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Pavlovic, G; Zupanic, J; Prohic, E; Tibljas, D
Geologia Croatica, 06/2002, Volume: 55, Issue: 1Journal Article
The following types of calcified deposits characterize Holocene waterfall tufas in the Zrmanja river: mossy deposits, algally laminatedcrusts and algally coated grains. Petrological examination revealed,that abundant organic remains belonging to mosses and algae provide supporting material, over which tufa accretion takes place, leavingwell-defined impressions of the biota. Postgenetic features likemeniscus, isopachous and drusy mosaic calcite spar cementation, aswell as aggradational neomorphism are only rarely present.
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