Milano Belt
Retour à Milan BeltReprésentation et statut
- Index
- Mi
- Couleur CMYK
- N/A
- Couleur RGB
- R: 241 G: 239 B: 237
- Rang
- tectonique
- Usage
- Ce terme est en usage.
- Status
- valide
Nomenclature
- Deutsch
- Überschiebungsgürtel von Mailand
- Français
- Ceinture de chevauchement de Milan
- Italiano
- Milano Belt
- English
- Milan Belt
- Origine du nom
-
Milano (Italia)
- Variantes historiques
-
Milan belt (Laubscher 1985), Lombardic Nappe (Schönborn 1992), Milano Belt (TK500 / Gouffon et al. 2024)
Âge
- Âge au sommet
-
- Miocène tardif
- Âge à la base
-
- Miocène moyen
Géographie
- Extension géographique
- Po Plain.
Références
- Révision
-
(2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
p.103: The southernmost and lowest thrust system is called the Milan Belt; its basement ramps are hidden below the Po Plain like most of the deformed sedimentary cover (Fantoni et al. 1999). The Milan Belt consists of thrust imbricates, locally inverting Mesozoic high-angle faults, developed as a frontal accretion of the western South Alpine domain during the Miocene. East of Lago di Garda, units equivalent to the Milan Belt crop out extensively along the External Giudicarie Zone.