Complesso Ivrea-Ceneri

Rappresentazione e statuto

Colore RGB
R: 241 G: 239 B: 237
Rango
zona tettonica
Uso
Unità non usata
Status
termine informale

Nomenclatura

Deutsch
Ivrea-Ceneri-Komplex
Français
Complexe Ivrea-Ceneri
Italiano
Complesso Ivrea-Ceneri
English
Ivrea-Ceneri Complex
Varianti storiche

Ivrea-Ceneri Complex (TK500 / Gouffon et al. 2024)

Gerarchia e successione

Paleogeografia e tettonica

Paleogeografia
margine continentale adriatico :

southern continental margin / platform

Termini generici
Tipo di origine
  • tettonico
Metamorfismo
non metamorfo

Referenze

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

p.105: The Alpine-tectonic Ivrea-Ceneri Complex includes the lower crustal rocks of the Ivrea Zone and the WNW part of the middle – upper crustal Strona-Ceneri Zone. In the northwest, the Ivrea-Ceneri Complex is separated from the Canavese Zone by the Internal Canavese Fault, east of Locarno from the Central Alps by the Tonale Fault. In the east and southeast, the transition to the Upper Orobic Nappe is not clearly defined. The boundary can be traced along the Tamaro Thrust (Bächlin 1937) and the Lago Maggiore Fault. In the south, west of Lago Maggiore, the Ivrea-Ceneri Complex with its Mesozoic cover is overlain by the post-orogenic deposits of the Po Plain.

  • Zona Ivrea-Verbano

    Name Origin

    Ivrea (Italia) e Verbano = Lago Maggiore

    Rango
    zona tettonica
    Statuto
    valido
    Nomenclatorial Remarks
    <p>non: Verbania (= zona di Strona-Ceneri)</p>
    In breve

    The Ivrea Zone is an ante-alpine, thick-skinned tectonic unit of the western South Alpine domain, made up of high-grade polymetamorphic gneisses ("kinzigite"), a mafic to ultramafic complex, as well as subordinated pegmatites and marbles.

    Age
    Paleozoico
  • Zona di Strona-Ceneri

    Rango
    zona tettonica
    Statuto
    valido
    In breve

    The Strona-Ceneri-Zone is an ante-alpine, thick-skinned tectonic unit of the western South Alpine domain. It is made up of polymetamorphic (para)gneisses and amphibolites, as well as late to post-Variscan plutonic and volcanic rocks.

    Age
    Mesozoico
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