Fig. 10

a Map illustrating the distribution of Cretaceous metamorphism in the ALCAPA, Tisza and Dacia mega-units (modified from Schmid et al. 2008; compare Fig. 1). Information on the timing and degree of metamorphism is based on Antić et al. (2016); Árkai et al. (2000); Balen et al. (2013, 2017); Ciulavu et al. (2008); Culshaw et al. (2012); Dallmeyer et al. (1996, 1999); Froitzheim et al. (2008); Gröger et al. (2013); Hoinkes et al. (1999); Iancu et al. (2005); Janák et al. (2004, 2015); Jeřábek et al. (2012); Kalmár (1996); Koroknai et al. (2001); Kounov et al. (2010); Lelkes-Felvári et al. (1996); Lelkes-Felvári et al. (2003); Schuster et al. (2004); Soroiu et al. (1985); Strutinski et al. (2006); van Gelder et al. (2015); Vojtko et al. (2016, 2017); Zincenco et al. (1990) and the results from this study. b Sketch of the situation along the European continental margin during pre-Miocene times. Rotational movements are indicated based on palaeomagnetic data and palaeogeographic reconstructions (Pătraşcu et al. 1994; Márton 2000; Márton and Fodor 2003; Márton et al. 2007;  Ustaszewski et al. 2008; Lorinczi and Houseman 2010)