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Late Eocene to Quaternary deformation and stress field evolution of the Orava region (Western Carpathians)
Structural geology Cenozoic Paleogene Faulting and folding Central Carpathian Palaeogene Basin
2009/10/20
The northern part of theWestern Carpathians suffered polyphase deformation at the boundary between their Central and Outer parts. Palaeostress analysis in the Orava region revealed the existence of fi...