‘Melt welt’ mechanism of extreme weakening of gabbro at seismic slip rates
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature11370.pdf
Reference24 articles.
1. Tsutsumi, A. & Shimamoto, T. High-velocity frictional properties of gabbro. Geophys. Res. Lett. 24, 699–702 (1997)
2. Goldsby, D. & Tullis, T. Low frictional strength of quartz rocks at subseismic slip rates. Geophys. Res. Lett. 29, (2002)
3. Di Toro, G., Goldsby, D. L. & Tullis, T. E. Friction falls towards zero in quartz rock as slip velocity approaches seismic rates. Nature 427, 436–439 (2004)
4. Hirose, T. & Shimamoto, T. Fractal dimension of molten surfaces as a possible parameter to infer the slip-weakening distance of faults from natural pseudotachylytes. J. Struct. Geol. 25, 1569–1574 (2003)
5. Fialko, Y. & Khazan, Y. Fusion by earthquake fault friction: Stick or slip? J. Geophys. Res. 110, B12407 (2005)
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