Platta-Ophiolith

Rappresentazione e statuto

Colore CMYK

(38%,0%,25%,37%)

Colore RGB

R: 100 G: 160 B: 120

Rango

unità litostratigrafia

Uso

Unità in uso.

Nomenclatura

Deutsch

Platta-Ophiolith

Français

Ophiolite du (Piz) Platta

Italiano

Ofiolite del (Piz) Platta

English

Platta Ophiolite

Origine del nome

Piz Platta (GR)

Varianti storiche

Ophiolithe vom Typus der Platta-Decke (Büchi & Trümpy 1976), Platta-Ophiolithe (Spillmann 1993), Ophiolites [of the Platta nappe] (Manatschal & Nievergelt 1997), Ophiolites of the Piz Platta region

Gerarchia e successione

Unità di rango inferiore

• Flix-Diabas
• Alp-Natons-Gabbro
• Fallerfurgga-Serpentinit
• Marmorera-Serpentinit

Geografia

Estensione geografica

Serpentinit, Grabbro, Basalt und Grünschiefer, mit untergeorneten Sedimenten.

Paleogeografia e tettonica

Paleogeografia

Bacino Piemontese

Termini generici

• Platta

Tipo di origine

• ofiolitico

Metamorfismo

monociclico

Facies metamorfica

• facies a scisti verdi

Osservazioni sul metamorfismo

Ultrabasic rocks are represented by lizardite-chrysotile-serpentinite north of Bivio and antigorite bearing lizardite-chrysotile-serpentinite south of Bivio, indicating an increase in Alpine metamorphism from north to south (Trommsdorff & Evans 1974, Trommsdorff 1983).

Referenze

Definizione

Dietrich Volker (1969) : Die Ophiolithe des Oberhalbsteins (Graubünden) und das Ophiolithmaterial der ostschweizerischen Molasseablagerung ein petrographischer Vergleich. Diss. ETHZ Nr.4397, 179 S.

Revisione

Manatschal Gianreto, Nievergelt Peter (1997) : A continent-ocean transition recorded in the Err and Platta nappes (Eastern Switzerland). Eclogae geol. Helv. 90/1, 3-27

p.8: Ophiolites [of the Platta nappe]

Massive basalts, pillow lava and breccia and hyaloclastites represent the extrusive part of the ophiolite suite of the Platta nappe (Steinmann 1905, Cornelius 1935. Dietrich 1969. 1970). With higher strain and grade of metamorphism towards the south, the primary extrusive structures are gradually obliterated (Dietrich 1969). Gabbro is rare and is intrusive together with basaltic dikes in serpentinite. Some gabbros are undeformed (e.g. Val Natons). whereas others are strongly foliated and exhibit a clear stretching lineation and asymmetric fabrics indicating non-coaxial shear under high-temperature conditions (at least 400 to 500 C). Plagioclase and pyroxene ribbons suggest crystal plastic deformation mechanisms, active during the deformation of these rocks. Since Alpine metamorphism in the area is only of greenschist facies (Trommsdorff 1983), a pre-Alpine age for these gabbroic mylonites is strongly suggested.

Ultrabasic rocks are represented by lizardite-chrysotile-serpentinite north of Bivio and antigorite bearing lizardite-chrysotile-serpentinite south of Bivio, indicating an increase in Alpine metamorphism from north to south (Trommsdorff & Evans 1974, Trommsdorff 1983). Unaltered relics of péridotites were not described, but from microscopic as well as from geochemical data spinel lherzolites and harzburgites are presumed to be the protoliths of the serpentinites (Dietrich 1969, Trommsdorff & Evans 1974. Burkhard & O'Neil 1988).