Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of the Seismological Society of America Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; December 2003; v. 93; no. 6; p. 2375-2388; DOI: 10.1785/0120020090
© 2003 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (16)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Nielsen, S.
Right arrow Articles by Madariaga, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

On the Self-Healing Fracture Mode

S. Nielsen and R. Madariaga

Istituto Nazionale di Geofisica e Vulcanologia
Roma, Italy
(S.N.)
Ecole Normale Superieure de Paris
Laboratoire de Géologie
Paris, France
(R.M.)

Manuscript received 27 March 2002.

We present the analytical solution for a fundamental fracture mode in the form of a self-similar, self-healing pulse. The existence of such a fracture mode was strongly suggested by recent numerical simulations of seismic ruptures but, to our knowledge, no formal proof of their origin has been proposed yet. We present a two-dimensional, anti-plane solution for fixed rupture and healing speeds that satisfies both the wave equation and crack boundary conditions for a simple Coulomb friction law in the absence of any rate or state dependence. This solution is an alternative to the classic self-similar crack solution by Kostrov. In practice, the self-healing impulsive mode rather than the expanding crack mode is selected depending on details of fracture initiation and is thereafter self-maintained. We discuss stress concentration, fracture energy, and rupture velocity and compare them to the case of a crack. The analytical study is complemented by various numerical examples and comparisons. On more general grounds, we argue that an infinity of marginally stable fracture modes may exist in addition to the crack solution or the impulsive fracture described here.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
S. Murphy and S. Nielsen
Estimating Earthquake Magnitude with Early Arrivals: A Test Using Dynamic and Kinematic Models
Bulletin of the Seismological Society of America, February 1, 2009; 99(1): 1 - 23.
[Abstract] [Full Text] [PDF]


Home page
Proc. Natl. Acad. Sci. USAHome page
X. Lu, N. Lapusta, and A. J. Rosakis
From the Cover: Pulse-like and crack-like ruptures in experiments mimicking crustal earthquakes
PNAS, November 27, 2007; 104(48): 18931 - 18936.
[Abstract] [Full Text] [PDF]


Home page
ScienceHome page
G. Lykotrafitis, A. J. Rosakis, and G. Ravichandran
Self-healing pulse-like shear ruptures in the laboratory.
Science, September 22, 2006; 313(5794): 1765 - 1768.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
E. Tinti, E. Fukuyama, A. Piatanesi, and M. Cocco
A Kinematic Source-Time Function Compatible with Earthquake Dynamics
Bulletin of the Seismological Society of America, August 1, 2005; 95(4): 1211 - 1223.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
J. R. Rice, C. G. Sammis, and R. Parsons
Off-Fault Secondary Failure Induced by a Dynamic Slip Pulse
Bulletin of the Seismological Society of America, February 1, 2005; 95(1): 109 - 134.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America