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Metamorphism and geothermobarometry of the Yunquera Unit in Casarabonela (Alpujárride Complex, Málaga)

dc.contributor.authorEsteban, José Julián
dc.contributor.authorCuevas, Julia
dc.contributor.authorTubía, José María
dc.contributor.authorGil Ibarguchi, José Ignacio
dc.date.accessioned2014-09-18T08:58:06Z
dc.date.available2014-09-18T08:58:06Z
dc.date.issued2004
dc.identifier.urihttp://hdl.handle.net/10272/8809
dc.description.abstractThe rocks of the Yunquera Unit (Alpujárride Complex) record two stages, at least, of recrystallization at different P-T conditions defined by the mineral associations: a) Grt + Pl + Ms + St + Ky + Qtz, and b) Grt + Pl + Sill + Qtz ± Bt. The metamorphic peak for the first stage has been estimated at ca. 1200-1300 MPa and 560-695 ºC through conventional thermobarometry. The second mineral association was equilibrated at 600 MPa and 700 ºC. These data support the existence of an initial high-pressure metamorphic stage followed by a pressure drop and final cooling during the Alpine exhumation of the Uniten_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.otherBetic Cordilleraen_US
dc.subject.otherAlpujarride Complexen_US
dc.subject.otherYunquera Uniten_US
dc.subject.otherThermobarometryen_US
dc.subject.otherHigh-pressure metamorphismen_US
dc.titleMetamorfismo y geotermobarometría de la Unidad de Yunquera en Casarabonela (Complejo Alpujárride, Málaga)en_US
dc.titleMetamorphism and geothermobarometry of the Yunquera Unit in Casarabonela (Alpujárride Complex, Málaga)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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