Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example

Special Issue Orogen lifecycle: learnings and perspectives from Pyrenees, Western Mediterranean and analogues

Open Access

Fig. 5

P-T-time evolution of the Alpujárride complex. A: P-T paths of the different units of the Alpujárride complex (Tubía and Gil Ibarguchi, 1991; Azañón et al., 1992, 1998; Goffé et al., 1994; Balanyá et al., 1997; Soto and Platt, 1999; Azañón and Crespo-Blanc, 2000; Booth-Rea et al., 2005; Chalouan et al., 2008; Massonne, 2014) and some age constraints after Platt and Whitehouse (1999) and Bessière (2019). B: P-T-time constraints from the Ronda and Beni Bousera peridotites and neighboring high-temperature crustal units (Sánchez-Rodríguez and Gebauer, 2000; Pearson and Nowell, 2004; Précigout et al., 2013; Acosta-Vigil et al., 2014; Barich et al., 2014; Massonne, 2014; Barich, 2016; Rossetti et al., 2020).

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