@article{10272/10170,
year = {1998},
url = {http://hdl.handle.net/10272/10170},
abstract = {The 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 coeval},
publisher = {Sociedad Geológica de España},
keywords = {Late-Hercynian},
keywords = {Magmatism},
keywords = {Permian},
keywords = {Pyrenees},
title = {Emplazamiento de sills y diques del Pérmico superior en el Macizo de Cinco Villas (Pirineo Navarro)},
title = {Upper Permian emplacement of sills and dykes, in the Cinco Villas Massif (Navarra, Western Pyrenees)},
author = {Lasheras Adot, E. and Lago San José, Marceliano and García Bellés, J. and Arranz, Enrique},
}