Titlebook: Orogenic Processes in the Alpine Collision Zone; Selected Contributio Nikolaus Froitzheim,Stefan M. Schmid Conference proceedings 2009 Birk

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Foreland and Hinterland basins: what controls their evolution?,of tectonic contraction or post-orogenic collapse, thermo-mechanical processes in the deep lithosphere and asthenosphere, but also by climate and other surface processes in fluencing erosion rates..Different types of sedimentary basins can develop in close association with orogens, either in the for

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Provenance of the Bosnian Flysch,of Upper Jurassic to Cretaceous mixed carbonate and siliciclastic sediments in the Dinarides. New petrographic, heavy mineral, zircon U/Pb and fission-track data as well as biostratigraphic evidence allow us to reconstruct the palaeogeology of the source areas of the Bosnian Fysch basin in late Meso

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From subduction to collision: thermal overprint of HP/LT meta-sediments in the north-eastern Lepontl to the orogen and was later truncated by two thermal domes characterised by Barrow-type metamorphism (Lepontine dome and Tauern window). This study documents for the first time that relics of Fe-Mg carpholite occur also within meta-sedimentary units that are part of the north-eastern Lepontine str

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