Bathymetric Signatures of Submarine Forearc Deformation: A Case Study in the Nankai Accretionary Prism

Abstract Large earthquakes and tsunamis in subduction zone forearcs occur via slip on the shallow plate boundary and upper plate faults, but the locations, geometries, and slip histories of these faults can be difficult to constrain in regions with minimal subsurface geophysical and stratigraphic da...

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Bibliographic Details
Main Authors: Emily R. Schottenfels, Christine A. Regalla
Format: Article
Language:English
Published: Wiley 2021-11-01
Series:Geochemistry, Geophysics, Geosystems
Online Access:https://doi.org/10.1029/2021GC010050