Pore Fluid Pressures and Strength Contrasts Maintain Frontal Fault Activity, Northern Hikurangi Margin, New Zealand
Author:
Affiliation:
1. Department of Earth, Environmental, and Planetary Sciences Rice University Houston TX USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL089209
Reference48 articles.
1. Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand
2. Slow slip source characterized by lithological and geometric heterogeneity
3. Slow wavespeeds and fluid overpressure in a region of shallow geodetic locking and slow slip, Hikurangi subduction margin, New Zealand
4. Hikurangi margin tsunami earthquake generated by slow seismic rupture over a subducted seamount
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3. Permeability and Elastic Properties of Rocks From the Northern Hikurangi Margin: Implications for Slow‐Slip Events;Geophysical Research Letters;2024-01-23
4. The Evolution of Pore Pressure, Stress, and Physical Properties During Sediment Accretion at Subduction Zones;Journal of Geophysical Research: Solid Earth;2023-06
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