Fig. 8
The West Philippine Basin, showing the tomographically-determined locations of its subducted parts depicted as unfolded slabs (i.e. slabs restored to their original horizontal extents), coloured according to the P-wave velocity perturbation. The tomographic image also includes the low-velocity Anagolay Plateau, identified in this image simply as a ‘Subducted Plateau?’. Annotated image from Fig. 14 of Wu et al. (2016), reproduced here under the terms of Creative Commons Attribution-NonCommercial-NoDerivs Licensing. Note the role suggested here for an extended Aurora Fault