Seismic evidence for thermal runaway during intermediate-depth earthquake rupture-Reference-Cited by-同舟云学术

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Seismic evidence for thermal runaway during intermediate-depth earthquake rupture

Published:2013-12-06 Issue:23 Volume:40 Page:6064-6068
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Prieto Germán A.¹,Florez Manuel¹,Barrett Sarah A.²,Beroza Gregory C.²,Pedraza Patricia³,Blanco Jose Faustino³,Poveda Esteban³

Affiliation:

1. Department of Earth, Atmospheric and Planetary Sciences; Massachusetts Institute of Technology; Cambridge Massachusetts USA

2. Department of Geophysics; Stanford University; Palo Alto California USA

3. Servicio Geológico Colombiano; Bogotá Colombia

Funder

NSF

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference41 articles.

1. Can observations of earthquake scaling constrain slip weakening?;Abercrombie;Geophys. J. Int.,2005

2. Global variations of stress drop for moderate to large earthquakes;Allmann;J. Geophys. Res.,2009

3. Fossil earthquakes recorded by pseudotachylytes in mantle peridotite from the Alpine subduction complex of Corsica;Andersen;Earth Planet. Sci. Lett.,2006

4. Stress release in exhumed intermediate-deep earthquakes determined from ultramafic pseudotachylyte;Andersen;Geology,2008

5. Radiated seismic energy from coda measurements and no scaling in apparent stress with seismic moment;Baltay;J. Geophys. Res.,2010

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