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It implies that extensional collapse of the Alpine orogene in\nthe Middle Miocene was controlled by listric normal faults, which\nusually crosscut Alpine nappes at shallow levels, but at depth merge\nwith overthrust planes separating the different Alpine units. The\nalternative structural model was tested along a transect across the\nDanube basin by gravity model calculations, and the results show that\nthe model of low-angle extensional faulting is indeed viable. Regarding\nthe whole lithosphere of the western Pannonian basin, gravity modelling\nindicates a remarkable asymmetry in the thickness minima of the\nattenuated crust and upper mantle. 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