Aseismic slip transients emerge spontaneously in three-dimensional rate and state modeling of subduction earthquake sequences

To investigate the possible physical mechanisms of recently observed aseismic slip events in the Cascadia, Japan and Mexico subduction zones, we apply a Dieterich‐Ruina rate and state friction law to a three dimensional model of a shallow subduction fault. That is loaded by imposed steady plate slip...

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Veröffentlicht in:	Journal of Geophysical Research. B. Solid Earth 2005-08, Vol.110 (B8), p.B08307.1-n/a
Hauptverfasser:	Liu, Yajing, Rice, James R.
Format:	Artikel
Sprache:	eng
Schlagworte:	3-D subduction fault aseismic slip transients Earth sciences Earth, ocean, space Exact sciences and technology rate and state friction
Online-Zugang:	Volltext
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