Schiahorn-Decke
Back to Schiahorn NappeRepresentation and status
- Color CMYK
- N/A
- Color RGB
- R: 241 G: 239 B: 237
- Rank
- nappe
- Validity
- Unit is in Use
- Status
- valid
Nomenclature
- Deutsch
- Schiahorn-Decke
- Français
- Nappe du Schiahorn
- Italiano
- Falda dello Schiahorn
- English
- Schiahorn Nappe
- Origin of the Name
-
Gross Schiahorn (GR), NW Davos
- Historical Variants
-
Aroser Dolomiten auct., Schiahorndolomit (Cadisch 1922), Schiahorn-Decke (Pfiffner 2015, Signer et al. 2018), Schiahorn Nappe (TK500 / Gouffon et al. 2024)
Description
- Description
-
Unterostalpine Decke
Hierarchy and sequence
- Subordinate units
Age
- Age at top
-
- Triassic
- Age at base
-
- Triassic
Geography
- Geographical extent
- NW der Engadin-Störung
Palaenography and tectonic
- Paleogeography
-
Adriatic continental margin
:
southern, passive continental margin / platform
- Tectonic unit (resp. main category)
- Kind of protolith
-
- tectonic
References
- Definition
-
2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
(
p.92: The Schiahorn Nappe (formerly “Arosa Dolomites”) is a small unit underlying the Silvretta Nappe between Tiefencastel and Davos. It consists of Triassic to Early Jurassic sediments with lithofacies similar to that of the Upper Austroalpine Ortler Nappe (see § 8.2.7; Furrer 1993, Eberli 1988, Froitzheim et al. 1994). In the Rätikon area (northeast corner of the Prättigau Half-Window), Nagel (2006) correlates the sedimentary “Southern Mittagspitz Zone” with the Schiahorn Nappe, both having a similar stratigraphic sequence with respect to the Allgäu Nappe, as well as a structurally comparable position with it.
-
«Südliche Mittagsspitz-Zone»
- Rank
- tectonic zone
- Status
- valid
- In short
-
In the Rätikon area (northeast corner of the Prättigau Half-Window), Nagel (2006) correlates the sedimentary «Southern Mittagspitz Zone» with the Schiahorn Nappe, both having a similar stratigraphic sequence with respect to the Allgäu Nappe, as well as a structurally comparable position with it.