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Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)

Report on geologic mapping of the Miocene sediments on the map sheet Vracov (34-222) in 1999

 

Zdeněk Novák, Pavla Petrová

Geoscience Research Reports 33, 2000 (GRR for 1999), pages 37–39
Map sheets: Hodonín (34-22)

Full text (PDF, 0.15 MB)

 

Abstract

Sarmatian and Pannonian sediments were studied on the map sheet Vracov. Clays, sands and silts are varicoloured and calcareous. Silts are the most wide-spread type of rocks and they are often similar to loess. Microfauna and macrofauna of the Sarmatian and Pannonian sediments are relatively rich, we have distinguished biozones B, C-D and E (Bzenec Formation in Lower Pannonian). Several layers of Pannonian gravels first of all consist of pebbles of quartz and cherts. Kyjov humodyl seam was reached just in boreholes, during mapping we only observed coal clays.