Early Eocene age of a sandstone from the Buntmergel Formation (Gresten Klippen Zone, Lower Austria)

Authors

  • M. Adam Gasiński Jagiellonian University Cracow
  • Volker Hoeck Paris Lodron University Salzburg
  • Andrzej Ślączka Jagiellonian University Cracow
  • Corina Ionescu Babes-Bolyai University Cluj-Napoca

DOI:

https://doi.org/10.7306/gq.1063

Keywords:

Gresten Klippen Zone, Eocene, planktonic foraminiferids, Lower Austria

Abstract

The Gresten Klippen Zone is an individual geological unit, mainly outcropping at the northern rim of the Northern Calcareous Alps. It is best exposed between the Enns Valley in the west and the Vienna Forest in the east. It contains a rock sequence ranging from Early Jurassic to Early Cretaceous, including sandstones, various limestones, breccias and radiolarites. The late Early Cretaceous–Paleogene is represented by the Buntmergel Formation. A sandstone block from the latter yields well-preserved planktonic foraminiferids which allow an assignment to the Early Eocene (E-7 Zone). The low density currents which deposited the parallel laminated sandstones originated in the lower shelf-middle slope. 

Author Biographies

M. Adam Gasiński, Jagiellonian University Cracow

Univ.Prof.Dr.Institute of Geological Sciences

Volker Hoeck, Paris Lodron University Salzburg

Univ.Prof.Dr.Department of Geography and Geology

Andrzej Ślączka, Jagiellonian University Cracow

Univ.Prof.Dr.Institute of Geological Sciences

Corina Ionescu, Babes-Bolyai University Cluj-Napoca

Univ.Prof.Dr.Department of Geology

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Published

2012-12-10

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Articles