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Preliminary report on the finding of diaspore related to the serpentinization of the Ronda peridotites

dc.contributor.authorEsteban, José Julián
dc.contributor.authorCuevas, Julia
dc.contributor.authorTubía, José María
dc.contributor.authorVegas, Néstor
dc.contributor.authorYusta, Iñaki
dc.date.accessioned2014-05-16T08:27:06Z
dc.date.available2014-05-16T08:27:06Z
dc.date.issued2009
dc.identifier.urihttp://hdl.handle.net/10272/8126
dc.description.abstractWe report the presence of large aggregates (diameter > 1 cm) of diaspore related to the serpentinization of the Sierra Alpujata massif of the Ronda peridotites (Betic Cordilleras, southern Spain). The diaspore is found in two different but related settings: in narrow metasomatic rims pervading the peridotites from steeply dipping tension joints and in the blackwall zone developed along the normal fault that separates the peridotites from the overlying metamorphic cover. The systematic association of diaspore with chlorite points to very low temperature conditions (T < 100 ºC) for diaspore formationen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherDiasporeen_US
dc.subject.otherChloritic blackwallen_US
dc.subject.otherSierra Alpujataen_US
dc.subject.otherRonda peridotitesen_US
dc.titleReseña preliminar sobre el hallazgo de diáspora asociada a la serpentinización de los macizos de peridotitas de Rondaen_US
dc.titlePreliminary report on the finding of diaspore related to the serpentinization of the Ronda peridotiteseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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