Evolving Fluid Source During the Growth of a Trench‐Parallel Seismogenic Fault System

Evolving Fluid Source During the Growth of a Trench‐Parallel Seismogenic Fault System

Abstract Fluid infiltration along seismically‐active faults and fluid‐rock interaction influence the mechanical behavior of faults. Nevertheless, how fluid infiltration and fluid‐rock interactions evolve at seismogenic depths with fault slip accumulation remain poorly constrained in the geological r...

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Main Authors: Simone Masoch, Luigi Dallai, Rodrigo Gomila, Michele Fondriest, Davide Novella, Giorgio Pennacchioni, José Cembrano, Giulio Di Toro
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
stable isotopes
seismogenic fault
hydrothermal systems
pseudotachylyte
intra‐arc fault system
Atacama Fault System
Online Access:https://doi.org/10.1029/2024GC011998
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https://doi.org/10.1029/2024GC011998

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