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Abstract

Paleogene sedimentary basins which are characteristic for the Internides of the Western Carpathians were formed in the period from Senonian to Oligocene, i.e. after overthrusting of superficial Mesozoic nappes.

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/content/papers/10.3997/2214-4609.201409117
1996-06-04
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409117
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