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Velocity‐Porosity Relations in Carbonate and Siliciclastic Subduction Zone Input Materials

Abstract The mechanical, physical, and frictional properties of incoming materials play an important role in subduction zone structure and slip behavior because these properties influence the strength of the accretionary wedge and megathrust plate boundary faults. Incoming sediment sections often sh...

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Autors principals: Tamara N. Jeppson, Hiroko Kitajima
Format: Artigo
Idioma:Inglês
Publicat: Wiley 2022-01-01
Col·lecció:Geochemistry, Geophysics, Geosystems
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Accés en línia:https://doi.org/10.1029/2021GC010074
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