Section 66
Chapter 65,035

Polyphase tectonic subsidence evolution of the Vienna Basin inferred from quantitative subsidence analysis of the northern and central parts

Lee, E Young; Wagreich, M

International Journal of Earth Sciences 106(2): 687-705


ISSN/ISBN: 1437-3254
DOI: 10.1007/s00531-016-1329-9
Accession: 065034844

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The Vienna Basin is a tectonically complex Neogene basin situated at the Alpine–Carpathian transition. This study analyzes a detailed quantification of subsidence in the northern and central parts of the Vienna Basin to understand its tectonic subsidence evolution. About 200 wells were used to arrange stratigraphic setting, and wells reaching the pre-Neogene basement were analyzed for subsidence.

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