Sinus Vindobonensis Geologia | Bibliographia et Nexus exteni | Nota | Tabula navigationisAmplificaTiefes Kreidemeer, tropische Flachsee und eiszeitlicher StaubPelamycybium (Sphyraenodus) sinus vindobonensisAmplifica

Regiones AustriaeRegiones CechiaeRegiones Slovaciae


AlpesCarpatesCampos PannonicosAustriam InferioremVindobonamCechiamSlovaciamDanubiosedimentis




Sinus Vindobonensis[1] est regio partim plana partim collina inter Alpes, Carpates et Campos Pannonicos ambitu 50 × 200 km². Circiter 80 % areae ad Austriam Inferiorem et Vindobonam, pars autem septentrionalis ad Cechiam et Slovaciam pertinet. Pluries nomen tantum ad regionem fere triangularem a Danubio in meridiem versus adhibetur, cum pars a Danubio in septentrionem versus Marchfeld appelletur.





Geologia |


Basis sinus Vindobonensis circiter 20 milliones annorum ante – formatione Alpium quasi finita – paulatim in profundum mergebat, quod terrae crustae in regione Vindobonensi zona debilis est. Hic motus adhuc 1-2 mm quotannis progreditur, quod crebrae (sed plerumque leves) terrae motus efficit. Sinus sedimentis marinis fluvialibusque completus est, quorum altitudo usque ad 6 km attingere potest.


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Bibliographia et Nexus exteni |


  • E.Thenius, Niederösterreich. Geologie der österr. Bundesländer, Vindobonae 1974

  • G.Gerstbach, Bestimmung der Sedimentdicke im Testfeld "Wiener Becken". Zeitschr.f.Vermessungsw., Stuttgardiae 1982

  • Geologische Bundesanstalt, Wiener Becken und angrenzende Gebiete. Tabula Geologica 1:200.000 cum commentationibus, Vindobonae 1993

  • Tiefes Kreidemeer, tropische Flachsee und eiszeitlicher Staub


Nota |



  1. ↑ Pelamycybium (Sphyraenodus) sinus vindobonensis, in: TOULA,F.1905. Ueber einem dem Thunfische verwandten Raubfisch der Congerienschichten der Wiener Bucht ..., Jb.k.k.Geol.Reichsanst., 55: 51-84






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