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The Osning Thrust is one of the major fault systems in Central Europe, with a length of approximately 115 km. It underwent a polyphase tectonic evolution in the Mesozoic that ranged from extensional movements in the Jurassic to reverse faulting and thrusting during inversion in the Late Cretaceous. A series of complex metre-scale faults and related fold structures are developed within the Upper Pleistocene...
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