Day 2 Tue, November 12, 2019 2019
DOI: 10.2118/197145-ms
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High Risk Exploration in a Hypermature Hydrocarbon Basin: An Example from the Vienna Pull-Apart Basin, Austria

Abstract: OMV’s exploration efforts in Austria include the prospecting for new fields in units of the Alpine thrust belt below the Neogene Vienna Basin. Current exploration efforts are targeting the deep and underexplored parts of the Paleogene thrust belt with potentially large structural closures within the so-called Rhenodanubian Flysch units. Interpretation of fold-thrust structures is primarily based on new 3D seismic reflection data, which images the Paleogene nappes buried below the Neogene Vienna … Show more

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Cited by 2 publications
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“…Miocene sediments in the proto-Vienna Basin were deposited on top of allochthonous Alpine tectonic units which had been thrust onto autochthonous basement (Bohemian Massif and its sedimentary cover) during Paleogene to early Miocene times (Beidinger and Decker, 2016;Beidinger et al, 2019). The basin fill comprises sediments deposited during a piggy-back basin phase (early Miocene) and subsequent middle to late Miocene pull-apart and east-west extensional stages (neo-Vienna Basin; Hinsch et al, 2005).…”
Section: Geological Settingmentioning
confidence: 99%
“…Miocene sediments in the proto-Vienna Basin were deposited on top of allochthonous Alpine tectonic units which had been thrust onto autochthonous basement (Bohemian Massif and its sedimentary cover) during Paleogene to early Miocene times (Beidinger and Decker, 2016;Beidinger et al, 2019). The basin fill comprises sediments deposited during a piggy-back basin phase (early Miocene) and subsequent middle to late Miocene pull-apart and east-west extensional stages (neo-Vienna Basin; Hinsch et al, 2005).…”
Section: Geological Settingmentioning
confidence: 99%