Complexe de nappes du Wildhorn
Représentation et statut
- Couleur CMYK
- N/A
- Couleur RGB
- R: 241 G: 239 B: 237
- Rang
- complexe de nappes
- Usage
- Ce terme est en usage.
- Status
- valide
- Discussion du statut
Nomenclature
- Deutsch
- Wildhorn-Deckenkomplex
- Français
- Complexe de nappes du Wildhorn
- Italiano
- Complesso di falde del Wildhorn
- English
- Wildhorn Nappe Complex
- Origine du nom
- Variantes historiques
-
Wildhorndecke, nappe du Wildhorn, Wildhorn Nappe Complex (Gouffon et al. 2024)
Description
- Description
-
Die Wildhorn-Decke schliesslich, die umfangreichste der drei Decken, zeigt einen ausgeprägten Stockwerkbau. Sie weist einzig auf der Ostseite des Kientals und am Bundstock einen Kern von Lias auf. Sonst sind die mächtigen «Aalénien- Schiefer» (=Molser Serie) das älteste Schichtglied. Ein komplizierter Malm/Dogger-Faltenbau ist durch die beweglichen Mergel des Berriasien vom Kreide- Stockwerk mit dem transgressiven Tertiär getrennt. (Herb et al. 1978 S.236)
Hiérarchie et succession
- Unités hiérarchiquement subordonnées
- Unités sus-jacentes
- Unités sous-jacentes
- Limite supérieure
-
chevauchement basal ultrahelvétique
Âge
- Âge au sommet
-
- Crétacé
- Âge à la base
-
- Trias
Paléogéographie et tectonique
- Paléogéographie
- domaine sud-helvétique
- Type de protolithe
-
- tectonique
Références
- Révision
-
2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
(
p.40: The Wildhorn Nappe Complex comprises a complete stratigraphic series ranging from Triassic to Paleogene. It occupies the Rawil axial depression: southwest of Rawilpass, the axes of the main folds dip to the NE, while northeast of the pass they dip to the SW. The nappe complex continues to the northeast up to the Kander Valley, where it is replaced by the Axen and Drusberg nappes. The Axen Nappe contains Jurassic strata, whereas the Drusberg Nappe is made up of Cretaceous–Paleogene strata. Hänni & Pfiffner (2001) set the northeastern limit of the Wildhorn Nappe Complex at the Mesozoic synsedimentary Bachli-Giesenen Fault, which was reactivated by Alpine nappe stacking. This fault induced an abrupt lateral increase in the thickness of the Cretaceous sediments toward the east which in turn caused an important change in structural style (Hänni & Pfiffner 2001).
The Wildhorn Nappe Complex consists of three superposed nappes: the Diablerets Nappe, present only in the southwest, at the base of the complex, is linked by a tight syncline to the Mont Gond Nappe, which is also outcropping mainly in the southwestern part of the complex. The highest Sublage Nappe forms the main body of the complex; it overlies the thin Jägerchrüz Nappe north of Sierre and the Gellihorn Nappe further northeast (see § 4.1.3).
-
Nappe du Sublage
- Name Origin
- Rang
- nappe
- Statut
- valide
- En bref
-
The Sublage Nappe is an Upper Helvetic tectonic nappe in the Western Swiss Alps. It is the highest unit of the Wildhorn Nappe Complex and forms the main body of the complex. To the southwest it overlies the Mont Gond Nappe, whereas it overlies the thin Jägerchrüz Nappe north of Sierre and the Gellihorn Nappe further northeast.
-
Synclinal du Prabé
- Name Origin
- Rang
- tectonique
- Statut
- terme informel
- En bref
-
Synclinal couché et très effilé de la nappe du Wildhorn, à coeur d'Ultrahelvétique (nappe d'Anzeinde) et structure interne complexe.
-
Anticlinal de Drône
- Name Origin
- Rang
- tectonique
- Statut
- terme informel
- En bref
- Anticlinal complexe, ramifié et asymétrique (absence du Lias dans le flanc normal), dont le coeur est constitué de gypse et dolomie triasiques.
- Age
- Trias
-
Nappe du Mont Gond
- Name Origin
-
Mont Gond de Conthey (VS), au nord de Conthey
- Rang
- nappe
- Statut
- valide
- En bref
-
The Mont Gond Nappe is an Upper Helvetic tectonic nappe in the Western Swiss Alps. Forming the middle part of the Wildhorn Nappe Complex, it is present only in the southwest and is linked by a tight syncline to the underlying Diablerets Nappe.
- Age
- Jurassique Moyen
-
Écaille de Prapio-Audon
- Name Origin
-
Col de Prapio (VD) et Becca d'Audon = Oldenhorn (VD)/(VS)/(BE)
- Rang
- écaille tectonique
- Statut
- terme local (informel)
- En bref
-
Flanc renversé de la nappe du Mont Gond.
-
Nappe des Diablerets
- Name Origin
- Rang
- nappe
- Statut
- valide
- En bref
-
The Diablerets Nappe is an Upper Helvetic tectonic nappe in the Western Swiss Alps. Forming the base of the Wildhorn Nappe Complex, it is present only in the southwest and is linked by a tight syncline to the overlying Mont Gond Nappe.
- Age
- Jurassique Moyen