Complesso del Monte del Forno

Representation and status

Color CMYK
(0%,1%,2%,7%)
Color RGB
R: 236 G: 234 B: 232
Rank
tectonically bounded lithostratigraphic unit
Validity
Unit is in Use
Status
informal term

Nomenclature

Deutsch
Monte-del-Forno-Komplex
Français
Complexe du Monte del Forno
Italiano
Complesso del Monte del Forno
English
Monte del Forno Complex
Origin of the Name

Monte del Forno (GR)/(Italia)

Historical Variants

Monte del Forno Series (Ferrario & Montrasio 1976), Fornoserie (Kubli 1983, Peretti 1983), Monte-del-Forno-Komplex (Peretti 1985), Mte del Forno-Komplex (Spillmann 1993), Forno mafics = Forno suite (Puschnig et al. 1996), ozeanische Fornoserie (Hansmann et al. 1996), Monte-del-Forno-Komplex = Forno-Ophiolithe (Spillmann & Trommsdorff 2007), Forno unit (TK500 / Gouffon et al. 2024)

Description

Description

Ophiolitische Abfolge (Metavulkanite/Amphibolite und Metasedimente) der Malenco-Forno-Lizun-Decke. Wurde von der Bergeller Intrusion durchschlagen und kontaktmetamorph überprägt (Ferrario & Montrasio 1976, Peretti 1985).

Palaenography and tectonic

Paleogeography
Piemont Basin
Tectonic unit (resp. main category)
Kind of protolith
  • tectonic

References

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

p.78: Three units with distinct lithological assemblages of oceanic origin, situated in adjacent areas, form the Malenco-Forno-Lizun Nappe. The Malenco unit (Montrasio et al. 2005) consists of large volumes of serpentinite that represent exhumed subcontinental mantle formerly exposed at the ocean floor, and, in a small area adjacent to the Margna Nappe, a transition into continental lower crust in Permian granulite facies, associated with a Permian gabbroic intrusion (Müntener & Hermann 1996). Further north, the Forno unit consists of metabasalts and metagabbros of oceanic origin covered by metasedimentary rocks of Jurassic to Early Cretaceous age, which are in direct contact with the roof of the Bregaglia Intrusion (Puschnig 1998, Froitzheim et al. 1996 a). The Lizun unit, located around the Piz Lizun, northwest of the Engadine Fault and sinistrally offset from the Forno unit (Schmid & Froitzheim 1993), exposes same rocks of oceanic origin as in this latter unit (Liniger & Nievergelt 1990). The Malenco-Forno-Lizun Nappe, together with the Platta Nappe, is located in the hangingwall of the Turba Normal Fault (Nievergelt et al. 1996).

  • Quarziti del Muretto

    Name Origin

    Val Muretto (GR), östlich des Malojapasses

    Rank
    lithostratigraphic Formation
    Status
    informal term
    In short
    Schistes quartzeux à diopside et plagioclase (bytownite). Le protolithe devait être une arkose à matrice argileuse et ciment carbonaté (Mützenberg 1986).
    Age
    Late Cretaceous
  • Formazione dei Rossi

    Name Origin

    I Rossi (GR)

    Rank
    lithostratigraphic unit
    Status
    informal term
    In short
    Metasedimente (kalkhaltige Andalusit-Granat-Biotitschiefer) des Monte-del-Forno-Komplexes.
    Age
    Late Jurassic
  • Quartziti di base

    Rank
    lithostratigraphic unit
    Status
    informal term
    In short
    Quarzit mit lokal zwischengeschaltete Amphibol-Pyroxen-Grünschiefer, Mn-Silikate und kalksilikat-führende Marmore.
  • Anfibolite del Forno

    Name Origin

    Monte del Forno (GR)

    Rank
    lithostratigraphic unit
    Status
    informal term
    In short
    Getüpfelter (gefleckter) bis gebänderter Amphibolit (MORB-Metabasalt ; Gautschi 1980) mit Porphyroblasten aus metamorphem Plagioklas. Pillowstrukturen (mit Epidotschlieren und Kalksilikatlagen als «Interpillow-Sedimente») und Hyaloklastite sind lokal erhalten.
    Age
    Callovian
  • Ofiolite del Forno

    Rank
    lithostratigraphic unit
    Status
    informal term
    In short
    Ophiolithsequenz des Monte-del-Forno-Komplexes.
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