Online: 26 December 2014
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The Arenig/Llanvirn boundary (Ordovician) in the Prague Basin (Bohemia)
Journal of the Czech Geological Society, volume 38 (1993), issue 3-4, 189 - 192
Abstract
Relations within the Klabava/Šárka Formations boundary interval at the Drahouš locality near Rokycany are described. In the lower part of the Šárka Formation, there is one biozone (Corymbograptus retroflexus Biozone) and Bouček’s (1973) horizons are of a local character. The Arenig/Llanvirn boundary is situated above the Klabava/Šárka Formations boundary, because the first appearance of Didymograptus spinulosus Perner is within the Corymbograptus retroflexus Biozone.
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Journal of Geosciences, Published by © Czech Geological Society, with support from the Czech Geological Survey.
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ISSN: 1803-1943 (online), 1802-6222 (print)
email: jgeosci(at)jgeosci.org
Webdesign inspired by aTeo. Hosted at the server of the Institute of Petrology and Structural Geology, Charles University, Prague.
ISSN: 1803-1943 (online), 1802-6222 (print)
email: jgeosci(at)jgeosci.org
IF (WoS, 2022): 1.4
5 YEAR IF (WoS, 2022): 1.8
Policy: Open Access
ISSN: 1802-6222
E-ISSN: 1803-1943