The Green's function (GF) method, which makes use of GFs, is an important and elegant tool
for solving a given boundary-value problem for the differential equation from a real …

Seismic anisotropy is a key observational tool for mapping flow in Earth's upper mantle.
However, interpreting patterns of anisotropy relies on a firm understanding of the …

Thermal runaway has been proposed as a potential mechanism to initiate intermediate-
depth earthquakes as well as lithospheric-scale shear zones at depths of 50–300 km where …

Seismic anisotropy arises in the upper mantle due to the alignment of olivine crystal lattices
and is often used to interpret mantle flow direction. Experiments on the evolution of olivine …

The nature of lattice‐preferred orientation (LPO) in olivine‐rich rocks strongly influences
many important physical properties of Earth's upper mantle. Different LPO types have been …

Crystallographic preferred orientation (CPO) of peridotite minerals is frequently invoked to
explain the widespread dependence of seismic wave speed on propagation direction in …

The crystallographic preferred orientation (CPO) of polycrystalline olivine affects both the
viscous and seismic anisotropy of Earth's upper mantle with wide geodynamical …

Seismic anisotropy records continental dynamics in the crust and convective deformation in
the mantle. Deciphering this archive holds huge promise for our understanding of the thermo …

Asthenospheric shear causes some minerals, particularly olivine, to develop anisotropic
textures that can be detected seismically. In laboratory experiments, these textures are also …

Viscoplastic deformation of mantle rocks produces crystal preferred orientations (CPO or
texture) of olivine and, by consequence, an anisotropic mechanical response for subsequent …