Travenanzes Formation | |
---|---|
Stratigraphic range: early Carnian (Tuvalian) ~ | |
Type | Geologic formation |
Underlies | Dolomia Principale |
Overlies | Heiligkreuz Formation (unconformably) |
Lithology | |
Primary | Dolomite |
Other | Limestone, marl |
Location | |
Coordinates | 46°12′N11°06′E / 46.2°N 11.1°E |
Approximate paleocoordinates | 18°36′N17°00′E / 18.6°N 17.0°E |
Region | Trentino-Alto Adigo |
Country | Italy |
Extent | Southern Limestone Alps |
The Travenanzes Formation is a Late Triassic (early Carnian, or early Tuvalian in the regional stratigraphy) limestone, marl and dolomite formation in the Southern Limestone Alps in Trentino-Alto Adige, Italy. [1]
The Travenanzes Formation is conformably overlain by the Dolomia Principale, [2] and overlies the Heiligkreuz Formation separated by an unconformity. Deposition of the formation took place just after the Carnian Pluvial Event (CPE). [3]
The following fossils have been described from the Travenanzes Formation: [1]