How Fault Rocks Form and Evolve in the Shallow San Andreas Fault
Author:
Affiliation:
1. Earth & Planetary Sciences Department McGill University Montréal QC Canada
2. Now at Department of Geoscience University of Wisconsin‐Madison Madison WI USA
3. Earth & Planetary Science University of California Santa Cruz Santa Cruz CA USA
Funder
Southern California Earthquake Center
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC010092
Reference92 articles.
1. Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones
2. Permeability and frictional strength of cation-exchanged montmorillonite
3. The San Andreas Fault Paleoseismic Record at Elizabeth Lake: Why are There Fewer Surface-Rupturing Earthquakes on the Mojave Section?
4. Seismic waves in rocks with fluids and fractures
5. Paleoseismic Event Dating and the Conditional Probability of Large Earthquakes on the Southern San Andreas Fault, California
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1. In-situ rock shattering and strain localization along a seismogenic fault in dolostones (Monte Marine fault, Italian Central Apennines);Journal of Structural Geology;2024-06
2. Hematite Frictional Behavior and He Loss From Comminution During Deformation Experiments at Slow Slip Rates;Journal of Geophysical Research: Solid Earth;2024-03
3. Microscale Spatial Variations in Coseismic Temperature Rise on Hematite Fault Mirrors in the Wasatch Fault Damage Zone;Journal of Geophysical Research: Solid Earth;2023-03
4. Dolostone pulverization induced by coseismic rapid decompression of CO2-rich gas in nature (Matese, Apennines, Italy);Earth and Planetary Science Letters;2023-02
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