Partnach Formation | |
---|---|
Stratigraphic range: Ladinian (Longobardian) ~ | |
Type | Geologic formation |
Underlies | Wetterstein Formation |
Overlies | Reifling Formation |
Lithology | |
Primary | Clayey shales (marls) and limestone |
Location | |
Coordinates | 47°06′N9°54′E / 47.1°N 9.9°E |
Approximate paleocoordinates | 8°36′N21°54′E / 8.6°N 21.9°E |
Region | Carinthia, Vorarlberg |
Country | Austria Slovakia |
Extent | Northern Limestone Alps |
Type section | |
Named for | Partnach |
Named by | Wilhelm von Gümbel |
The Partnach Formation is a Middle Triassic geologic formation in the eastern Northern Limestone Alps and Western Carpathians, within Austria and Slovakia, Central Europe. [1] The formation consists of alternating grey and green marls and shales (Partnach shales) and grey limestones (Partnach Limestone), often brecciated, oncolithic and containing clay intraclasts. [2] The formation is gradually evolving from the Reifling Formation. It is usually overlain by the Lunz/Reibl Formation or Wetterstein Formation. Sediments of the Partnach Formation were deposited in intrashelf basins.
The rock unit was originally defined as Partnachschichten by Wilhelm von Gümbel in 1858.
It preserves fossils dated to the Ladinian age of the Middle Triassic Epoch of the Triassic Period. [1] [3]
Nothosaurus is an extinct genus of sauropterygian reptile from the Triassic period, approximately 240–210 million years ago, with fossils being distributed throughout the former Tethys Ocean, from North Africa and Europe to China. It is the best known member of the nothosaur order.
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The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians.
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