Piz-Nair-Serpentinit

Representation and status

Color CMYK
(5%,0%,41%,27%)
Color RGB
R: 175 G: 185 B: 110
Rank
lithostratigraphic unit
Validity
Unit is in Use
Status
informal term

Nomenclature

Deutsch
Piz-Nair-Serpentinit
Français
Serpentinite du Piz Nair
Italiano
Serpentinite del Piz Nair
English
Piz Nair Serpentinite
Origin of the Name

Piz Nair (GR), oberhalb Champatsch

Historical Variants

serpentine du Nordriff (Vuagnat 1965), Ophiolithe des Piz Nair = Zone von Champatsch = Randzone (Cadisch et al. 1968), Piz Nair serpentinite (Florineth & Froitzheim 1994), Serpentinit vom Piz Nair (Gruber et al. 2010)

Nomenclatorial Remarks

cf. Vuichard 1984

Components

Mineral Content
  • clinopyroxene
  • chrysotile
  • spinel

Geography

Geographical extent
Unterengadiner Fenster.

Palaenography and tectonic

Tectonic unit (resp. main category)
Conditions of formation

Subkontinentaler Mantelperidotit, exhumiert durch tektonische Denudation (Florineth & Froitzheim 1994)

Metamorphism
monocyclic
Metamorphic facies
  • greenschist facies (epizone)

References

Definition
Vuichard D. (1984) : The ophiolitic suite of the Alp Champatsch (Lower Engadine window, Switzerland): the metamorphic and tectonic evolution of a small oceanic basin in the Penninic realm? Ofioliti 9/3, 619-632

p.619: A serpentinised peridotite originating from lherzolitic mantle material forms the main component of the ophiolie complex [of the Alps Champatsch].

Back to top