“…It is associated with high-to ultra-high-temperature metamorphism (Barbey et al, 2015;Kunz et al, 2018;Pin & Vielzeuf, 1983) and bimodal magmatism that has affected the whole Franke (2014) for the northern realm of the Variscan belt and Stampfli et al (2013) for the southern realm (Alleghanian belt, Alpine Mediterranean domain, and Paleotethys) with modifications for Corsica, Sardinia, and Maures-Tanneron relative positions by considering recent paleomagnetic syntheses by Edel et al (2014Edel et al ( , 2018. Directions of stretching are represented only for the 310-290 Ma period and were synthesized from (1) Michard et al (2010), (2) review from Martínez Catalán et al ( 2014), (3) Cochelin et al (2017), (4) Corsini and Rolland (2009), (5) Carosi and Palmeri (2002), (6) Casini et al (2012), (7) Choulet et al (2012), (8) Ledru et al (2001), (9) Echtler and Malavieille (1990), (10) Faure et al (1990), (11) Faure et al (2009), (12) Genna et al (1998) and Rolin and Colchen (2001), (13) review from Gapais et al (2015), ( 14) Saspiturry et al (2019), (15) Carreras and Debat (1996), ( 16) de Saint Blanquat (1993), (17) Díez Fernández et al (2012, (18) Escuder Viruete et al (19) Hernández Enrile (1991). Abbreviations: CZ, Cantabrian Zone; CIZ, Central Iberian Zone; FMC, French Massif Central; AM, Armorican Massif; BM, Bohemian Massif; MN, Montagne Noire; MT, Maures-Tanneron; CS, Corsica-Sardinia.…”