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Lower Miocene structural evolution of the central Vienna Basin (Austria)
Authors:Monika Hölzel  Kurt Decker  András Zámolyi  Philipp Strauss  Michael Wagreich
Institution:1. Department of Geodynamics and Sedimentology, University of Vienna, Centre of Earth Sciences, Althanstr. 14, 1090 Vienna, Austria;2. OMV Exploration & Production GmbH, Trabrennstr. 6-8., 1020 Vienna, Austria;3. Department of Geophysics and Space Sciences, Eötvös University, Budapest, Hungary
Abstract:The tectonic evolution of the Vienna Basin overlying the Alpine-Carpathian fold and thrust belt includes two stages of distinct basin subsidence and deformation. The earlier phase contemporaneous with thrusting of the Alpine-Carpathian floor thrust is related to the formation of a wedge-top basin (“piggy-back”), which was connected to the evolving foreland basin (Lower Miocene; c. 18.5–16 Ma). This stage is followed by the formation of a pull-apart basin (Middle to Upper Miocene; c. 16–8 Ma). Sediments of the latter unconformably overly wedge-top basin strata and protected them against erosion.
Keywords:Wedge-top  Piggy-back  Vienna Basin  Miocene  Fault propagation folds  Strike-slip
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