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Cuyo Basin

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Not to be confused with Cuyania.
Cuyo Basin
Cuenca Cuyana
Map showing the location of Cuyo BasinMap showing the location of Cuyo BasinLocation of the basin in Argentina
Coordinates34°15′S 68°34′W / 34.250°S 68.567°W / -34.250; -68.567
EtymologyCuyo River
Country Argentina
State(s)Mendoza, San Juan
CitiesMendoza
Characteristics
On/OffshoreOnshore
BoundariesAndes
Part ofAndean foreland basins
Area~30,000 km (12,000 sq mi)
Hydrology
River(s)Cuyo River
Geology
Basin typeForeland basin
PlateSouth American
OrogenyAndean
AgeTriassic-Pliocene
StratigraphyStratigraphy
Field(s)Tupungato

Cuyo Basin (Spanish: Cuenca Cuyana) is a sedimentary basin in Mendoza Province, western Argentina. The Cuyo Basin has a NNW-SSE elongated shape and is limited to the west by the Sierra Pintada System and to the east by the Pampean pericraton. To the north the basin reaches the area around the city of Mendoza.

Description

The Cuyo Basin has an approximate area of 30,000 square kilometres (12,000 sq mi). It has two major sub-basins: Cacheuta (Spanish: Subcuenca Cacheuta) in the north and Alvear (Spanish: Subcuenca Alvear) in the south. The northern fringes of Cacheuta sub-basin reaches into San Juan Province. The basin existed already during the Triassic but its current shape is derivative of the Andean orogeny.

The basin originated as a rift basin in the context of extensional tectonics and crustal thinning that followed the Paleozoic Gondwanide orogeny.

Stratigraphy

The stratigraphy of the Cuyo Basin comprises the following formations:

Age
bold is SALMA type
Group Formation Lithologies Depositional environment Notes
Pleistocene Tunuyán
Mio-Pliocene
Huayquerian
Huayquerías Mudstones, sandstones, tuff Fluvial
Miocene Mogotes Alluvial
Miocene La Pilona Shales and sandstones Alluvial
Middle Miocene
Laventan
Mariño Sandstones Alluvial and eolian
Late Oligocene
Deseadan
Early Oligocene Hiatus
Priabonian
Bartonian
Divisaderan
Divisadero Largo Fluvial
Lutetian Papagayos Fluvial
Early Eocene Hiatus
Paleocene
Late Cretaceous
Early Cretaceous Punta de las Bardas Basalts Volcanic
Late Jurassic
Barrancas Sandstones and conglomerates Alluvial to fluvial
Rhaetian Uspallata Río Blanco Fluvial-deltaic
Norian
Carnian Cacheuta Black shales Lacustrine
Potrerillos Tuffs, conglomerates, sandstones, shales Alluvial to fluvial
Ladinian Cerro de las Cabras Mudstones and conglomerates
Anisian
Olenekian Río Mendoza Volcaniclastic conglomerates
Induan
Late Permian Choiyoi Group
Carboniferous Hiatus
Devonian
Early Paleozoic Cuyania

See also

Notes and references

Notes

  1. These tectonics are not related to the break-up of Gondwana later in the Mesozoic.

References

  1. ^ "Cuenca Cuyana". Secretaría de Energía (in Spanish). Government of Argentina. Retrieved 30 November 2015.
  2. Zencich et al., 2008, p.110
  3. ^ Spalletti et al., 2008, p.270
  4. Yrigoyen, 1993
  5. Garrido et al, 2017, p.51
  6. ^ Zencich et al., 2008, p.112
  7. ^ Spalletti et al., 2008, p.269
  8. Spalletti et al., 2005
  9. ^ Finney, 2007
  10. ^ Keller et al., 1998

Bibliography

General
Divisadero Largo Formation
Huayquerías Formation
Mariño Formation

Further reading

Major South American geological features
Tectonic plates
Cratons and shields
Structures undergoing subduction
Faults and shear zones
Rifts and grabens
Sedimentary basins
Orogenies
Metallogenetic provinces
Volcanism
Volcanic provinces
Hotspots
Sedimentary basins of Argentina
Onshore & offshore
Northern Region
Patagonia
Cuyo Basin is located in Argentina
Offshore
Sources      Álvarez Pontoriero, O.; Giménez, M.; Braitemberg, C.; Martínez, M.; Ruíz, F.; Introcaso, A.; Guspí, F. (2011). Principales cuencas sedimentarias de Argentina, interpretadas mediante Gravimetría Satelital. VIII Congreso de Exploración y Desarrollo de Hidrocarburos. pp. 13–20. Retrieved 2018-08-28.
      Mapa de cuencas sedimentarias (Map). YPF. p. 1. Retrieved 2018-08-28.
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