Colorado Basin, Argentina

The Colorado Basin (Spanish: Cuenca del Colorado) is a sedimentary basin located in northeastern Argentina. The basin stretches across an area of approximately 180,000 square kilometres (69,000 sq mi), of which 37,000 square kilometres (14,000 sq mi) onshore in the southern Buenos Aires Province and the easternmost Río Negro Province extending offshore in the South Atlantic Ocean.

For other uses, see Colorado Basin.
Colorado Basin
Cuenca del Colorado
Location of the basin in Argentina
Coordinates41°30′S 61°00′W
EtymologyColorado River
Country Argentina
State(s)Buenos Aires & Río Negro Provinces
CitiesBahía Blanca, Viedma
Characteristics
On/OffshoreBoth
BoundariesVentania High (N)
Argentina Basin (E)
Rawson/Río Negro High (S)
San Rafael Block (W)
Part ofSouth Atlantic rift basins
Area~180,000 km2 (69,000 sq mi)
Hydrology
Sea(s)South Atlantic
River(s)Río Negro & Colorado Rivers
Geology
Basin typePassive margin on rift basin
PlateSouth American
OrogenyBreak-up of Pangea
AgeEarly Cretaceous-Quaternary
StratigraphyStratigraphy
Field(s)none

The basin comprises a sedimentary succession dating from the Permian (pre-rift stage) and Early Cretaceous (rift stage) to the Quaternary, representing the passive margin tectonic phase of the basin history. The Mesozoic rifting in the basin resulted from the break-up of Pangea and the formation of the South Atlantic. Long hiatuses exist in the succession.

The basin is of paleontological significance for hosting fossiliferous stratigraphic units dating to the Late Miocene. The Arroyo Chasicó Formation defines the Chasicoan South American land mammal age and contains a rich mammal and other vertebrate fauna. The contemporaneous Cerro Azul Formation has provided fossil rodents, armadillos and opossums. The Middle to Late Miocene Gran Bajo del Gualicho Formation contains vertebrate fossils of the cetacean Preaulophyseter gualichensis. The Río Negro Formation has provided fossils of the glyptodont Plohophorus figuratus. The Permian succession in the basin has provided flora microfossils.

Contrasting with the South Atlantic passive margin basins to the north (Santos Basin in southern Brazil) and south; Golfo San Jorge and Austral Basins, the Colorado Basin does not produce hydrocarbons. Exploration for petroleum started in the 1940 with the drilling of two onshore wells and several onshore and offshore wells have been drilled in the 1960s, 1970s and 1990s. The main source rocks are found in the Permian succession, with reservoir rocks the Colorado Formation. Seals are provided by the Early Paleocene Pedro Luro Formation.

Description
View of Viedma and Carmen de Patagones, separated by the Río Negro

The Colorado Basin stretches across an approximate area of 180,000 square kilometres (69,000 sq mi) with about 37,000 square kilometres (14,000 sq mi) onshore, underlying the southernmost Buenos Aires Province and the southeasternmost Río Negro Province. Cities inside the basin are Bahía Blanca and Carmen de Patagones in Buenos Aires Province and Viedma in Río Negro Province, the earliest founded city in Patagonia. The onshore part of the basin is crossed by the eponymous Colorado and Río Negro rivers. Surrounding the Río Negro, many salt lakes are present in the basin.[1]

Some authors group the basin together with the Claromecó Basin to the north.[2] The offshore part of the Colorado Basin laterally correlates with and gradually ranges into the sub-parallel Salado Basin and the deeper offshore Argentina Basin.[3][4] The offshore extension of the basin into neighboring basins led to different definitions of its area, some authors use a surface area of 125,000 square kilometres (48,000 sq mi).[5]

The Colorado Basin is bound to the north by the Ventania High,[6] Sierra de la Ventana,[7] or Sierras Australes,[2] separating the basin from the Claromecó Basin, and to the south by the Rawson,[8] or Río Negro High.[9] In the northwest, the basin grades into the Macachín Basin and the western boundary is formed by the San Rafael Block.[9]

Basin evolution
Pangea in the Permian (~250 Ma). The Colorado Basin experiences glaciations and a marine transgressive phase in the south polar region.
Sketch of the paleogeographic situation of South America during the Late Cretaceous and Early Paleogene, roughly 85 to 63 Ma. The Colorado Basin, located north of the North Patagonian Massif in the South Gondwanan Province (grey), is exposed and eroded during the Maastrichtian.

