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The Valsequillo precambrian (Ossa-Morena zone, Iberian Massif, Spain)

dc.contributor.authorBandrés, A.
dc.contributor.authorEguiluz, Luis
dc.contributor.authorApraiz, A.
dc.description.abstractThe 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. Beneath this rocks there are arkosic conglomerates from Tremadoc. Tremadoc rocks are discordant, over Malcocinado poligenics conglomerates. Malcocinado conglomerates containt decimetric pebbes of Valsequillo granite and dioritoids. The Valsequillo granite is a subvolcanic igneous bodie intruded into dioritoids and pelitic series and contact metamorphisme generates. A brittle trhust overline dioritoids and Valsequillo granite over devonian rocks with a transcurrent senestral componenten_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherIberian Massifen_US
dc.subject.otherOssa-morena Zoneen_US
dc.subject.otherMalcocinado comglomeratesen_US
dc.titleEl granito Precambrico deValsequillo (zona de Ossa-Morena, Macizo Iberico, España)en_US
dc.titleThe Valsequillo precambrian (Ossa-Morena zone, Iberian Massif, Spain)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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