0322508 - GLÚ 2009 DE eng A - Abstract
Suttner, T. J. - Berkyová, S. - Hubmann, B. - Koptíková, Leona - Frýda, J. - Hladil, Jindřich
The Basal Chotec Event in neritic sequences of the Prague Basin and the Graz Palaeozoic compared.
[Porovnání bazálního chotečskeho eventu v mělkovodních sekvencích pražské pánve a paleozoika Grazu.]
From Gondwana and Laurussia to Pangea: Dynamics of Oceans and Supercontinents. 20th International Senckenberg-Conference and 2nd Geinitz-Conference. Final Meeting of IGCP 497 and IGCP 499 : abstracts and programme. Frankfurt ; Dresden: Senckenberg Forschungsinstitut und Naturmuseum ; Staatliche naturhistorische Sammlungen Dresden Museum für Mineralogie und Geologie, 2008 - (Königshof, P.; Linnemann, U.). s. 232-234. ISBN 978-3-910006-39-3.
[From Gondwana and Laurussia to Pangea: Dynamics of Oceans and Supercontinents ; International Senckenberg-Conference /20./ ; Geinitz- Conference /2./. 30.09.2008-03.10.2008, Frankfurt am Main]
R&D Projects: GA AV ČR KJB307020602
Institutional research plan: CEZ:AV0Z30130516
Keywords : Basal Chotec Event * Prague Basin * Graz Palaeozoic
Subject RIV: DB - Geology ; Mineralogy

Shallow marine deposits of the Prague Basin and the Graz Palaeozoic were evaluated to trace the Basal Chotec Event close to the Emsian/Eifelian boundary. This event, recognized and typified within the pelagic sequence of the Prague Basin is the first of three globally documented Middle Devonian events. Two sections are compared regarding fossil content, sedimentary conditions, and geochemical composition spanning critical interval: Cerveny Quarry in Prague Basin and Forstweg Attems in Graz Palaeozoic. This critical interval is represented by the boundary between Suchomasty and Acanthopyge limestone members (Daleje-Trebotov and Chotec formations) in Prague Basin, and, similarly, between Flosserkogel and Plabutsch formations in Graz Palaeozoic.
Permanent Link: http://hdl.handle.net/11104/0170739