“…The geodynamic evolution of the TMVB is very complex due to their significant differences in geochemical, isotopic, and geochronological composition of the volcanic rocks, as well as tectonic setting. Several kinds of models (subduction‐related, plume‐related, continental rifting, and strike‐slip faulting) have been proposed by several researchers for the origin and evolution of the TMVB (Díaz‐Bravo, Gómez‐Tuena, Ortega‐Obregón, & Pérez‐Arvizu, 2014; Frey et al, 2014; Gómez‐Tuena, Langmuir, Goldstein, Straub, & Ortega‐Gutiérrez, 2007; Petrone, Orozco‐Esquivel, & Ferrari, 2014; Verma & Nelson, 1989; Verma et al, 2016) and an extensional tectonic regime is developed in the triple rift system known as Tepic‐Zacoalco Rift, Colima Rift and Chapala Rift (TZR‐CR‐ChR; Frey, Lange, Hall, Delgado‐Granados, & Carmichael, 2007; Luhr, Nelson, Allan, & Carmichael, 1985).…”