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The Magallanes Basin or Austral Basin is a major sedimentary basin in southern Patagonia. The basin covers a surface of about 170,000 to 200,000 square kilometres (66,000 to 77,000 sq mi) 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 . 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 .

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  • Cuenca de Magallanes (es)
  • Magallanes arroa (eu)
  • Magallanes Basin (en)
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  • La cuenca de Magallanes es una cuenca sedimentaria que llega por el norte hasta la Patagonia superior en Chile. Las rocas dentro de ella se derivan del período Jurásico, e incluye la formación Cerro Toro. Esta cuenca ofrece la oportunidad de estudiar numerosas formas de vida de fósiles antiguos y otros elementos naturales prehistóricos debido a la estratificación sedimentaria profunda.​ Tiene una extensión de 250km norte-sur y constituye la mayor reserva de carbón del país.​ (es)
  • Magallanes arroa edo Austral arroa arro sedimentarioa da, iparraldetik Txileko goiko Patagoniara iristen dena. Bere barnean dauden arrokak Jurasiko arotik eratorriak dira, eta Cerro Toro formazioa barne hartzen du. Arro honek antzinako fosilen bizimodu ugari eta historiaurreko beste elementu natural batzuk aztertzeko aukera ematen du estratifikazio sedimentario sakona dela eta. Ipar-hegoaldera 250 km luzatzen da eta herrialdeko erreserba handiena da. (eu)
  • The Magallanes Basin or Austral Basin is a major sedimentary basin in southern Patagonia. The basin covers a surface of about 170,000 to 200,000 square kilometres (66,000 to 77,000 sq mi) 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 . 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 . (en)
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  • Magallanes or Austral Basin (en)
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