“…Regional paleogeographic models, stratigraphic considerations or scarce geochemical data have been commonly used to propose two different tectonic environments: (1) a continental volcanic arc related with the Pacific subduction (Boschman, et al, 2014;Bustamante et al, 2010;McCourt et al, 1984;Meschede and Frisch, 1998;Pindell and Tabbutt, 1995;Pindell and Erikson, 1993;Spikings et al, 2014;Toussaint, 1995), (2) an intracontinental extensional rifting that can be associated to the breakup of Pangea in the Triassic and Early Jurassic (Cediel et al, 2003;Cochrane et al, 2014;Pindell and Dewey, 1982;Ross and Scotese, 1988).…”