The normalised optimised anisotropic wavelet coefficient (NOAWC) method: An image processing tool for multi-scale analysis of rock fabric

Philippe Gaillot (1) , José Darrozes (1, 2) , Michel de Saint Blanquat (1, 2) , Guy Ouillon (3)

1 Laboratoire de Pétrophysique et Tectonique
2 LMTG - Laboratoire des Mécanismes et Transfert en Géologie
3 LPMC - Laboratoire de physique de la matière condensée

The 2D Anisotropic Wavelet Transform (2DAWT) is an image analysis tool which is able to decipher signals where information obtained from different scales are intermixed. Extended from the Optimised Anisotropic Wavelet Coefficient method (OAWC) of Ouillon et al. [1995], we present a method which discriminates the objects and groups of objects depending on their area, shape ratio, orientation and position. Illustrated in a synthetic example, we show that this method allows one to distinguish between different sub-populations of objects within a single phase, and quantify the anisotropies of shape, orientation and spatial distribution at different scales (objects, clusters of objects, alignments of objects or clusters). Applied to a natural rock sample (Sidobre granite, Montagne Noire, France), the 2DAWT has permitted us to detect and accurately characterise the different levels of mineral organisation, and thus, to contribute to the understanding of the physical processes, such as crystallisation, fluid migration, deformation, etc... responsible for such organisations.

Mots clés: Physical Properties of Rocks: General or miscellaneous

Domaines: Sciences de la Terre

Philippe Gaillot, José Darrozes, Michel de Saint Blanquat, Guy Ouillon. The normalised optimised anisotropic wavelet coefficient (NOAWC) method: An image processing tool for multi-scale analysis of rock fabric. Geophysical Research Letters, 1997, 24, pp.1819-1822. ⟨10.1029/97GL01601⟩. ⟨hal-00590664⟩