Drusberg-Decke

Représentation et statut

Couleur CMYK

N/A

Couleur RGB

R: 241 G: 239 B: 237

Rang

nappe

Usage

Ce terme est en usage.

Status

valide

Nomenclature

Deutsch

Drusberg-Decke

Français

Nappe du Drusberg

Italiano

Falda del Drusberg

English

Drusberg Nappe

Origine du nom

Drusberg = Druesberg (SZ)

Variantes historiques

Drusberg-Decke (Lienert et al. 2003)

Description

Description

Die Hauptmasse der oberhelvetische Drusberg-Decke besteht aus Gesteinen der helvetischen Kreide. Frontalen Schuppen der Drusberg-Decke bilden der helvetische Randkette (Niederhorn, Pilatus, Bürgenstock, Urmiberg, Rigi Hochflue).

Hiérarchie et succession

Unités hiérarchiquement subordonnées

• Fluebrig–Drusberg-Element
• Rederten-Element
• Wiggis-Element
• Wissenwand-Schuppe
• Niederhorn–Pilatus-Schuppe
• Bürgenstock-Urmiberg-Schuppe
• Hochflue-Schuppe

Âge

Âge au sommet

• Eocène

Âge à la base

• Crétacé

Références

Révision

Gouffon Yves (Editor) (2024) : Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern

p.40: From the Kander Valley, the Axen and Drusberg nappes represent the eastward continuation of the Wildhorn Nappe Complex. The transition is caused by a synsedimentary fault (Bachli-Giesenen Fault, Hänni & Pfiffner 2001), which led to the development in the east of a very thick marl sequence (earliest Cretaceous Palfris Formation) that acted as décollement layer during Alpine nappe stacking.

Up to the Engelberg Valley, the stratigraphic series of the Axen Nappe and that of the Drusberg Nappe are practically complementary. The Axen Nappe is composed of a Jurassic series with some Triassic fragments in its base and Cretaceous and Paleogene sediments in the eastern part of the area. The Drusberg Nappe consists only of Cretaceous to Paleogene sediments. Between the Engelberg Valley and the Klöntal, where the Axen Nappe series is complemented by overlying Paleogene sediments, the internal structure of the nappe becomes more complex due to the presence of numerous thrusts following additional décollement levels which split the nappe into several slices. In contrast, the stratigraphic series of the Drusberg Nappe does not change. However, three slices of Late Jurassic limestone (Quinten Formation) are present at its base; one is located in the Muotatal and underlies the Palfris Formation (Wissenwand Slice, Hantke et al. 2013), the other two crop out between the Engelberg Valley and the Vierwaldstättersee, intercalated into the Palfris Formation (Maisander Slices, Menkveld 1995); the latter are considered part of the Axen Nappe.

Between the Thunersee and the Vierwaldstättersee, the Drusberg Nappe contains a large-scale open synformal structure which preserves tectonically higher units in its core, from bottom to top: the Habkern Mélange Zone, the Lower Penninic Schlieren Nappe and klippen of the Middle Penninic Préalpes Médianes Nappe. The internal structure of the Axen Nappe changes abruptly across the Engelberg Valley (Pfiffner et al. 2010, Pfiffner 2011) owing to a fault perpendicular to the fold axes and active during nappe formation. In a similar manner, a fault must be assumed along the southeastern part of the Vierwaldstättersee which explains the very different nappe structure of the Axen and the Drusberg nappes on both sides of the lake (Pfiffner et al. 2010, Pfiffner 2011).

East of the Vierwaldstättersee, the two nappes can be traced all the way up to the Linth Valley. On the western flank of this valley, they are underlain by the Glarus Nappe Complex (including the Mürtschen Nappe), while they are replaced by the Glarus Nappe Complex and the Säntis Nappe on the eastern flank. A major N – S oriented fault is assumed to be present along the Linth Valley in order to explain the dramatic change in internal structure of the Helvetic nappes on either side of the valley.