RT Journal Article
T1 Metamorfismo y geotermobarometría de la Unidad de Yunquera en Casarabonela (Complejo Alpujárride, Málaga)
T1 Metamorphism and geothermobarometry of the Yunquera Unit in Casarabonela (Alpujárride Complex, Málaga)
A1 Esteban, José Julián
A1 Cuevas, Julia
A1 Tubía, José María
A1 Gil Ibarguchi, José Ignacio
AB The rocks of the Yunquera Unit (Alpujárride Complex) record two stages, at least, of recrystallization atdifferent 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. 1200-1300MPa and 560-695 ºC through conventional thermobarometry. The second mineral association wasequilibrated at 600 MPa and 700 ºC. These data support the existence of an initial high-pressuremetamorphic stage followed by a pressure drop and final cooling during the Alpine exhumation of theUnit
PB Sociedad Geológica de España
YR 2004
FD 2004
LK http://hdl.handle.net/10272/8809
UL http://hdl.handle.net/10272/8809
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026