RT Journal Article
T1 Estructuras sigmoïdes en el macizo granítico hercínico de Cauterets-Panticosa (Pirineos)
T1 Sigmoid structures in the Hercynian Cauterets-Panticosa granité (Pyrenees)
A1 Leblanc, D.
A1 Gleizes, Gérard
A1 Santana, V.
A1 Olivier, Phillippe
A1 Bouchez, J. L.
A1 Aranguren, A.
AB 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
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12476
UL http://hdl.handle.net/10272/12476
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026