Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4740945 | Journal of Applied Geophysics | 2009 | 8 Pages |
Abstract
Some numerical experiments are designed to elucidate geometrical details of fractures by studying scattering of elastic waves. The response in the time domain does not seem to provide much information. In the frequency domain, geometrical features of diffractors stamp a signature on reflected and diffracted wave fields. Results show that radiation patterns in the Mie regime are a promising device to infer some aspects such as shape and connectivity of the fractures. A combination of the direct and the indirect boundary element methods is used to compute numerical results. The numerical method is validated with analytic solutions for canonical problems.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
Rossana Vai, Francisco Luzón, Ursula Iturrarán-Viveros, Francisco J. Sánchez-Sesma,