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Thermobarometry in the gneis of the Bentomiz extensional unit, Alpujarride Complex (central Betics)

dc.contributor.authorAlonso Chaves, Francisco Manuel 
dc.contributor.authorPascual Martínez, Emilio 
dc.contributor.authorOrozco, Miguel
dc.date.accessioned2017-06-12T10:49:49Z
dc.date.available2017-06-12T10:49:49Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/13800
dc.description.abstractIn the gneis of the Bentomiz extensional unit (Sierra Tejeda area), the alpine metamorphic evolution was studied. These rocks show high pressure-high temperature (HP/HT) assemblages. An extensional deformation before Neogene has been recognized in the Aipujarride Complex.en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherThermobarometryen_US
dc.subject.otherExtensional deformationen_US
dc.subject.otherBeticsen_US
dc.titleTermobarometría en los gneises de la unidad extensional de Bentomiz, Complejo Alpujárride (Béticas centrales)en_US
dc.titleThermobarometry in the gneis of the Bentomiz extensional unit, Alpujarride Complex (central Betics)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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