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The Tatric-Fatric-Veporic convergence zone of the Central Western Carpathians involved a basinal area that originated by Lower Jurassic rifting of Variscan continental crust. In mid-Cretaceous times shortening affected first the southern, Veporic margin of the basin, which was converted to the toe of the orogenic wedge prograding from the hinterland. A system of ductile basement/cover large-scale...
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