Wikipedia / Magallanes Basin
Wikipedia / Magallanes Basin
The Magallanes Basin or Austral Basin is a major sedimentary basin in southern Patagonia. The basin covers a surface of about and has a NNW-SSE oriented shape. The basin is bounded to the west by the Andes mountains and is separated from the Malvinas Basin to the east by the Río Chico-Dungeness High. The basin evolved from being an extensional back-arc basin in the Mesozoic to being a compressional foreland basin in the Cenozoic. Rocks within the basin are Jurassic in age and include the Cerro Toro Formation. Three ages of the SALMA classification are defined in the basin; the Early Miocene Santacrucian from the Santa Cruz Formation and Friasian from the Río Frías Formation and the Pleistocene Ensenadan from the La Ensenada Formation.
The Magallanes Basin contains most of Chile's coal reserves dwarfing those found in the Arauco Basin or around Valdivia (e.g. Catamutún, Mulpún). Its coals are lignitic to sub-bituminous.
Stratigraphy
Aysén Basin
The northwesternmost reaches of the basin form a sub-basin known as Aysén Basin or Río Mayo Embayment. From top to bottom the fill the basin is:
Late Cretaceous volcanic rock
Divisadero Group (Aptian to Albian)
Coihaique Group (Late Jurassic to Aptian)
Northwestern basin
In the Argentinian parts of the basin, the following formations have been registered from north to south:
Cerro Boleadoras Formation (Santacrucian)
Río Jeinemeni Formation (Colhuehuapian)
Mata Amarilla Formation (Albian to Santonian)
Divisadero Group (Aptian to Albian)
Río Belgrano Formation (Barremian to Aptian)
El Tranquilo Group (Late Triassic)
South-central basin
Pinturas Formation (Santacrucian)
La Irene Formation (Maastrichtian)
Monte Chico Formation (Maastrichtian)
Cerro Cazador Formation (Campanian to Maastrichtian)
Alta Vista Formation (Early to Middle Campanian)
Tobífera Formation (Late Jurassic)
Tierra del Fuego
See also
Notes
References
Bibliography
Cretaceous
Neogene
Further reading