Thesis Collection
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Browsing by Author "Abati, J."
Now showing items 1-6 of 6
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Edad U-Pb en monacitas y rútilos de los paragneises de la Unidad de Agualada (Complejo de Ordenes, NW del Macizo Ibérico)
(Sociedad Geológica de España, 2002)The Agualada Unit is a small (3x5 km) tectonic slice of the lowermost allochthon of the Órdenes Complex. It is mainly formed by orthogneisses, migmatitic paragneisses and numerous mafic lenses. The nature of the lenses ... -
Evolución metamórfica de los esquistos de AP/BT de Ceán (Unidad de Malpica-Tui, NW del Macizo Ibérico)
(2007)Metapelitic schists from the upper structural levels of the Malpica-Tui Unit contain an initial blueschist facies mineral assemblage that appears mainly preserved as micro-inclusions in garnet, albite and chloritoid po ... -
Phase equilibrium modelling in the KFMASH system to show the Metamorphic Evolution of the Ceán Schists (Malpica-Tui Unit, NW Iberian Massif)
(2008)Para complementar los resultados obtenidos mediante termobarometría convencional (termómetro granatemoscovita y barómetros GRIPS y GASP) en los Esquistos de Ceán (López-Carmona et al., 2008) se ha construido una pseudosección ... -
Plegamiento recumbente en la Serra do Galiñeiro (Pontevedra, NO España)
(2006)Three main deformation phases (D1, D2 and D3) have been identified in the Serra do Galiñeiro using macro and microstructural analysis. The geometric characterization of those showing macrostructural elements (D2 and D3), ... -
Subduction and syn-collisional exhumation of a Paleozoic continental margin: an integrated study based on structures and P-T paths of the Basal Units in the Ordenes Complex (Galicia, Spain)
(Sociedad Geológica de España, 1996)According to their metamorphic evolution, the Basal Units of the Galician Allochthonous Complexes are thought to represent a part of the margin of the Paleozoic Gondwana, subducted at the onset of the Variscan Orogeny. ... -
Tectonic setting of the Monte Castelo Gabbro (Ordenes Complex, NW Iberian Massif)
(Sociedad Geológica de España, 2002)En el Complejo de Ordenes (NW del Macizo Ibérico) la unidad tectonoestratigráfica superior está constituida por una potente secuencia metasedimentaria (Serie de Ordenes), intruida por ortogneises y gabros. El Cabro de Monte ...
