Title: The tectonic deformation of Quaternary deposits within the Kleszczów Graben, central Poland
Abstract: Three, well recognizable structural stages can be observed within the Kleszczów Graben (Central Poland). They are divided by angular discordances. The Valachian stage consists of strongly folded and faulted deposits of Miocene age. The Belchatów stage consists both of Pliocene and Quaternary deposits. The last stage dates back to the beginning of the Drenthe-Warthe interglacial. The tectonic origin or Quaternary deformation (folding) of the Belchatovian age seems rather unquestionable. In the uppermost structural stage only some glaciotectonic deformations can be observed.
Publication Year: 1989
Publication Date: 1989-07-01
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 8
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