Schiahorn-Decke

Back to Schiahorn Nappe

Representation 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

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
Gouffon Yves (Editor) (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.

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