Schams-Deckenkomplex

Rappresentazione e statuto

Index

Sch

Colore CMYK

(0%,1%,2%,5%)

Colore RGB

R: 241 G: 239 B: 237

Rango

complesso di falde

Uso

Unità in uso.

Status

valido

Discussione del statuto

Muntogna/Tgea da Schons, Valle di Schams, Vallée de Schams

Nomenclatura

Deutsch

Schams-Deckenkomplex

Français

Complexe de nappes du Schams

Italiano

Complesso di falde dello Schams

English

Schams Nappe Complex

Origine del nome

Schams = Val Schons (GR), Hinterrheintal

Varianti storiche

Schamser Decken (Zyndel 1912, Wyss & Isler 2007), Schamserdecken (Wilhelm 1933), Falde dello Schams (Sciesa 1991), nappes du Schams (Mayerat Demarne 1994), Schams Nappe Complex (TK500 / Gouffon et al. 2024)

Nota sul nome

cf. Schreurs 1990, Schmid et al. 1990

Descrizione

Descrizione

Komplex verfaltetes Deckenkomplex, das in Graubünden zwischen den nordpenninischen Bündnerschiefern und den ophiolithführenden südpenninischen Einheiten liegt und um die Front der Tambo- und Suretta-Decken herumgewickelt ist.

Età

Geomorfologia

• Eocene

Età alla base

• Carbonifero

Geografia

Estensione geografica

Südliche Fortsetzung zwischen die Tamboalp und der Einshorn (Mayerat Demarne 1994).

Paleogeografia e tettonica

Paleogeografia

terrane brianzonese :

microcontinent briançonnais

Termini generici

• Schams

Tipo di origine

• tettonico

Referenze

Revisione

Gouffon Yves (Editor) (2024) : Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern

p.75: The Schams Nappe Complex comprises a set of small nappes, composed of sedimentary sequences exhibiting large facies variations and rich in sedimentary syn-rift breccias of Middle Jurassic to Early Cretaceous age, indicating contemporaneous extension and sinistral strike-slip (Rück 1995). The mid-Cretaceous to Cenozoic post-rift sediments are very similar to those found in the Falknis Nappe. After its emplacement, this nappe complex was folded around the Tambo-Suretta pair during the Niemet-Beverin post-nappe folding (Schreurs 1995). The fact that the Schams nappes are folded around a locally near-isoclinal fold has long raised the question about the origin of this nappe complex either below the Tambo Nappe or on top of the Suretta Nappe (Schmid et al. 1990). Structural criteria clearly show that the Schams Nappe Complex has to be rooted below the Tambo Nappe (Schreurs et al. 1995). Retrodeformation suggests that the Schams nappes formerly occupied an area north of the depositional area of the Tambo and Suretta Mesozoic (Schmid et al. 1997). This is supported by facies arguments indicating that sediments in the originally northernmost paleogeographical position (now forming the Gelbhorn Nappe) suggest N-directed shedding of syn-rift breccias, and by the Subbriançonnais-type facies of the Triassic strata (Rück 1995). The Schams Nappe Complex also contains different mélanges: to the west, in the lower limb of the Niemet-Beverin Backfold, the Knorren Mélange is in contact with the Tambo Nappe, while the Areua-Bruschghorn Mélange marks the boundary with the Tomül Nappe; to the east, in the upper (overturned) limb of the Niemet-Beverin Backfold, the Martegnas Mélange is in contact with the Arblatsch Flysch belonging to the Tomül Nappe (Mayerat Demarne 1994, Schreurs 1995).

Materiale e vario