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pro vyhledávání: '"Faciès rhodolitiques"'
Autor:
M. Gonera
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
The Neogene in Central Paratethys was the period when flysch deposition was replaced by that of molasse in both the Carpathian foldbelt and its foredeep. The sedimentation processes were coeval, closely relevant with tectonic phases of the Carpathian