The Vienna Basin formations are a series of sedimentary layers that were deposited in the Neogene . It was formed by pull apart mechanism and the Vienna Basin fault system on which the Vienna Basin lies remains seismically active . Significant earthquakes that propagated across the Vienna Basin include the Neulengbach earthquake of 1590 , and the strong temblor that hit Carnuntum in the mid-4th century
Neulengbach earthquake
1590 Neulengbach earthquake
Vienna Basin