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Swiss Journal of Geosciences
Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: Marine facies differentiation along complex paleotopography: an example from the Middle Miocene (Serravallian) of Lower Austria

Fig. 6

A Polished core surface of the transgression conglomerate of Triassic dolomite clasts lithified by several cement generations. Some of the components are bored by Entobia igen. (En.), the brownish/reddish coloration stems from pyrite crystals (sample HA 518/16). B Limestone sample immediately above the Triassic basement with bored (Entobia igen., En.) dolomite clasts, coralline algal encrusted clasts and rhodolites and branch fragments of coralline algae (polished core surface, sample HA 540/15)

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