The Long Recurrence Intervals of Small Repeating Earthquakes May Be Due to the Slow Slip Rates of Small Fault Strands
Author:
Affiliation:
1. School of Earth and Environment University of Leeds Leeds UK
2. Department of Earth Sciences University of Oxford Oxford UK
3. École et Observatoire des Sciences de la Terre Université de Strasbourg Strasbourg France
Funder
National Centre for Earth Observation
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084778
Reference48 articles.
1. Stress drops of repeating earthquakes on the San Andreas Fault at Parkfield
2. Spatial and temporal stress drop variations in small earthquakes near Parkfield, California
3. Global variations of stress drop for moderate to large earthquakes
4. Quasi-Static Slip-Rate Shielding by Locked and Creeping Zones as an Explanation for Small Repeating Earthquakes at Parkfield
5. A Simple Stick-Slip and Creep-Slip Model for Repeating Earthquakes and its Implication for Microearthquakes at Parkfield
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1. Partial Ruptures Cannot Explain the Long Recurrence Intervals of Repeating Earthquakes;Journal of Geophysical Research: Solid Earth;2024-01
2. A Repeating Earthquake Catalog From 2003 to 2020 for the Raukumara Peninsula, Northern Hikurangi Subduction Margin, New Zealand;Geochemistry, Geophysics, Geosystems;2021-04-30
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