“…This continent-arc collision conditioned the different orientations of the fault trends during the Mid Ordovician-Early Devonian times (von Gosen et al, 2002;Astini and Dávila, 2004). Furthermore, this collision produced the current exposures of the Famatinian deep paleo-arc that show a continuous deepening from north to south (Otamendi et al, 2010;Tibaldi et al, 2013;Cristofolini et al, 2014) and from east to west (Camilletti et al, 2020). During the Famatinian belt construction, the deformation was regionally resolved in different ways; through large scale fold and thrust belts in the upper crust (Astini and Dávila, 2004), along major shear zones in the front and margins of the Famatinian paleo-arc (von Gosen and Prozzi, , 2005Höckenreiner et al, 2003;Cristofolini et al, 2014;Mulcahy et al, 2014), through large-scale west-verging shear zones located in the Pampean basement (Sims et al, 1997;Martino, 2003;Cristofolini et al, 2017;Semenov et al, 2019), and double-vergent structures developed in the paleo-backarc (Larrovere et al, 2017;Christiansen et al, 2019).…”