The basin started forming in the Middle to Late Jurassic with the break-up of Pangea and the formation of the Southern Atlantic.[10] The main rifting took place in the Early Cretaceous.[5] The pre-rift sequence of the basin comprises the Pennsylvanian Lolén Formation of the Ventana Group,[11] and the Sauce Grande, Piedra Azul, Bonete and Tunas Formations of the Pillahuincó Group,[2] dating to the Permian.[12] During the late Paleozoic, the Colorado Basin was located in the south polar region, causing a sequence of glacial deposits in the basin. These deposits were mostly sourced from the African basin, the Karoo and Kalahari Basins. The Early Permian sediments are characterized by the presence of diamictites. A transgression in the Permian led to the deposition of the Piedra Azul Formation.[13] The succession contains several hiatuses, dating to the Triassic and Early Jurassic, Albian and Paleogene.[14]

The early Mesozoic succession is missing, and the main rifting phase happened in the Barremian and Aptian, around 120 million years ago, represented in the Fortín Formation.[15] The post-rift sag stage dates to the early Late Cretaceous leading to the deposition of the alluvial and fluvial sediments of the Colorado Formation.[14] The drift stage is represented by the Pedro Luro Formation.[14] The later Cenozoic succession is characteristic of a terrestrial passive margin setting and comprises the Paleocene Elvira,[14] Middle Miocene Barranca Final Formation,[16] and the Middle to Late Miocene Gran Bajo de Gualicho Formation.[17] This formation in most of the basin is overlain by the Río Negro Formation.[18] The Late Miocene succession in the westernmost area of the basin is represented by the Arroyo Chasicó and eolian Cerro Azul Formations,[19] cropping out in the northern onshore part of the basin.[20] This sequence is covered by the Late Miocene to Early Pliocene eolian and fluvial Río Negro Formation,[21][22] outcropping in a thin band along the eponymous river.[1]

Stratigraphy
AgeGroupFormationEnvironmentTectonic regimeMaximum thicknessPetroleum geologyNotes
QuaternaryalluviumPassive margin
Early PlioceneRío NegroEolian & fluvial480 m (1,570 ft)[21][22]
Late Miocene
Chasicoan-HuayquerianCerro AzulEolian180 m (590 ft)[19][23]
ChasicoanArroyo ChasicóFloodplain[24]
MayoanGran Bajo de GualichoShallow marine57 m (187 ft)[17]
Laventan
Colloncuran
Friasian
Santacrucian
Mid MioceneBarranca FinalMarine300 m (980 ft)[16]
OligoceneHiatus
Late Eocene
Middle EoceneElvira[14]
Early EoceneHiatus
Late Paleocene
Early PaleocenePedro LuroDriftSeal[14]
MaastrichtianHiatus
CampanianColoradoAlluvial & fluvialSagReservoir[14]
Santonian
Coniacian
Turonian
Cenomanian
AlbianHiatus
AptianFortínSyn-riftReservoir
Source		[15]
Barremian
Middle JurassicHiatus
Early Jurassic
Triassic
Late PermianPillahuincóTunasPre-rift1,500 m (4,900 ft)Source[2]
Early PermianBoneteSource[2]
Piedra Azul[2]
Sauce Grande[2]
PennsylvanianVentanaLolénBasement[11]

