Geologic Evidence of Lithostatic Pore Fluid Pressures at the Base of the Subduction Seismogenic Zone
Abstract Geophysical and rheological work below the subduction seismogenic zone suggest that elevated pore fluid pressures (Pfs) may facilitate slow slip and tremor. However, quantification of Pf and its variation in this environment remain indirect and incomplete. We examine brittle‐frictional defo...
Saved in:
Main Authors: | C. B. Condit, M. E. French |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2022-06-01
|
Series: | Geophysical Research Letters |
Subjects: | |
Online Access: | https://doi.org/10.1029/2022GL098862 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Extensional forearc structures at the transition from Alaska to Aleutian Subduction Zone: slip partitioning, terranes and large earthquakes
by: Kahrizi, Amin, et al.
Published: (2023-07-01) -
Fluids, faulting and earthquakes in the brittle crust: recent advances and new challenges
by: Fabbri, Olivier, et al.
Published: (2024-05-01) -
Accretion versus erosion and sediment transfer balance near the subduction interface
by: Lallemand, Serge, et al.
Published: (2024-04-01) -
From subduction to collision and subduction again, the drivers of crustal-scale deformation in the Hellenides-Aegean region
by: Ferriere, Jacky, et al.
Published: (2023-11-01) -
Measurement and modeling of excess pore-water pressure in warm saturated frozen soil based on dynamic loading effect
by: Hu Zhang, et al.
Published: (2025-01-01)