Faglia del Lago Maggiore
Darstellung und Status
- Farbe RGB
- R: 250 G: 50 B: 50
- Rang
- Störungszone
- Gebrauch
- Element ist nicht in Gebrauch
- Status
- lokaler Begriff (informell)
Nomenklatur
- Deutsch
- Lago-Maggiore-Störung
- Français
- Faille du Lago Maggiore
- Italiano
- Faglia del Lago Maggiore
- English
- Lago Maggiore Fault
- Herkunft des Namens
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Lago Maggiore
- Historische Varianten
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Lago Maggiore Fault (TK500 / Gouffon et al. 2024)
Paläogeografie und Tektonik
- Tektonische Einheit (bzw. Überbegriff)
- Herkunftstyp
-
- tektonisch
- Metamorphose
- unmetamorph
Referenzen
- Neubearbeitung
-
(2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
p.107: The Lago Maggiore Fault was originally an Early Mesozoic rift fault that separated the Early Jurassic Monte Nudo Basin in the east from the Gozzano High in the west. The Lago Maggiore Fault extends largely below the lake, but in the south, it runs onshore between the Permian volcanics of the Ivrea-Ceneri Complex, overlain by Middle Triassic dolomites, and the Cretaceous – Cenozoic sediments of the Varesotto Imbricates. To the north, the Lago Maggiore Fault probably follows the lake towards the northeast, possibly reflecting the original listric geometry of the Mesozoic precursor fault.