Paleontological significance
Neocavia pampeana of the Cerro Azul Formation

The Miocene formations cropping out onshore have provided a rich mammal fauna. The Arroyo Chasicó Formation is the defining formation for the Late Miocene Chasicoan South American land mammal age, ranging from 10 to 9 million years ago.[25] The formation contains many mammal species, birds and reptiles.[26] The Cerro Azul Formation contains fossils of the rodents Chasichimys bonaerense,[27] Neocavia pampeana,[28] Reigechimys plesiodon and R. simplex,[29] the armadillos Chasicotatus ameghinoi,[23] and Macrochorobates scalabrinii,[27] and the opossum Zygolestes tatei,[30] among other mammals. The Río Negro Formation has provided fossils of the glyptodont Plohophorus figuratus.[31]

The marine Gran Bajo de Gualicho Formation contains many bivalve, gastropod and echinoid fossils,[32] and the cetacean Preaulophyseter gualichensis.[33] The Eocene succession in boreholes of the basin has provided many species of dinoflagellates,[34] and in the Permian sequence 131 species of spores, algae, funghi and pollen were registered.[35]

Petroleum exploration

Contrary to other Southern Atlantic marginal basins, as the Golfo San Jorge and Austral Basins to the south, and Santos Basin of Brazil to the north, the Colorado Basin is not producing hydrocarbons. The first wells in the northern onshore part of the basin were drilled in 1946 (Pedro Luro-1) and 1948 (Ombucta-1) by YPF. Another phase of onshore exploration happened in the 1960s, with seven wells drilled by Shell.[36] Offshore drilling started in 1970 by Hunt Oil and after seismic acquisition in the 1970s by YPF,[37] some wells were drilled in 1977 by the same company. Renewed exploration started in the mid-1990s with several wells drilled by Union Texas and Shell.[38] The offshore Cruz del Sur x-1 well provided oil shows of 39° API.[39]

See also

References
  1. Geologic Map Hojas 4163-II/IV & I/III, 2006
  2. Balarino, 2012, p.344
  3. Pucci, 2006, p.17
  4. ENARSA, s.a., p.3
  5. ENARSA, s.a., p.2
  6. Daners et al., 2016, p.285
  7. Balarino, 2009, p.20
  8. ENARSA, s.a., p.1
  9. Barredo & Stinco, 2010, p.60
  10. Geologic Map Hojas 3963-III & IV, 2009, p.42
  11. Balarino, 2009, p.24
  12. Balarino, 2009, p.22
  13. Balarino, 2009, p.23
  14. ENARSA, s.a., p.4
  15. Barredo & Stinco, 2010, p.52
  16. Geologic Map Hojas 3963-III & IV, 2009, p.39
  17. Reichler, 2010, p.192
  18. Reichler, 2010, p.183
  19. Visconti et al., 2010, p.259
  20. Geologic Map Hojas 3963-III & IV, 2009, p.5
  21. Pérez, 2010, p.7
  22. Geologic Map Hojas 3963-III & IV, 2009, p.8
  23. Scillato Yané et al., 2010, p.51
  24. Zárate et al., 2007
  25. Chasicoan at Fossilworks.org
  26. Arroyo Chasicó at Fossilworks.org
  27. Verzi et al., 2008
  28. Madozzo Jaén et al., 2018, p.250
  29. Sostillo et al., 2014
  30. Goin et al., 2000, p.108
  31. Punta Bermeja at Fossilworks.org
  32. Reichler, 2010, pp.191-192
  33. Buono, 2013, p.36
  34. Daners et al., 2016, p.293
  35. Balarino, 2012, p.343
  36. Rossello, 2016, p.175
  37. ENARSA, s.a., p.8
  38. ENARSA, s.a., p.5
  39. Pucci, 2006, p.18

Bibliography
General
Geologic maps
Arroyo Chasicó Formation
Cerro Azul Formation
Gran Bajo del Gualicho Formation
Río Negro Formation
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