Fig. 5From: Facies architecture, geochemistry and petrogenesis of Middle Triassic volcaniclastic deposits of Mt. Ivanščica (NW Croatia): evidence of bimodal volcanism in the Alpine-Dinaridic transitional zoneA Nb/Y – Zr/TiO2*10–4 classification diagram (Winchester & Floyd, 1977) and B Ce/Yb – Ta/Yb discrimination diagram after Pearce (1982) for the basaltic volcaniclastics and rhyodacite tuff from Mt. IvanščicaBack to article page