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physics.geo-ph2024
Aftershocks as a time independant phenomenon
A. Mathey, J. Crassous, D. Marsan +2
Sequences of aftershocks following Omori's empirical law are observed after most major earthquakes, as well as in laboratory-scale fault-mimicking experiments. Nevertheless, the or…
physics.geo-ph2008★ 174 cited
High resolution 3D laser scanner measurements of a strike-slip fault quantify its morphological anisotropy at all scales
Francois Renard, Christophe Voisin, Davd Marsan +1
The surface roughness of a recently exhumed strikeslip fault plane has been measured by three independent 3D portable laser scanners. Digital elevation models of several fault surf…