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Rudists and Larger Foraminifera below the Cretaceous-Tertiary Boundary in the Dolenja Vas Section

  • Mario Pleničar
  • Katica Drobne
  • Bojan Ogorelec
Part of the Österreichische Akademie der Wissenschaften Schriftenreihe der Erdwissenschaftlichen Kommissionen book series (ERDWISSENSCHAFT, volume 9)

Summary

The Vreme beds are part of the Liburnian Formation. At Dolenja vas which is situated on the Trieste-Komen platform, the Upper Maastrichtian age has been proved with co-occurring rudistids and foraminifera.

Keywords

Carbonate Platform Micritic Limestone Large Foraminifera Tidal Deposit Lower Valve 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Österreichische Akademie der Wissenschaften 1992

Authors and Affiliations

  • Mario Pleničar
    • 1
  • Katica Drobne
    • 2
  • Bojan Ogorelec
    • 3
  1. 1.Katedra za geologijo in paleontologijo FNTLjubljanaSlovenia
  2. 2.Paleontološki inštitut I. Rakovca ZRC SAZUSlovenia
  3. 3.Geološki zavod Ljubljana. DimičevaSlovenia

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