(Q56997365)

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

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

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Yajing Liu

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language of work or name

English

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publication date

2005

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published in

Journal of Geophysical Research

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volume

110

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issue

B8

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cites work

Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault

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reference URL

https://api.crossref.org/works/10.1029%2F2004JB003424

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21 January 2018

A silent slip event on the deeper Cascadia subduction interface

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7 January 2021

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A slow thrust slip event following the two 1996 Hyuganada Earthquakes beneath the Bungo Channel, southwest Japan

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https://api.crossref.org/works/10.1029%2F2004JB003424

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7 January 2021

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High pore fluid pressure may cause silent slip in the Nankai Trough.

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https://api.crossref.org/works/10.1029%2F2004JB003424

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7 January 2021

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A large silent earthquake in the Guerrero seismic gap, Mexico

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https://api.crossref.org/works/10.1029%2F2004JB003424

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7 January 2021

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Transient fault slip in Guerrero, southern Mexico

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7 January 2021

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Nonvolcanic deep tremor associated with subduction in southwest Japan

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7 January 2021

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Detection and monitoring of ongoing aseismic slip in the Tokai region, central Japan

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7 January 2021

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Seismic consequences of warm versus cool subduction metamorphism: examples from southwest and northeast japan

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7 January 2021

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Spatio-temporal complexity of slip on a fault

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7 January 2021

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Slip complexity in earthquake fault models

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7 January 2021

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Stability of Steady Frictional Slipping

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7 January 2021

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Rate and state dependent friction and the stability of sliding between elastically deformable solids

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https://api.crossref.org/works/10.1029%2F2004JB003424

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7 January 2021

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Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip

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7 January 2021

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Earthquakes and friction laws

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7 January 2021

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On the physical mechanism of silent slip events along the deeper part of the seismogenic zone

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7 January 2021

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Transition between frictional slip and ductile flow for halite shear zones at room temperature.

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https://api.crossref.org/works/10.1029%2F2004JB003424

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7 January 2021

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

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