Thesis Collection
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Browsing by Author "Bandrés, A."
Now showing items 1-4 of 4
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El complejo ígneo de Valle de La Serena: características y significado geodinàmico
(Sociedad Geológica de España, 1998)The Valle de la Serena igneous outcrops are situated in the Obejo-Valsequillo-Puebla de la Reina domain of the northern Ossa-Morena zone (OMZ, Iberian Massif). This sector is considered to correspond to the contact area ... -
El granito Precambrico deValsequillo (zona de Ossa-Morena, Macizo Iberico, España)
(Sociedad Geológica de España, 1999)The Valsequillo granite is situated in the Peraleda de Zaucejo antiform (Obejo-Valsequillo-Puebla de la Reina Domain) at the northern Ossa-Morena Zone. This antiform is defined by Armorican Quartzite and Devonian rocks. ... -
El Macizo de Mérida, un arco volcánico cadomiense reactivado en el hercínico
(Sociedad Geológica de España, 1998)The Merida igneous outcrops are situated in the Obejo-Valsequillo-Puebla de la Reina Domain (DOVPR) of the northern Ossa-Morena Zone (Iberian Massif). This massif is composed by plutonic and volcanic rocks. These rocks are ... -
Litoestratigrafía de la formación El Hoyo (zona de Ossa-Morena, Macizo Ibérico, España)
(Sociedad Geológica de España, 1999)The El Hoyo Formation js located at the boundary: between the Obejo-Valsequil/o-Puebla de la Reina Domain and the Badajo/.-Córdoba Shear Belt. This serie is composed by quartz-schists and mica-schists, finé grained quartzites, ...
