Leblanc, D.Gleizes, GérardSantana, V.Olivier, PhillippeBouchez, J. L.Aranguren, A.2016-07-082016-07-081996http://hdl.handle.net/10272/12476The 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 zonesspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/GranitesPyreneesMagnetic susceptibilityjournal articleopen access