Plate‐Rate Frictional Behavior of Sediment Inputs to the Hikurangi Subduction Margin: How Does Lithology Control Slow Slip Events?
Author:
Affiliation:
1. MARUM Center for Marine Environmental Sciences University of Bremen Bremen Germany
2. Faculty of Geosciences University of Bremen Bremen Germany
Funder
European Research Council
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010369
Reference86 articles.
1. Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand
2. Site U1520
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4. Physical analysis of the state- and rate-dependent friction law. II. Dynamic friction
5. Crossover from creep to inertial motion in friction dynamics
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