@article{10272/12476,
year = {1996},
url = {http://hdl.handle.net/10272/12476},
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},
publisher = {Sociedad Geológica de España},
title = {Estructuras sigmoïdes en el macizo granítico hercínico de Cauterets-Panticosa (Pirineos)},
title = {Sigmoid structures in the Hercynian Cauterets-Panticosa granité (Pyrenees)},
author = {Leblanc, D. and Gleizes, Gérard and Santana, V. and Olivier, Phillippe and Bouchez, J. L. and Aranguren, A.},
}