@article{10272/18403,
year = {1988},
url = {http://hdl.handle.net/10272/18403},
abstract = {The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the third hercynian deformation phase (F) and are cross-cut by the Berzosa Fault, a normal accident with a dextral wrench component
 The ductile shear zone that outcrops in the core the El Cardoso Antiform can be related to that which exists west of the Berzosa Fault and also to that which affects the overturned  limb of the Hiendelaencina Anticline},
publisher = {Sociedad Geológica de España},
keywords = {Geología estructural},
keywords = {Orógeno Herciniano},
keywords = {Sierra de Guadarrama},
keywords = {Structural geology},
keywords = {Hercynian Orogeny},
title = {Sobre la estructura del Antiforme de El Cardoso y el Sinforme de Majaelrayo y su relación con la Falla de Berzosa},
author = {González Lodeiro, Francisco and Martínez Catalán, José R. and Macaya, J. and Álvarez, F.},
}