Milano Belt
Torna a Milan BeltRappresentazione e statuto
- Index
- Mi
- Colore CMYK
- N/A
- Colore RGB
- R: 241 G: 239 B: 237
- Rango
- tettonica
- Uso
- Unità in uso.
- Status
- valido
Nomenclatura
- Deutsch
- Überschiebungsgürtel von Mailand
- Français
- Ceinture de chevauchement de Milan
- Italiano
- Milano Belt
- English
- Milan Belt
- Origine del nome
-
Milano (Italia)
- Varianti storiche
-
Milan belt (Laubscher 1985), Lombardic Nappe (Schönborn 1992), Milano Belt (TK500 / Gouffon et al. 2024)
Età
- Geomorfologia
-
- tardo Miocene
- Età alla base
-
- Miocene medio
Geografia
- Estensione geografica
- Po Plain.
Referenze
- Revisione
-
(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.