Constraining the Effect of Bathymetric High Subduction in an Accretionary Wedge: Evidence From the Tokai Area of the Nankai Trough, Japan

Abstract The Tokai area in the eastern Nankai Trough is characterized by the subduction of a rough plate interface caused by bathymetric highs related to the adjacent Izu‐Bonin arc and fault fabrics in the oceanic crust. However, the effect of this process on the structural development of its accret...

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Bibliographic Details
Main Authors: Andrzej Górszczyk, Rafael Almeida, Romain Brossier, Ludovic Métivier, Stéphane Operto
Format: Article
Language:English
Published: Wiley 2025-03-01
Series:Geochemistry, Geophysics, Geosystems
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Online Access:https://doi.org/10.1029/2024GC011754
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