Abstract
This study is based on a data set of aftershocks (location, fault-plane solutions) following the M=5.1 Arudy earthquake (02/29/80, French Western Pyrenees), and complementary geomorphological data (virtual geology using DEM and aerial photography). Data processing using Geophysical Information System are combined with identification of multi-structures based on the anisotropic wavelet formalism (NOAWC method). A local tectonic model and images of 2D propagation of the post-mainshock rupture are presented.
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