Fig. 13From: Facies architecture, geochemistry and petrogenesis of Middle Triassic volcaniclastic deposits of Mt. Ivanščica (NW Croatia): evidence of bimodal volcanism in the Alpine-Dinaridic transitional zoneSchematic geodynamic model (scale is approximate) for ensialic infant arc – back-arc rifting in the central part of the Mediterranean region according to van Hinsbergen et al. (2020) palaeogeographic reconstruction. CAB calc-alkaline and shoshonitic basalts/volcaniclastites, AB alkaline basalts, OIB ocean island basalts, NCTRB Northwestern Croatian Triassic Rift BasinBack to article page