arXiv · cond-mat/0403173
Observation of Weak Localization of Seismic Waves
Abstract
We report the observation of weak localization of seismic waves in a natural environment. It emerges as a doubling of the seismic energy around the source within a spot of width a wavelength, that is several tens of meters in our case. The characteristic time for its onset is the scattering mean free time, that quantifies the internal heterogeneity.
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E. Larose, L. Margerin, B. A. van Tiggelen, M. Campillo. 2004-03-05. Observation of Weak Localization of Seismic Waves. https://arxiv.org/abs/cond-mat/0403173
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