Neue Untersuchungen der Oberottnangischen Sande in Niederösterreich, Molasse Becken

  • Markus Palzer (Autor*in)
  • Wagreich, M. (Autor*in)
  • Wolfgang Knierzinger (Autor*in)

Aktivität: VorträgePosterpräsentationScience to Science

Beschreibung

In the Early Miocene (Late Ottnangian), a global sea level drop and the continuous rise of the Alps lead to the regression of the Parathethys and to the sedimentation of the Upper Freshwater Molasse. In the Lower Austrian Molasse Basin, this event is represented by yellowish-brownish to greyish white mica-rich and carbonate-free sands and silts with clayish interlayers, formerly called Oncophora Beds (OB), which crop out between St. Pölten and Tulln. A new definition combines these sediments, now called Traisen-Formation (TF) together with the Dietersdorf Formation within the Pixendorf Group. Drill cores from OMV-wells predominantly from the NW show hundreds of meters thick sequences of pelites with intersections of sands interpreted as representing the OB. Contrary to the mainly brackish TF, a turbiditic deeper-water environment is inferred. An OMV-funded project will investigate the relationship between these sediments, their stratigraphical and chronological range, provenance and internal stratigraphy.First results from outcrops and the Wildendürnbach-K4 well confirm large differences in grain size, structures and carbonate content. XRD-results indicate quartz, feldspar, muscovite, chlorite, calcite and dolomite as the main minerals within the sands and pelites. Pyrite is frequent. Halite and kaolinite occur. Heavy minerals show high amounts of homogenous almandine-rich garnets (60-70 %), up to 20 % epidote and amphiboles (8-15%) for the TF. Characteristic chemical compositions of garnet (alm~65; gro~22; pyr~9; spes~4) and high white mica contents possibly point towards medium grade metapelitic rocks from Austroalpine Crystalline Complexes of the Eastern Alps as a main source area, but other sources could also be identified. Further investigations will show, if the “deep-water OB” can be defined as a further separate formation of the Pixendorf Group.
Zeitraum16 Sept. 2014
EreignistitelPANGEO 2014
VeranstaltungstypKonferenz
OrtWien, ÖsterreichAuf Karte anzeigen

Schlagwörter

  • Oncophora
  • Obere Süßwassermolasse
  • Traisen Formation
  • Schwerminerale