinuities in the Earth's mantle. To determine what precisely contributes to the …

Full-waveform inversion (FWI) is a high-resolution and computationally intensive imaging
technique to reconstruct unknown parameters in the computational model in which the …