Attempt to Dating of Accretion in the West Carpathian Flysch Belt: Apatite Fission Track Thermochronology of Tuff Layers From: Geolines | Date: January 1, 2006| Author: Dunkl, Istvà Eynatten, Hilmar von; Rauch-Wlodarska, Marta; ¡ Botor, Dariusz; n | Copyright Institute of Geology 2006. Provided by ProQuest LLC.Copyright information

The Carpathians are a part of the European Alpine chain created by convergence and collision of the European and African plates (Golonka et al. 2000). The Outer Western Carpathians are a north-verging fold-and-thrust belt composed largely of Lower Cretaceous to Lower Miocene flysch sediments arranged into stacked complex of several nappes (from top to bottom: Magura, Dukla and Fore-Magura, Silesian, Sub-Silesian and Skole nappes. The tectonic evolution of the Outer Carpathians is subdivided i...

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