Esteban, José JuliánCuevas, JuliaTubía, José MaríaGil Ibarguchi, José Ignacio2014-09-182014-09-182004http://hdl.handle.net/10272/8809The 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 UnitspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Betic CordilleraAlpujarride ComplexYunquera UnitThermobarometryHigh-pressure metamorphismjournal articleopen access