Fig. 6From: 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 N-MORB-normalised multielement and B REE patterns for the basaltic volcaniclastics and rhyodacite tuff from Mt. Ivanščica. Normalisation values are from Sun and McDonough (1989). Fields for Active continental margin-Continental arc calc-alkaline basaltic andesites in the Andes (Wilson, 1989, page 215) are plotted for comparisonBack to article page