ABSTRACT: 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 “troughâ€ 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.
You are not registered as a current subscriber. If your institution has an active subscription, contact us to ask for help with your computer's IP address. If you have an active personal subscription, log in.
Subscribe to Micropaleontology
|Online only||Added print|