Investigation of mantle kinematics beneath the Hellenic-subduction zone with teleseismic direct shear waves
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文摘

Splitting parameters obtained from teleseismic direct shear waves.

Reference Station Technique allowed receiving splitting parameters for 35 stations.

Increased number (∼10 times) of observations per station compared to previous studies.

Good regional coherency of NE-SW fast polarization directions and azimuthal coverage.

In agreement with prior studies and geodynamical simulations.

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