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  5. Can flash heating of asperity contacts prevent melting?
 
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Can flash heating of asperity contacts prevent melting?

Author(s)
Bizzarri, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Language
English
Obiettivo Specifico
3.1. Fisica dei terremoti
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Geophysical Research Letters  
Issue/vol(year)
/36 (2009)
Publisher
AGU
Pages (printed)
L11304
Date Issued
June 4, 2009
DOI
10.1029/2009GL037335
Alternative Location
http://www.bo.ingv.it/~bizzarri/
URI
https://www.earth-prints.org/handle/2122/5070
Subjects
04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution  
Subjects

Earthquake dynamics

Constitutive laws

Abstract
We solve the elasto-dynamic problem for a 3-D
rupture, spontaneously propagating on a fault, obeying rate- and state-dependent friction. We explore, through numerical simulations with physically realistic constitutive parameters, the effects on dynamic traction evolution of the flash heating of microscopic asperity contacts. Our results demonstrate that the inclusion of flash heating tends to increase the degree of instability of a homogeneous fault:
the supershear rupture regime is favored, significantly larger stress drops are realized and weakening distance and fracture energy increase. We show that the key parameter which controls the temperature evolution and the activation of the flash heating is the slipping zone width, 2w. We found that for localized shear the rupture exhibits a pulse-like behavior. On the contrary, for large slipping zones, the rupture develops as a sustained crack. Finally, we show that flash heating enhances the onset of melting.
Type
article
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2009GL037335.pdf

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