Integrated high-resolution stratigraphy: Relative contributions of tectonics, eustasy and climate on basin evolution (Vienna Basin, Austria)

W.E. Paulissen

Sedimentary basins form in a range of large-scale tectonic settings involving extensional, compressional or lateral movements. The dynamics of the basin infill are controlled by driving mechanisms such as tectonics, climate and eustatic control. The created accommodation space in the basin is filled