Malmurainza-Formation
Back to Fuorcla-d’Alp-FormationRepresentation and status
- Color CMYK
- (5%,0%,40%,18%)
- Color RGB
- R: 200 G: 210 B: 125
- Rank
- lithostratigraphic Formation
- Validity
- Unit is in Use
- Status
- informal term
Nomenclature
- Deutsch
- Malmurainza-Formation
- Français
- Formation du (Piz) Malmurainza
- Italiano
- Formazione del (Piz) Malmurainza
- English
- Malmurainza Formation
- Origin of the Name
- Historical Variants
-
Bündnerschiefer auct., Malmurainza-Formation (Bertle 2004)
Description
- Thickness
- Mehr als 100 m (Bertle 2004).
Age
- Age at top
-
- Late Cretaceous
- Age at base
-
- Late Cretaceous
Geography
- Geographical extent
- Unterengadiner Fenster.
References
- Definition
-
2004) :
The Sedimentary Record of North Penninic Schistes lustrés of the Lower Engadine Window and its Correlation to the Tauern Window (Eastern Alps). Jahrbuch der Geologischen Bundesanstalt 144/2, 165-171
p.167: They are in turn overlain by a sedimentary sequence of turbiditic character: the Malmurainza Formation. It consists of a rhythmic layering of dark shales/phyllites and sandstones with some few intercalated coarse grained breccias. The age of the Malmurainza Formation is late Cretaceous in general, an early Tertiary age cannot be excluded, as the tectonically highermost part of the Zone of Pfunds is latest Cretaceous taceous in age, indicated by Lepidorbitoides sp. and Globotruncana ex gr. arca (BERTLE, 1999).
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