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Changing patterns of shortening and lateral extension, Exhumation of the Eastern Alpine orogenic core, Strain partitioning during orogenic indentation

Subject Area Palaeontology
Term from 2009 to 2015
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 150447119
 
Final Report Year 2017

Final Report Abstract

Our study reveals that Alpine-type collisional belts grow in three continuous stages: (1) subduction of continental lithosphere leading to stacking of the ocean-continent transition onto distal parts of the downgoing continental margin; (2) nappe stacking and duplex thrusting of proximal members of the downgoing continental margin; (3) indentation of the entire nappe stack by crustal wedges at the leading edge of the upper plate. However our studies also show that lateral orogenic escape in the Eastern Alps is not typical of the rest of the Alps, or of most mountain belts, due to a switch in subduction polarity in Miocene time. This switch involved fragmentation of the indenting Adriatic crust and intracrustal decoupling in the new (European) upper plate; the combination of these events focussed folding and extensional exhumation in the Tauern area. The 4D kinematic view (3D-structure back in time) afforded by this project provides a valuable starting point for advanced seismological and tectonic studies that form the German component of the European AlpArray Project.

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