Falda dei Camosci
Retour à nappe des CamosciReprésentation et statut
- Couleur CMYK
- N/A
- Couleur RGB
- R: 241 G: 239 B: 237
- Rang
- zone tectonique
- Usage
- Ce terme est en usage.
- Status
- valide
Nomenclature
- Deutsch
- Camosci-Decke
- Français
- Nappe des Camosci
- Italiano
- Falda dei Camosci
- English
- Camosci Nappe
- Origine du nom
-
Ghiacciao risp. Alpe dei Camosci (Italia)
- Variantes historiques
-
Bedretto Zone (Hansen 1972, Bianchi et al. 1998), Camosci nappe (Carrupt 2003), Camosci-Zone, Camosci Nappe (Berger et al. 2017)
- Remarques nomenclatoriales
-
= Alpage des Chamois
Âge
- Âge au sommet
-
- Jurassique
- Âge à la base
-
- Trias
Références
- Définition
- (2003) : New stratigraphic, structural and geochemical data from the Val Formazza - Binntal area (Central Alps). Mémoires de Géologie (Lausanne) 41, 103 p.
- Révision
-
(2017) :
Geological Map of the Aar Massif, Tavetsch and Gotthard Nappes. Geological Special Map 1:100'000, Explanatory Notes 129
p.79: CARRUPT (2003) defined the Camosci Nappe including parts of the “Bedretto Zone” of BIANCHI et al.(1998). This nappe comprises the “Sabbione Zone” of LEU (1986) and parts of the Termen Zone, and is dominated by dolomite and calcite marble and dark calcareous micaschist (“graphitic unit” of CARRUPT 2003). The first group has often been considered as Triassic in age (LEU 1986, CARRUPT 2003), whereas the ages of the other units are under debate (LEU 1986, CARRUPT 2003). A detailed discussion of the Camosci Nappe is given in CARRUPT (2003).