Vol 7, (1976)

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Category: Vol 7, (1976)

• Pennsylvanian
• geology
• Czech
• Carboniferous and Permian deposits
• PALAEOGEOGRAPHY

Authors: Václav Havlena

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 Abstract: In the Lower Carboniferous time two Palaeozoic geosynclines are believed to trench on the territory of Czechoslovakia. The Upper Carboniferous and Permian deposits of Czechoslovakia are classified with regard to the evolutionary pattern of a geosyncline established by Aubouin (1965). The Bruno-Vistulikum platform is delineated which played the role of Aubouin's intermediate foreland during the times concerned. The marine Carboniferous and Permian deposits of the Spiš-Gemer Mountains appear to be laid down in a special molasse intra-deep. The Verrucano basins of the West Carpathians are regarded as limnic basins of the Upper Permian time-interval.