Goms-Gneiskomplex
Back to Gotthard NappeRepresentation and status
- Index
- G-Go
- Color CMYK
- (0%,16%,16%,2%)
- Color RGB
- R: 250 G: 210 B: 210
- Rank
- lithostratigraphic Formation
- Validity
- Unit is in Use
- Status
- informal term
Nomenclature
- Deutsch
- Goms-Gneiskomplex
- Français
- Complexe gneissique de Goms
- Italiano
- Complesso gneissico di Goms
- English
- Goms Gneiss Complex
- Origin of the Name
- Historical Variants
-
Goms Gneiss Complex (Berger et al. 2017)
Hierarchy and sequence
- Subordinate units
Age
- Age at top
-
- Paleozoic
- Age at base
-
- Precambrian
References
- Definition
-
2017) :
Geological Map of the Aar Massif, Tavetsch and Gotthard Nappes. Geological Special Map 1:100'000, Explanatory Notes 129
p.67: Following OBERHOLZER (1955), the two slices of polycyclic gneisses were depicted on the present map but, due to the map scale, these two lithologically distinguished units were grouped into one single unit called the Goms Gneiss Complex. OBERHOLZER (1955) described two-mica plagioclase K-feldspar gneiss, migmatite (“Mischgneise”) and biotite-plagioclase gneiss derived from sedimentary protoliths intercalated with amphibolitic layers and a serpentinite lens. These rock associations are very similar to sequences in the “Streifengneis” Complex, Paradis Gneiss Complex and the Val Nalps Gneiss Complex of the adjacent Ausserbinn-Piz Cavel Zone of the Gotthard Nappe. Noteworthy is a strong alteration of the gneisses in the region of Ernen and an epidote- and chlorite-rich metagranodiorite (“Gneis von Unterwasser”, OBERHOLZER 1955).
(
- Definition
- 2017) : Geological Map of the Aar Massif, Tavetsch and Gotthard Nappes. Geological Special Map 1:100'000, Explanatory Notes 129 (
-
Unterwassern-Gneis
- Name Origin
-
Unterwassern (VS), Obergoms
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
- In short
-
Feinaugig-flaseriger Serizit-Chlorit- bis Serizit-Biotit-Chloritgneis (Epidot- und Chlorit-reicher Metagranodiorit).