Rodingitización y formación de pectolita en diques graníticos de las Peridotitas de Ronda (Cordilleras Béticas, España)

dc.contributor.authorEsteban, José Julián
dc.contributor.authorCuevas, Julia
dc.contributor.authorTubía, José María
dc.contributor.authorYusta, Iñaki
dc.date.accessioned2015-01-27T12:14:28Z
dc.date.available2015-01-27T12:14:28Z
dc.date.issued2001
dc.description.abstractThis work reports the local occurrence of rodingites formed from granitic dykes intrusive in the Ronda Peridotites. Representative mineral assemblages include chlorite, hydrogrossular, and prehnite but also pectolite, and xonotlite uncommon mineral in rodingites. In addition, some granitic dykes are characterized by the albitization of plagioclases. The development oflizardite in the adjacent serpentinites suggests that rodingitization was a low-temperature metasomatic process, which affects the granitic dykes in contact with peridotites during serpentinizationen_US
dc.identifier.urihttp://hdl.handle.net/10272/9725
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.otherRodingiteen_US
dc.subject.otherPectoliteen_US
dc.subject.otherRonda peridotitesen_US
dc.subject.otherBetic Cordillerasen_US
dc.titleRodingitización y formación de pectolita en diques graníticos de las Peridotitas de Ronda (Cordilleras Béticas, España)en_US
dc.titleRodingitization and pectolite development in granitic dykes from the Ronda peridotites (Betic Cordilleras, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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