Massif des Aiguilles Rouges

Darstellung und Status

Farbe CMYK

N/A

Farbe RGB

R: 241 G: 237 B: 239

Rang

Gebirgsmassiv

Gebrauch

Element ist in Gebrauch

Status

gültig

Diskussion des Status

Nomenklatur

Deutsch

Aiguilles-Rouges-Massiv

Français

Massif des Aiguilles Rouges

Italiano

Massiccio delle Aiguilles Rouges

English

Aiguilles Rouges Massif

Herkunft des Namens

Aiguilles Rouges de Chamonix (France)

Historische Varianten

Gruppe der Aiguilles Rouges = Centralmasse der Aiguilles Rouges (Gerlach 1871), massif des Aiguilles Rouges de Chamonix (Argand 1911b), massif cristallin des Aiguilles Rouges (Collet et al. 1952), Aiguilles Rouges Massiv (Büchi & Trümpy 1976), Aiguilles Rouges massif (von Raumer & Bussy 2004), Aiguilles Rouges Massif (Gouffon et al. 2024)

Beschreibung

Beschreibung

Massif cristallin externe composé d'un socle anté-varisque (micaschistes et gneiss, en partie migmatitiques) et d'intrusions carbonifères. La schistosité verticale de direction N-S est recoupée par des structures NE-SW (Granite de Vallorcine et sa bordure orientale mylonitique, graben permo-carbonifère de Salvan-Dorénaz).

Hierarchie und Abfolge

Untergeordnete Einheiten

• fossé permo-carbonifère de Salvan-Dorénaz
• Submassif de l'Arpille
• Submassif de Fully

Referenzen

Neubearbeitung

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

p.33: The Aiguilles Rouges Massif is made up of the same rocks as the Belledonne Massif, but also includes Permian sediments. It has a relatively thin autochthonous Mesozoic–Cenozoic sedimentary cover, except in the Val d’Illiez and on the slopes of the Rhône Valley between Monthey and St-Maurice, where the series ends with an autochthonous Molasse formation, which has long been considered an internal slice of the Subalpine Molasse. The Dent de Valère Flysch outcropping north of the Dents du Midi – considered as “Ultrahelvetic” on the previous versions of the map – seems to belong to the autochthonous flysch (Jeanbourquin et al. 1992).
The Aiguilles Rouges Massif is separated from the Mont Blanc Massif by a thin band of Mesozoic sediments often referred to as the “Chamonix Syncline” in the literature. Most of these sediments can be considered as belonging to the cover of the Mont Blanc Massif, although its basal contact is strongly tectonized, even tectonic (Pfiffner et al. 2010). This band hides important tectonic contacts, not only that between both massifs and their sedimentary cover, but also a probable SW extension of the Rhône-Simplon Fault (Mancktelow 1992, Hubbard & Mancktelow 1992, Egl i & Mancktelow 2013).

Wichtige Publikationen

von Raumer Jürgen F., Neubauer F. (1993) : Pre-Mesozoic Geology in the Alps. Springer Verlag, 677 pages