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Anisotropy and mantle flow of the Indo-Burma subduction zone from shear wave splitting and shear wave splitting tomography
(University of Missouri--Columbia, 2020)
the slab in response to the slab roll-back. The mantle wedge shows a complex deformational fabric with an average lag time of over 0.5s. Dextral motion along the Sagaing fault induces a dominant trench parallel fabric on the mantle wedge. Null results...