Lasheras Adot, E.Lago San José, MarcelianoGarcía Bellés, J.Arranz, Enrique2015-03-262015-03-261998http://hdl.handle.net/10272/10170The emplacement of basaltic sills and dykes outcropping in the Cinco Villas Massif (Western Pyrenees), northwards of the North-pyrenean fault, was controled by the hercynian main-phase cleavage (dykes) and by the orientation of three small half-graben permian basins (sills), unconformably overlain by the Buntsandstein conglomerates. Both types of magmatism are cogenetic and coevalspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Late-HercynianMagmatismPermianPyreneesjournal articleopen access