Fig. 3
From: Provenance of Cretaceous synorogenic sediments from the NW Dinarides (Croatia)
Chronostratigraphic and lithostratigraphic logs of the studied clastic formations and their basement (Babić et al. 2002; Lužar-Oberiter et al. 2009, and references therein). Note scale change at 150 Ma. Pie charts illustrate the average compositions of heavy mineral assemblages in the sandstones of each investigated formation (Crnjaković 1981, 1987, 1989; Zupanič 1981; Zupanič et al. 1981)