RT Journal Article
T1 Estructura del pluton sincinematico de Lys (Zona Axial del Pirineo)
T1 Structure of the synkinematic Lys pluton (Pyrenean Axial Zone)
A1 Hilario, Asier
A1 Aranguren, A.
A1 Tubía, José María
A1 Pinotti, Lucio P.
AB From the structural study (using field, microstructural and anisotropy of magnetic susceptibility data) of the central traverse across the Lys pluton (Pyrenean Axial Zone), w'e propose that the emplacement of this pluton is synkinematic with the Variscan deformation of the Cambro-Ordovician schists that form its northern envelop. The late emplacement events involve a dextral transpressional deformation leading to the development of the Esera-Gistain and Caillaouas ductile shear zones. These Variscan shear zones were reactivated during the Pyrenean orogeny
PB Sociedad Geológica de España
YR 2003
FD 2003
LK http://hdl.handle.net/10272/9040
UL http://hdl.handle.net/10272/9040
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026