Falda dei Camosci
Zurück zu Camosci-DeckeDarstellung und Status
- Farbe CMYK
- N/A
- Farbe RGB
- R: 241 G: 239 B: 237
- Rang
- tektonische Zone
- Gebrauch
- Element ist in Gebrauch
- Status
- gültig
Nomenklatur
- Deutsch
- Camosci-Decke
- Français
- Nappe des Camosci
- Italiano
- Falda dei Camosci
- English
- Camosci Nappe
- Herkunft des Namens
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Ghiacciao risp. Alpe dei Camosci (Italia)
- Historische Varianten
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Bedretto Zone (Hansen 1972, Bianchi et al. 1998), Camosci nappe (Carrupt 2003), Camosci-Zone, Camosci Nappe (Berger et al. 2017)
- Nomenklatorische Bemerkungen
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= Alpage des Chamois
Alter
- Alter Top
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- Jura
- Alter Basis
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- Trias
Referenzen
- Erstdefinition
- (2003) : New stratigraphic, structural and geochemical data from the Val Formazza - Binntal area (Central Alps). Mémoires de Géologie (Lausanne) 41, 103 p.
- Neubearbeitung
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(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).