Granite de Vallorcine

Darstellung und Status

Farbe CMYK

(0%,48%,56%,6%)

Farbe RGB

R: 240 G: 125 B: 105

Rang

lithostratigraphische Formation

Gebrauch

Element ist in Gebrauch

Status

informeller Begriff

Nomenklatur

Deutsch

Vallorcine-Granit

Français

Granite de Vallorcine

Italiano

Granito di Vallorcine

English

Vallorcine Granite

Herkunft des Namens

Vallorcine (France)

Historische Varianten

granite de Valorcine (Necker 1828), granite de Valorsine (Delesse 1850), Valorsine-Granit = Granit bei Poyaz (Gerlach 1871), Valorsine-Granit = Granit der Barberine (Studer 1872), granite de Vallorcine (Corbin & Oulianoff 1931, Dhellemmes 1955, Krummenacher 1959), Vallorcine-Granit (Labhart & Rybach 1972), Vallorcine anatectic granite (Bussy et al. 2000, Capuzzo et al. 2003); mylonite: Reinhard & Preiswerk 1927

Links

Synonyme

Granite des Aiguilles Rouges

Mylonite de Miéville

Hierarchie und Abfolge

Übergeordnete Einheit

• Mittelvariszische Intrusiva

Untergeordnete Einheiten

• Mylonite de Miéville

Untergrenze

Contact intrusif dans le Complexe gneissique du Brévent visible dans la région de Vallorcine (Dhellemmes 1955).

Alter

Alter Top

• Spätes Karbon

Alter Basis

• Spätes Karbon

Datierungsmethode

307 +/-2 Ma (U/PB on zircon and monazite ; Bussy et al. 2000), 306.5 +/-1.5 Ma

Geografie

Geographische Verbreitung

Etroite bande s'étendant d'Argentière (vallée de Chamonix) à Vernayaz (plaine du Rhône), sur le flanc SE de la partie septentrionale du massif des Aiguilles Rouges.

Typusregion

vallée de Vallorcine

Referenzprofile

• carrière de Miéville
  Koordinaten
  • (568270 / 110960)
  Notizen
  • différents stades de mylonitisation sont observables

Paläogeografie und Tektonik

• Variszische Plutonite des Helvetikums

Tektonische Einheit (bzw. Überbegriff)

• Aiguilles Rouges :
  massif des Aiguilles Rouges

Herkunftstyp

• plutonisch

Metamorphose

monozyklisch

Metamorphosefazies

• Grünschiefer-Fazies (Epizone)

Bemerkung zur Metamorphose

contact SE intensément mylonitisé

Referenzen

Erstdefinition

Necker Louis Albert (1828) : Mémoire sur la vallée de Valorsine. Mém. Soc. phys. hist. nat. Genève IV 209

«Granite à feldspath blanc dominant, à quartz gris, à mica noir, dont les feuillets sont irrégulièrement disséminés dans toute la masse. De grands cristaux de feldspath donnent à ce granite la structure porphyrique». (Necker 1828 p.209)

Neubearbeitung

Bussy François, von Raumer Jürgen, Capuzzo Nicola (2001) : Mont-Blanc, Aiguilles-Rouges massifs (External Massifs) - an example of polyorogenic evolution. Fieldtrip Guide 1, 53-84, Univ. Lausanne

p. 67: Located in the northern part of the Aiguilles- Rouges massif (stop 1A and 1G1), the Vallorcine granite is a 15-km-long by 1-km thick sheet-like pluton (see fig. 23), which intruded at 306.5 ± 1.5 Ma along a steeply dipping, NE-SW trending, dextral strike-slip shear zone (Brändlein 1991; Brändlein et al. 1994). Syntectonic intrusion is inferred on the basis of structural analysis, which documents long-lasting strike-slip shearing both in the country rocks (pre- and post-intrusion fabrics) and in the granite. The latter developed an early NE-SW trending magmatic flow structure, evolving locally into a post-solidus foliation. The Vallorcine granite was subsequently affected along its SE contact by an intense low-T ductile shearing leading to the well-known “Miéville ultramylonite” (Kerrich et al. 1980) of Late Variscan age (but reworked during the Alpine orogeny). Alpine relief provides a 2000 m-high natural cross-section through the pluton. The lowermost facies is a biotite-rich monzogranite hosting numerous enclaves up to 30 cm in size; including gneiss xenoliths from the country rocks, hornfelses, micaceous restites with sillimanite and hercynite, early cordierite-bearing leucogranite blocks and mafic microgranular enclaves. The upper facies is finer-grained with less biotite and almost no enclaves, pointing to an enclave unmixing process during upward motion of the magma. Aplitic and subvolcanic dykes are concentrated within the wall rocks of the upper contact. The Vallorcine intrusion is a typical S-type granite, as confirmed by zircon typology, stable isotopes (Brändlein et al. 1994) and the presence of Al-rich minerals (cordierite, muscovite, andalusite, etc.).

Wichtige Publikationen

Necker Louis Albert (1828) : Mémoire sur la vallée de Valorsine. Mém. Soc. phys. hist. nat. Genève IV 209

Delesse A. (1850) : Analyse du granite de Valorsine. Bull. Soc. geol. Fr. (2) VII, 424

Labhart Toni P., Rybach L. (1972) : Der Vallorcine-Granit und seine radiometrischen Anomalien. Schweiz. Min. Petr. Mitt. 52/3, 571-574

Material und Varia