Marne di Monte Serrone | |
---|---|
Stratigraphic range: Early Toarcian ~ | |
Type | Geological formation |
Sub-units | Valdorbia, Colle d'Orlando, Pale Vallone & Pozzale Sections |
Underlies | Rosso Ammonitico, Calcari e Marne a Posidonia & Calcari Diasprigni Formations |
Overlies | Corniola & Calcare Massicio Formations |
Thickness | 64–80 m (210–262 ft) |
Lithology | |
Primary | Calcilutites & clay-rich greenish marls with calcareous lenses |
Other | Argillaceous gray green marls with calcarenites alternated with marls |
Location | |
Coordinates | 42°59′30.1″N 12°50′58.2″E / 42.991694°N 12.849500°E |
Region | Umbria |
Country | Italy |
Extent | Umbria-Marche Basin |
Type section | |
Named for | Monte Serrone |
Named by | Pialli |
Year defined | 1969 |
The Marne di Monte Serrone ("Monte Serrone Marl") is a geological formation in Italy, dating to roughly between 181 and 178 million years ago,[1] and covering the early and middle Toarcian stage of the Jurassic Period of central Italy.[2] It is the regional equivalent to the Toarcian units of Spain such as the Turmiel Formation, units in Montenegro, such as the Budoš Limestone and units like the Tafraout Formation of Morocco.[2][3]