Caracterización químico-mineralógica de las cromitas ofiolíticas de Calzadilla de los Barros (Badajoz)

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dc.contributor.authorMartos, Rubén
dc.contributor.authorOrtega, Lorena
dc.contributor.authorGervilla, Fernando
dc.contributor.authorPiña, Rubén
dc.contributor.authorMonterrubio, Serafín
dc.contributor.authorLunar Hernández, Rosario
dc.contributor.authorAlbert, Helena
dc.date.accessioned2014-03-10T13:58:16Z
dc.date.available2014-03-10T13:58:16Z
dc.date.issued2010
dc.description.abstractThe Cerro Cabrera and Sierra Cabeza Corda peridotite massifs (Calzadilla de los Barros, Badajoz) comprise serpentinites hosting podiform chromite mineralization and have been interpreted as part of an ophiolitic slab. The chromites are Al-rich and cristallized from a MORB-type melt. The subsolidus reequilibration with olivine depleted the chromite margins in Al and Mg. Later metamorphic alteration produced a enrichment in Te3+, resulting in the formation offerrichromiteen_US
dc.identifier.urihttp://hdl.handle.net/10272/7840
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherChromiteen_US
dc.subject.otherPodiform,en_US
dc.subject.otherOphioliteen_US
dc.subject.otherDuniteen_US
dc.subject.otherHarzburgiteen_US
dc.titleCaracterización químico-mineralógica de las cromitas ofiolíticas de Calzadilla de los Barros (Badajoz)en_US
dc.titleCompositional features ofophiolitic chromites from Calzadilla de los Barros (Badajoz)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 48, (2010)