Organisation of joints and faults from 1-cm to 100-km scales revealed by optimized anisotropic wavelet coefficient method and multifractal analysis
The classical method of statistical physics deduces the macroscopic behaviour of a system from the organization and interactions of its microscopical constituents. This kind of problem can often be solved using procedures deduced from the Renormalization Group Theory, but in some cases, the basic mi...
Main Authors: | G. Ouillon, D. Sornette, C. Castaing |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
1995-01-01
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Series: | Nonlinear Processes in Geophysics |
Online Access: | http://www.nonlin-processes-geophys.net/2/158/1995/npg-2-158-1995.pdf |
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