Fig. 6

Summary of fissure monazite ages from this study compared to published crystallization and cooling ages.[1] Bergemann et al. (2019); Gasquet et al. (2010); Grand’Homme et al. (2016a); [2] Grand’Homme et al. (2016a); [3] Gasquet et al. (2010); Leutwein et al. (1970); Marshall et al. (1998); Rossi and Rolland (2014); [4] Gasquet (1979); [5] Agard et al. (2002); Bellanger et al. (2015); Corsini et al. (2004); Crespo-Blanc et al. (1995); Kirschner et al. (2003); Lanari et al. (2014); Rolland et al. (2008); Sanchez et al. (2011a); Simon-Labric et al. (2009); Strzerzynski et al. (2012); Villa et al. (2014); [6] Freeman et al. (1997, 1998); [7] Cenki-Tok et al. (2014); [8] Beucher (2009); Beucher et al. (2012); Bigot-Cormier et al. (2006); Bogdanoff et al. (2000); Fügenschuh et al. (1999); Fügenschuh and Schmid (2003); Lelarge (1993); Leloup et al. (2005); Malusà et al. (2005); Sabil (1995); Sanchez et al. (2011b); S. Schwartz et al. (2007); Seward and Mancktelow (1994); Seward et al. (1999); Soom 1990; Tricart et al. (2007); van der Beek et al. (2010); [9] Beucher (2009); Bigot-Cormier et al. (2006); Carpéna (1992); Crouzet et al. (2001); Fügenschuh and Schmid (2003); Glotzbach et al. (2011); Malusà and Vezzoli (2006); Schwartz et al. (2007); Schwartz (2000); Seward and Mancktelow (1994); Soom (1990); van der Beek et al. (2010); Vance (1999); [10] Sanchez et al. (2011b). AFT: apatite fission track, ZFT: zircon fission track, N: north, S: south. Square brackets to the left delimit the main periods of monazite growth discussed in the text: (1) Top-NNW thrusting, (2) Top-WNW thrusting, (3) Top-SW thrusting and orogen parallel deformation