Collón Curá Formation

The Collón Curá Formation (Spanish: Formación Collón Curá) is a Middle Miocene fossiliferous geological formation of the southern Neuquén Basin in northwestern Patagonia and the western Cañadón Asfalto Basin of central Patagonia, Argentina. The formation crops out from the southern Neuquén Province, the western Río Negro Province to the northern Chubut Province.

Collón Curá Formation
Stratigraphic range: Langhian-earliest Tortonian
(typically Colloncuran)
~
Area around the Comallo railway, with outcrops of this formation
TypeGeological formation
Sub-unitsTobaceo Las Bayas & Pilcaniyeú Ignimbrite Members
UnderliesCaleufú Formation & Chenqueniyeu Basalt (Neuquén Basin)
El Mirador, Río Negro Formation & alluvium (Cañadón Asfalto Basin)
OverliesCerro Bandera, Huitrera & Cerro Petiso Formations, crystalline basement (Neuquén Basin)
Ñirihuau, Lefipán & La Pava Formations (Cañadón Asfalto Basin)
ThicknessUp to 300 m (980 ft)
Lithology
PrimaryTuff, sandstone
OtherSiltstone, marl, limestone, calcareous concretions, pumice
Location
Coordinates40.0°S 70.8°W / -40.0; -70.8
Approximate paleocoordinates40.6°N 66.4°W / 40.6; -66.4
RegionNeuquén, Río Negro & Chubut Provinces
CountryArgentina
ExtentCañadón Asfalto & Neuquén Basins
Type section
Named forCollón Curá River & Estancia Collón Curá
Named byYrigoyen
LocationLácar Department
Year defined1969
Coordinates40°04′56.6″S 70°51′55.3″W
RegionNeuquén Province
Country Argentina
Thickness at type section50 m (160 ft)

Outcrop locations of the Collón Curá Formation

The formation, with a maximum thickness of 300 metres (980 ft), comprises tuffs and sandstones with minor siltstones, marls and limestones, deposited in a fluvial, deltaic and shallow to deep lacustrine environment in small basins separated by faults. The formation dates from the Langhian to earliest Tortonian epochs of the Middle to Late Miocene, typically Colloncuran.

The Collón Curá Formation is named after Estancia Collón Curá (1 on the map in the infobox) along the Collón Curá River (2), a tributary of the Limay River in the Río Negro watershed, and lends its name to the Colloncuran, one of the South American land mammal ages. The formation has provided many fossils of mammals, reptiles, among others the snake Waincophis australis, and the largest terror bird Kelenken guillermoi. The rodent Galileomys colloncurensis and the typothere Protypotherium colloncurensis were named after the formation.

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