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Accumulative sequences in the Valencia del Ventoso plutonic complex

dc.contributor.authorSarrionandia Eguidazu, Fernando
dc.contributor.authorCarracedo Sánchez, Manuel
dc.contributor.authorEguiluz, Luis
dc.contributor.authorApalategui, Octavio
dc.date.accessioned2014-10-20T08:17:53Z
dc.date.available2014-10-20T08:17:53Z
dc.date.issued2004
dc.identifier.urihttp://hdl.handle.net/10272/8898
dc.description.abstractIn the Valencia del Ventoso plutonic complex it has been detected the basal part of a previous stock formed by cumulates. This accumulative sequence is subdivided in base of textural criteria in five zones, called from the bottom to the upper part Zone I, II, III, IV and V respectively. Textural, modal and mineralogical criteria indicate the existence of at least two chamber recharges. The principal fractionation mechanism that takes place during the early stages is related with continuous convection, but the progressively thermal equilibrium with the host rocks led to crystal settling mechanism. With these two continuous processes, take place eventual processes related with compaction and chamber rechargeen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCumulatesen_US
dc.subject.otherValencia del Ventoso igneous complexen_US
dc.subject.otherOssa-Morena Zoneen_US
dc.subject.otherBadajozen_US
dc.titleSecuencias acumulativas en el Complejo Plutónico de Valencia del Ventosoen_US
dc.titleAccumulative sequences in the Valencia del Ventoso plutonic complexeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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