Primera descripción de capas de esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)

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dc.contributor.authorTubía, José María
dc.contributor.authorCuevas, Julia
dc.contributor.authorEsteban, José Julián
dc.date.accessioned2014-10-17T12:12:45Z
dc.date.available2014-10-17T12:12:45Z
dc.date.issued2004
dc.description.abstractThis work reports the finding of layers of zircon-bearing chlorite schists in the southwestern part of the Sierra Bermeja peridotites, the biggest massif of the Ronda peridotites (Alpujarride Complex, Betic Cordillera, southern Spain). Structural, petrographic and geochemical data support a metasomatic origin for these rocks, at temperature conditions of 280-350 ºC, related to the serpentinization of the peridotites and the rodingitization of the granite dykes of the Ronda peridotitesen_US
dc.identifier.urihttp://hdl.handle.net/10272/8890
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherZr-bearing chlorite schisten_US
dc.subject.otherSerpentinizationen_US
dc.subject.otherRodingitizationen_US
dc.subject.otherRonda peridotitesen_US
dc.titlePrimera descripción de capas de esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)en_US
dc.titleFirst report of zircon-bearing chlorite schists in the Ronda peridotites (Betic Cordilleras)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 37, (2004)