The adjoint method is a popular method used for seismic (full-waveform) inversion today.
The method is considered to give more realistic and detailed images of the interior of the …

We investigate the properties of mantle discontinuities beneath the Arctic Ocean and the
Aleutian-Alaska subduction zone with underside reflections of PP and SS waves. The depth …

The dynamic processes associated with subducting tectonic plates and rising plumes of hot
material are typically treated separately in dynamical models and seismological studies …

There is mounting evidence for the presence of seismic reflectors in the mantle at a depth of
around 1000 km, however, the cause for these reflectors is not yet well established and …

The coesite‐stishovite phase transition is considered the most plausible candidate to
explain the X‐discontinuity observed at around 300 km depth in a variety of tectonic settings …

Abstract The Transantarctic Mountains (TAMs), Antarctica, exhibit anomalous uplift and
volcanism and have been associated with regions of thermally perturbed upper mantle that …

The effects of reaction kinetics of bridgmanite and ferropericlase transforming to ringwoodite
on elastic properties in upwelling mantle are investigated using data of kinetic experiments …

Detailed geomorphology of the 410-km phase-transition discontinuity offers important
information about the thermal state and dynamics of the Earth interior. We generated a high …