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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.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.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherAlpujarride Complexen_US
dc.subject.otherYunquera Uniten_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

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