Neuquén Group

Short description: Group of geologic formations in Argentina

Neuquén Group
Stratigraphic range: Early Cenomanian-Early Campanian
~98–79 Ma

PreЄ

Almost the whole extent of the Neuquén Group is exposed between Lake Los Barreales and the bend of the Neuquén River in the center of this photo.To the lower left of the lake, a swath of light yellowish sandstones of the group's Huincul Formation are visible.

Type| Group
Sub-units|  Río Colorado Subgroup
Anacleto Formation
Bajo de la Carpa Formation

Río Neuquén Subgroup
Plottier Formation
Portezuelo Formation

Río Limay Subgroup
Lisandro Formation
Huincul Formation
Candeleros Formation
Underlies| Malargüe Group
Allen Formation
Overlies| Lohan Cura Formation
Thickness| 500 m (1,600 ft)
Location
Coordinates|  [ ⚑ ] : 38°30′S 68°42′W﻿ / ﻿38.5°S 68.7°W﻿ / -38.5; -68.7
Paleocoordinates|  [ ⚑ ] 44°24′S 47°12′W﻿ / ﻿44.4°S 47.2°W﻿ / -44.4; -47.2
Region| Río Negro, Neuquén & Mendoza Provinces
Country| Argentina
Extent| Neuquén Basin
Type section
Named for| Neuquén

Neuquén Group (Argentina)

The Neuquén Group is a group of geologic formations found in Argentina . Rocks in the Neuquén Group fall within the Cenomanian to early Campanian stages of the Late Cretaceous Period. It overlies the older Lohan Cura Formation and is itself overlain by the younger Allen Formation of the Malargüe Group, separated from both by unconformities, dated to 98 and 79 Ma respectively.[1]

## Contents

* 1 Description
* 1.1 Subdivision
* 2 See also
* 3 References
* 3.1 Bibliography

## Description

Deposits have been located in the provinces of Río Negro, Neuquén, and Mendoza. Although several different types of environments are represented in various sections of the Neuquén Group, the dominant regime is alluvial deposition. Many dinosaur and other fossil types have been discovered in these sediments.

### Subdivision

There are seven formations within the Neuquén Group. These are divided into three subgroups named after major rivers in the area. In some works, the subgroups themselves are treated as formations and what usually is considered to be the formations as mere members of these. However, particularly in the Río Limay Subgroup, the formations are clearly composed of very distinct rock layers.[2]

Neuquén Group strata, ordered from youngest to oldest

* Río Colorado Subgroup (Santonian to early Campanian)
* Anacleto Formation (early Campanian)
* Bajo de la Carpa Formation (Santonian)
* Río Neuquén Subgroup (late Turonian to Coniacian)
* Plottier Formation (late Coniacian ?to early Santonian)
* Sierra Barrosa Formation (middle Coniacian)
* Los Bastos Formation (early Coniacian)
* Portezuelo Formation (late Turonian to earliest Coniacian)
* Cerro Lisandro Formation (middle Turonian)
* Río Limay Subgroup (Cenomanian to early Turonian)
* Lisandro Formation (middle to late Turonian)
* Huincul Formation (late Cenomanian to early Turonian)
* Candeleros Formation (early Cenomanian)

South of Añelo, on the road between Lake Los Barreales and the Neuquén River are views on the successively younger formations, starting with the Lisandro Formation to the northwest of Lake Los Barreales, and finally crossing the Anacleto Formation about 35 kilometres (22 mi) down the road near the eastern tip of the lake. The older strata are exposed south of Lake Los Barreales.[2]

## See also

* List of fossil sites
* Angostura Colorada Formation, Campanian to Maastrichtian fossiliferous formation of the North Patagonian Massif
* Asencio Formation, Campanian to Maastrichtian fossiliferous formation of the Paraná Basin
* Bajo Barreal Formation, Cenomanian to Turonian fossiliferous formation of the Golfo San Jorge Basin
* Bauru Group, Coniacian to Maastrichtian fossiliferous group of the Paraná Basin
* Cerro Fortaleza Formation, Cenomanian fossiliferous formation of the Austral Basin
* Colorado Formation, Campanian to Maastrichtian fossiliferous formation of the Colorado Basin
* Lago Colhué Huapí Formation, Campanian to Maastrichtian fossiliferous formation of the Golfo San Jorge Basin
* Los Blanquitos Formation, Campanian fossiliferous formation of the Salta Basin
* Mata Amarilla Formation, Albian to Santonian fossiliferous formation of the Austral Basin
* Santa Marta Formation, Santonian to Campanian fossiliferous formation of northern Antarctica

## References

1. ↑ Leanza et al., 2004, p. 63
2. ↑ 2.0 2.1 Sánchez et al. (2006)

### Bibliography

* Leanza, H.A.; Apesteguia, S.; Novas, F.E.; De la Fuente, M.S. (2004). "Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages". Cretaceous Research 25: 61-87. https://www.researchgate.net/publication/257047651_Cretaceous_terrestrial_beds_from_the_Neuquen_Basin_Argentina_and_their_tetrapod_assemblages. Retrieved 2019-02-16.
* Sánchez, María Lidia; Heredia, Susana; Calvo, Jorge O. (2006). "Paleoambientes sedimentarios del Cretácico Superior de la Formación Plottier (Grupo Neuquén), Departamento Confluencia, Neuquén (Sedimentary paleoenvironments in the Upper Cretaceous Plottier Formation (Neuquen Group), Confluencia, Neuquén)". Revista de la Asociación Geológica Argentina 61: 3-18. https://www.researchgate.net/publication/262615949_Paleoambientes_sedimentarios_del_Cretacico_Superior_de_la_Formacion_Plottier_Grupo_Neuquen_Departamento_Confluencia_Neuquen. Retrieved 2019-02-16.

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