1996•Repositorio Institucional de la Universidad de Huelva (Universidad de Huelva)Open access

Estructuras sigmoides en el macizo granítico hercínico de Cauterets-Panticosa (Pirineos).

Denis R. LeBlanc, Gérard Gleizes, V. Santana, Phillippe Olivier, J. L. Bouchez, A. Aranguren

Abstract

The emplacement of the Cauterets-Panticosa granite massif (western Pyrenees) was controlled by dextral, 100° E-trending shear zones. The anisotropy of magnetic susceptibility allows us to obtain detailed structural maps of foliation trajectories and magmatic lineations of the Cauterets-Panticosa massif. Both types of structures draw large-scale sigmoid structures related to the dextral shear zones

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Available abstract

Key concepts: Sinistral and dextral, Massif, Lineation, Geology, Shear zone, Shear (geology), Foliation (geology), Geomorphology