Elasticity is described in general by a fourth-order tensor with 21 independent coefficients,
which corresponds to the triclinic symmetry class. However seismological observations are …

Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth′ s …

We study the 3-D strain evolution of the northern Aegean and the vertical coherency of
deformation. We observe that finite strain orientations in the mantle inferred from published …

Twenty‐six broadband seismic stations in an areal array spanning 500× 500 km across
Ethiopia were used for shear‐wave splitting studies. Our results show small‐to‐moderate …

We use forward models based on recent high‐pressure experimental data on mantle
minerals to predict the seismic anisotropy produced by plastic strain of orthorhombic …

We measure SKS splitting parameters and P and S delay times in the Mediterranean region
using broad-band recordings from the temporary MIDSEA array and permanent networks …

The nature of upper-mantle seismic anisotropy beneath central and eastern North America
has been evaluated using the phase velocities of surface waves traversing the length of the …

During mantle flow at mid-ocean ridges, viscous shear deformation imparts a structural
fabric that remains in the lithosphere as it cools, preserving a record of ridge processes over …

We present a high-resolution Sv-wave velocity and azimuthal anisotropy model for the upper
mantle beneath the North Atlantic and surrounding region derived from the analysis of over …

Despite similar surface transform faulting behaviour, observed shear-wave splitting patterns
in the California and New Zealand plate boundary regions are markedly different. To better …