(Q60704480)

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

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

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Bunichiro Shibazaki

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English

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publication date

2003

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Geophysical Research Letters

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volume

30

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issue

9

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cites work

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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Laboratory-Derived Friction Laws and Their Application to Seismic Faulting

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7 January 2021

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Dynamic rupture modeling with laboratory-derived constitutive relations

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

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Rock friction and its implications for earthquake prediction examined via models of Parkfield earthquakes

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Spatio-temporal complexity of slip on a fault

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Nucleation of large earthquakes determined by the seismic–aseismic boundary: agreement between models and observations

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7 January 2021

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Transition process from nucleation to high-speed rupture propagation: scaling from stick-slip experiments tonatural earthquakes

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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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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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