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Geochemical characterization and geodynamic setting of the metabasites from Sierra del Algarrobo (eastern Betic Cordillera)

dc.contributor.authorPuga, Encarnación
dc.contributor.authorRodríguez Martínez Conde, José Ángel
dc.contributor.authorDíaz de Federico, Antonio
dc.contributor.authorManteca Martínez, José Ignacio
dc.contributor.authorDíaz Puga, Miguel Ángel
dc.description.abstractThe metabasites cropping out in the Sierra del Algarrobo have been studied from petrological and geochemical points of view. They consist of gabbros, dolerites and basalts, which were transformed into eclogites or amphibolites during the Alpine metamorphism. Their primary magmas were tholeiitic basalts originated in E-MORB to N-MORB geodynamic conditions. By comparing these metabasites with those of the Betic and Alpine-Apennine Ophiolites and with basalts from current oceanic ridges, we classify them as ophiolitic and tectonically deriving from the oceanic floor of the Jurassic Western Tethysen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherBetic ophiolitesen_US
dc.subject.otherSierra del Algarroboen_US
dc.subject.otherMulhacén Complexen_US
dc.subject.otherNevadofilábride Domainen_US
dc.subject.otherEastern Betic Cordilleraen_US
dc.titleCaracterización geoquímica y ambiente geodinámico de génesis de las metabasitas de la Sierra del Algarrobo (Cordillera Bética oriental)en_US
dc.titleGeochemical characterization and geodynamic setting of the metabasites from Sierra del Algarrobo (eastern Betic Cordillera)eng

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