| Main Dolomite Hauptdolomit Fődolomit Dolomia Principale | |
| Type: | Geological formation |
| Age: | Carnian-Norian |
| Period: | Norian |
| Prilithology: | Dolomite |
| Otherlithology: | Limestone |
| Namedfor: | "Main Dolomite" |
| Namedby: | Gümbel |
| Year Ts: | 1857 |
| Region: | Limestone Alps & Apennines Central Europe |
| Country: | Austria Germany Hungary Italy Slovakia |
| Thickness: | 0- |
Main Dolomite (German: Hauptdolomit, Hungarian: Fődolomit, Italian: Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857.
Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.[1] The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main".
The formation is found in:
It is primarily made of dolomite, ranging from 0mto2200mm (00feetto7,200feetm) in thickness. Main Dolomite is represented by the medium bedded dolomitic layers often with characteristic stromatolitic lamination. The formation was deposited in shallow lagoons during the Late Carnian and Early Norian ages of the Late Triassic Epoch in the Triassic Period, during the Mesozoic Era.
Fossil sauropodomorph tracks, likely made by a plateosaurid, have been reported from the formation.[2]