Fig. 2

Available geochronological data for the intrusive rocks from the Jurassic ophiolites of the Alpine-Apennine belt. Data sources: 1, Rossi et al. (2002); 2, Li et al. (2015); 3, Tribuzio et al. (2016); 4, Bortolotti et al. (1995); 5, Rubatto and Scambelluri (2003); 6, Bill et al. (1997); 7, Rubatto et al. (1998); 8, Liati et al. (2005); 9, Rubatto et al. (2008); 10, Kaczmarek et al. (2008); 11, Li et al. (2013); 12, Rubatto and Hermann (2003); 13, Lombardo et al. (2002); 14, Schaltegger et al. (2002); 15, Stucki et al. (2003). Methods used: (a), U–Pb zircon age; (b), ⁴⁰Ar/³⁹Ar amphibole plateau age; (c), U–Pb baddeleyite age. U–Pb zircon ages acquired by conventional isotope dilution TIMS for felsic rocks by Ohnenstetter et al. (1981), Borsi et al. (1996) and Costa and Caby (2001) are not reported