Abstract
We investigate the resolving power of ISC/NEIC P
travel time data in tomographic inveisions for the geometry of the
subduction zones in the NW Pacific. From thermal models for the
Kurile, Japan, Izu-Bonin, Mariana and Ryukyu slabs, we generate
three dimensional synthetic velocity anomalies for subducting
slabs which are then projected onto a cell model
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