Crena-Martin-Schuppe
Darstellung und Status
- Farbe CMYK
- (0%,1%,2%,5%)
- Farbe RGB
- R: 241 G: 239 B: 237
- Rang
- tektonische Schuppe
- Gebrauch
- Element ist in Gebrauch
- Status
- lokaler Begriff (informell)
Nomenklatur
- Deutsch
- Crena-Martin-Schuppe
- Français
- Écaille du Crena Martin
- Italiano
- Scaglia della Crena Martin
- English
- Crena-Martin Slice
- Herkunft des Namens
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Crena Martin (GL)/(GR), Pass zwischen Sernftal und Val da Pigniu/Surselva
- Historische Varianten
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Crena-Martin Slice (von Däniken & Frehner 2017)
Paläogeografie und Tektonik
- Paläogeografie
- Europäischer Kontinent
- Tektonische Einheit (bzw. Überbegriff)
Referenzen
- Neubearbeitung
-
(2017) :
3D structural model and kinematic interpretation of the Panixer Pass Transverse Zone (Infrahelvetic Complex, eastern Switzerland). Swiss J. Geosc. 110/2, 653-675
p.654: The Crena-Martin Slice crops out very locally in the Panixer Pass area and forms the recumbent to downward facing Crena Martin Fold (CMF; Figs. 2, 3), which is a major element of the Panixer Pass Transverse Zone. It comprises Triassic dolomite (Röti Fm.) and Permian Verrucano-Breccia in stratigraphically inverted position (Fig. 3b). The assumption that the Crena-Martin Slice may be correlated with the Cavistrau
Nappe further south-west (Wyssling 1950) seems reasonable due to its lithological content and tectonic position.