Wrinkle-like Weertman pulse at the interface between two blocks of foam rubber with different velocities

Citation
A. Anooshehpoor et Jn. Brune, Wrinkle-like Weertman pulse at the interface between two blocks of foam rubber with different velocities, GEOPHYS R L, 26(13), 1999, pp. 2025-2028
Citations number
7
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICAL RESEARCH LETTERS
ISSN journal
00948276 → ACNP
Volume
26
Issue
13
Year of publication
1999
Pages
2025 - 2028
Database
ISI
SICI code
0094-8276(19990701)26:13<2025:WWPATI>2.0.ZU;2-3
Abstract
We verify the existence of self-sustaining wrinkle-like Weertman velocity p ulses along a prestressed interface between two dissimilar (Delta V = 60%) blocks of foam rubber. Properties of the observed velocity pulses are simil ar to the theoretical prediction of Weertman (1980), and the numerical calc ulations of Andrews and Ben-Zion (1997). Particle displacement, in the dire ction perpendicular to the fault, is much larger in the slower medium than in the faster medium, resulting in a separation of the interface during the passage of the slip pulse. The rupture velocity is neat the shear wave vel ocity in the slower material, and the direction of propagation is nearly al ways in the direction of the shear particle motion in the slower block. The pulse is self-maintaining, that is, it does not die out from radiation dam ping, obtaining the necessary energy by releasing locally stored shear pote ntial energy.