Lithospheric anisotropy beneath the Pyrenees from shear wave splitting

Mesozoic rifting had minimal impact on our study area, except locally within the Bay of Fundy and in southern Nova Scotia, where fast directions are subparallel to the opening

Since Fresnel zones of the com- monly used SKS waves are of the order of 100 km at upper mantle depths, and since splitting parameters vary at these scale length ( Fig. 2 a),

Upper mantle flow beneath the French Massif Central is investigated using teleseismic shear wave splitting induced by seismic anisotropy.. About 25 three-component stations

A combination of data from multiple experiments is used to obtain shear wave splitting parameters and a three-dimensional tomographic velocity model beneath a large portion of