Thesis Collection
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Browsing by Author "Díaz García, F."
Now showing items 1-6 of 6
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Estructura del granito de Beariz (Ourense, Galicia)
(2006)The geological map, cross-sections and structural analysis of the Beariz granite are presented. The Geometric and structural characteristics of this intrusive body are in good agreement with a sinkynematic emplacement within ... -
Evolución tectonotermal de la Unidad de Santiago (Complejo de Ordenes): un ejemplo de subducción eo-hercín¡ca y descompresión sin-colisional
(Sociedad Geológica de España, 1992)The syn-D2 uplift of the Santiago Unit, inmediately after of the high-pressure eo-Hercynian metamorphic event, cause a markedly decompressive-slightly prograde P,T,t path. This path very likely suggests that the majority ... -
Metapelitas de alta presión de la Unidad de Santiago (Complejo de Ordenes, NO del Macizo Ibérico)
(Sociedad Geológica de España, 1992)A high - pressure - low - to intermediate temperature eo - Hercynian metamorphic event characterizes the tectonothermal evolution of the Santiago Unit, in the western margin of the Ordenes Complex. P-T conditions fo r the ... -
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 ... -
Tectónica y magmatismo Ordovícicos en el área de Sanabria, Macizo Ibérico
(Sociedad Geológica de España, 2002)Structural and metamorphic criteria allow us to distinguish two units (Cneissic and Porphyroid) belonging to the Olio de Sapo formation in the Sanabria región. The high-grade gneissic unit and the lower Ordovician metasediments ...
