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Browsing by Subject "Crustal thinning"
Now showing items 1-5 of 5
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Fallas normales de bajo ángulo a gran escala en las Béticas occidentales
(Sociedad Geológica de España, 1990)Low angle normal faults (LANF) related with extensional detachments are mapped in the Western Betics. They developed during the Middle and Late Miocene on continental crust which was previously thickened by fold- and ... -
Les failles normales a faible pendage du Rif interne (Maroc) et leur effet sur l'amincissement crustal du domaine D'Alboran
(Sociedad Geológica de España, 1994)Several low angle, shallow dippinng normal faults are described from the internal domaine of the Rif chain. They dip gently towards the Alboran sea and cause important omissions in the stratigraphictectonic pile. These ... -
Registro metamorfico de alta presión-baja temperatura en la unidad de Jubrique e imbricaciones de Benarrabá (Cordillera Bético-Rifeña)
(Sociedad Geológica de España, 1994)The presence of carpholitep seudomorphs and the kyanite-chloritoid-chlorite association in the Jubrique unitphy/iites and in the Benarrabá imbrications indicates metam rphic conditions of T < 450º C and P> 8 Kb. This means ... -
Relación estructural entre los cuerpos peridotíticos situados al Norte y al Sur del Estrecho de Gibraltar
(Sociedad Geológica de España, 1994)The peridotite bodies of the Bedes and Rif, on either side of the Strait of Gibraltar, are intercaled among the highest units of the Alpujarride complex. Before Miocene times, they must have constituted an uitramaficsiab ... -
Sobre el adelgazamiento mioceno del Dominio Cortical de Alborán, el Despegue Extensional de Filabres (Béticas orientales)
(Sociedad Geológica de España, 1988)In the Alboran Domain, the Alpujarride/Nevado-Filabride major boundary is a brittleductile and brittle detachment (Filabres Extensional Detachment, FED) which thinned the Nevado-ñlabride complex during the Miocene. The FED ...
