Fig. 10From: Geographical distribution of shear wave anisotropy within marine sediments in the northwestern PacificInterpretation of the observed S anisotropy within the marine sediments. a Sketch showing cracks and normal faulting within sediments in the outer rise region. b Sketch showing fractures within sediments due to basement deformation. c Sketch showing cracks and faults in the outer rise region due to the tensional stress associated with the bending of the Pacific PlateBack to article page