Laguna Brava Formation
From Wikipedia, the free encyclopedia
Laguna Brava Formation (Spanish: Formación Laguna Brava), formerly referred to as Santo Domingo Formation, is a Late Eocene (Tinguirirican in the SALMA classification) sedimentary formation located in the Argentine Northwest.[1] The formation contains beds with fossil bird tracks described as Gruipeda dominguensis.[2]
Laguna Brava Formation | |
---|---|
Stratigraphic range: Late Eocene (Tinguirirican) | |
Type | Geological formation |
Overlies | Quebrada Santo Domingo Formation |
Lithology | |
Primary | Sandstone, red beds, tuff |
Location | |
Coordinates | 28.5°S 68.8°W |
Approximate paleocoordinates | 30.6°S 60.6°W |
Region | Mendoza Province, Argentine Northwest |
Country | Argentina |
Extent | Precordillera |
Type section | |
Named for | Laguna Brava |
It was formerly thought that the formation was of Triassic age.[3]
References
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