Micropaleontology; Fall 2006; v. 52; no. 3;
p. 281-286; DOI: 10.2113/gsmicropal.52.3.281
© 2006 Micropaleontology Project
The age of the Tilovica breccias in Central Dalmatia, Croatia
Vlasta Cosovic,
Vlasta Premec Fuèek,
Ivan Gu
ic,
Vladimir Jelaska and
Alan Moro
Department of Geology and Paleontology, Faculty of Science, University of Zagreb, Horvatovac 102 A, 10000 Zagreb, Croatia, email: Vlasta1501{at}yahoo.com, INA Industrija nafte, d.d. Research and Laboratory Testing Department, Lovinèiceva bb, 10000 Zagreb, Croatia
The recently discovered Tilovica breccias in Central Dalmatia are of submarine origin and assigned to a Paleocene age by means of smaller benthic and planktonic foraminifera found either in pelagic interbeds or in the matrix. The breccias define a "trough" produced by Cretaceous tectonics and submerged by the global sea-level rise. This provides a new insight into the evolution of the External Dinarides (Croatia) and suggests a new paleogeographic interpretation of the region.
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