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Succession of felsic volcanic sequences in the Volcano-Sedimentary Complex in the Iberian Pyrite Belt: discrimination between volcanic and subvolcanic models

dc.contributor.authorDonaire Romero, Teodosio 
dc.contributor.authorPascual Martínez, Emilio 
dc.contributor.authorValenzuela Aznar, Alfonso
dc.contributor.authorGonzález Roldán, Manuel Jesús
dc.contributor.authorToscano Macías, Manuel 
dc.date.accessioned2014-07-28T09:47:34Z
dc.date.available2014-07-28T09:47:34Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8635
dc.description.abstractA field study is presented on two selected areas in the Volcano-Sedimentary Complex (VSC) of the Iberian Pyrite Belt (IPB), the Odiel River section and the Paymogo Volcanic lineament. Field evidence has allowed to distinguish two major groups of felsic rocks, which successively appear in the stratigraphic column. Probably, this conclusion can be extended to other areas in the IPB. In addition, field, petrographic and geochemical evidence shows that at least the felsic rhyolitic succession in the Odiel River (and probably also in Paymogo) formed in a volcanic, environment, favouring a volcanic-pile model in the VSCen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Españaen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherIberian Pyrite Belten_US
dc.subject.otherDaciteen_US
dc.subject.otherRhyoliteen_US
dc.subject.otherPeperiteen_US
dc.subject.otherVolcaniclastic depositsen_US
dc.titleSucesión de secuencias volcánicas félsicas en el Complejo Vulcanosedimentario de la Faja Pirítica Ibérica: discriminación entre modelos volcánicos y subvolcánicosen_US
dc.titleSuccession of felsic volcanic sequences in the Volcano-Sedimentary Complex in the Iberian Pyrite Belt: discrimination between volcanic and subvolcanic modelseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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