Golfo San Jorge Basin

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Golfo San Jorge Basin
Cuenca del Golfo San Jorge
Iconos de la energia.JPG
Oil well near the port city of Comodoro Rivadavia
Map showing the location of Golfo San Jorge Basin
Map showing the location of Golfo San Jorge Basin
Location of the basin in Argentina
Coordinates45°00′S 67°50′W / 45.000°S 67.833°W / -45.000; -67.833
EtymologySan Jorge Gulf
LocationSouthern South America
RegionPatagonia
Country Argentina
State(s)Chubut, Santa Cruz
CitiesComodoro Rivadavia
Characteristics
On/OffshoreBoth
BoundariesNorth Patagonian Massif, Deseado Massif, Andes
Part ofSouthern Atlantic rift basins
Area170,000 km2 (66,000 sq mi)
Hydrology
Sea(s)South Atlantic
River(s)Chico River
Lake(s)Lake Musters and Lake Colhué Huapí
Geology
Basin typeRift
PlateSouth American
OrogenyOpening of the South Atlantic
AgeEarly Jurassic-Pleistocene
StratigraphyStratigraphy
Field(s), , ,
Photograph of the first oil well in Comodoro Rivadavia

The Golfo San Jorge Basin (Spanish: Cuenca del Golfo San Jorge) is a hydrocarbon-rich sedimentary basin located in eastern Patagonia, Argentina. The basin covers the entire San Jorge Gulf and an inland area west of it, having one half located in Santa Cruz Province and the other in Chubut Province. The northern boundary of the basin is the North Patagonian Massif while the Deseado Massif forms the southern boundary of the basin. The basin has largely developed under condition of extensional tectonics, including rifting.[1]

The basin is of paleontological significance as it hosts six out of 22 defining formations for the SALMA classification, the geochronology for the Cenozoic used in South America.

At the center of the basin accumulated sediments reach more than 8,000 metres (26,000 ft) of thickness. Oil was first discovered in 1907 and over the years it has become the second most productive hydrocarbon basin in Argentina after Neuquén Basin.[1]

Stratigraphy[]

The stratigraphy of the Golfo San Jorge Basin covers the following units:[1][2][3]

Unit Age
bold is SALMA type
Tectonic regime Depositional environment Thickness
(m)
Petroleum geology
Pleistocene Glacio-fluvial 40
Mayoan
Santacrucian Fluvio-deltaic 200
Shallow marine 280

 
Colhuehuapian Fluvio-lacustrine 120
Deseadan
Tinguirirican
Divisaderan Lacustrine 42
Mustersan

Casamayoran Fluvio-lacustrine 44
Riochican Fluvial 42
Itaboraian
Peligran 25
Peligran Shallow marine-deltaic-fluvial 200 Petroleum reservoir
Tiupampan
Lago Colhué Huapí Maastrichtian
Campanian
Fluvial


Bajo Barreal
Laguna Palacios
Santonian
Aptian
Late sag Deltaic
Fluvio-lacustrine
4000+


Bajo Barreal
Alluvial-fluvial-lacustrine

Fluvio-lacustrine

Early sag 1500+ Source rock and petroleum reservoir
Neocomian Late rift Fluvio-lacustrine 560
Lacustrine 1700+ Source rock

Cerro Carnerero Mid-Late Jurassic Early rift Volcaniclastic 1300+
Early Jurassic Pre-rift Shallow marine 700+
Basement Paleozoic

See also[]

References[]

  1. ^ a b c Sylwan, Caudio A. (2001). "Geology of the Golfo San Jorge Basin, Argentina". Journal of Iberian Geology. 27: 123–157. Retrieved 4 December 2015.
  2. ^ Raigemborn et al., 2010, p.243
  3. ^ Cortés, 1986, p.49

Bibliography[]

General
Cretaceous

Paleogene[]

Andesitas Huancache Formation
Bororó Formation
Casamayor Formation
Las Flores Formation
Koluel Kaike Formation
Peñas Coloradas Formation
Río Chico Group
Salamanca Formation

Neogene[]

Río Mayo Formation
  • Ecosteguy, Leonardo; Carlos Dal Molín; Mario Franchi; Silvena Guena; Omar Lapido, and Adolfo Genini. 2003. Hoja Geológica 4772-II Lago Buenos Aires, 1–80. Instituto de Geología y Recursos Minerales, . Accessed 2018-09-10.
Sarmiento Formation & Colhué Huapí Member

Further reading[]

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