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Swiss Journal of Geosciences
Fig. 2 | Swiss Journal of Geosciences

Fig. 2

From: Facies architecture, geochemistry and petrogenesis of Middle Triassic volcaniclastic deposits of Mt. Ivanščica (NW Croatia): evidence of bimodal volcanism in the Alpine-Dinaridic transitional zone

Fig. 2

A drone image of the quarry front with sample positions. Different colours represent different facies and pertaining lithotypes. AF—Autoclastic effusive facies presented by the lithotype of autoclastic basalt breccia with flow texture matrix containing clasts of several different basalts. RAF—Resedimented autoclastic facies with two different lithotypes: block to lapilli-sized basalt breccia with epiclasts, and coarse-sized ash lithoclastic tuff. SPF – Secondary pyroclastic facies with three different lithotypes: (1) coarse-sized ash lithoclastic tuff, (2) fine-sized ash cyrstaloclastic tuff and (3) fine-sized ash vitroclastic tuff. General coordinates of the quarry 16˚3′21.42’’ E; 46˚11′41.42’’ N. Graphical scale is indicated in the figure

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