«Detritische Einheit» (der Camosci-Decke)
Back to Camosci NappeRepresentation and status
- Color RGB
- R: 200 G: 150 B: 100
- Rank
- lithostratigraphic Formation
- Validity
- Unit is in Use
- Status
- incorrect name (though informally used)
Nomenclature
- Deutsch
- «Detritische Einheit» (der Camosci-Decke)
- Français
- «Unité détritique» (de la nappe des Camosci)
- Italiano
- «Unità detritica» (della falda dei Camosci)
- English
- «Detritic unit» (of the Camosci nappe)
- Origin of the Name
-
Camosci
- Historical Variants
-
Detritic unit (Carrupt 2003)
Description
- Thickness
- Max. 20-25 m (Carrupt 2003)
Age
- Age at top
-
- Middle Jurassic
- Age at base
-
- Middle Jurassic
- Dating Method
-
Base érosive et analogie de faciès avec les Schistes mordorés (Bajocien-Bathonien ; Carrupt 2003).
Palaenography and tectonic
- Tectonic unit (resp. main category)
- Kind of protolith
-
- sedimentary
References
- Definition
-
2003) :
New stratigraphic, structural and geochemical data from the Val Formazza - Binntal area (Central Alps). Mémoires de Géologie (Lausanne) 41, 103 p.
p.17: Detritic unit: the contact with the Graphitic unit is always clear-cut. Strikingly, the Detritic unit is in contact only with the calcareous micaschist and never with the black micaschist. The detrital input shows a clear evolution: the deposit begins with a hard, grey argillaceous-rich quartzitic metasandstone that becomes riches in dolomitic detritic grains towards the top. It simulates a paragneiss and contains locally centimetric pyrite crystals. This deposit suddenly ends with the abrupt shedding of a very quartz- and clay-poor dolomitic metasandstone. The whole unit has a maximum thickness of 20-25 m.
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