IAS Post Graduate Grant Scheme Report - 2nd Session 2013. Sedimentary evolution of the southwestern Scotia Sea (Antarctica): tectonic and palaeoceanographic implications

Lara F. Pérez

IAS Post Graduate Grant Scheme Report - 2^nd Session 2013. Sedimentary evolution of the southwestern Scotia Sea (Antarctica): tectonic and palaeoceanographic implications

Publikation: Bidrag til tidsskrift › Artikel › Formidling

Resumé

The Scotia Sea is located to the east of the Drake Passage, which is in between the southern tip of South America and the northern end of the Antarctic Peninsula (Fig. 1). It is usually considered the last barrier for complete establishment of circum-Antarctic deepwater flow and the determination of the Antarctic Continent isolation (Lawver et al., 1992).

Originalsprog	Engelsk
Sider (fra-til)	24-30
Antal sider	7
Tidsskrift	International Association of Sedimentologists Newsletter
Udgave nummer	255
Status	Udgivet - feb. 2015
Udgivet eksternt	Ja

Programområde

Programområde 3: Energiressourcer

Adgang til dokumentet

https://www.sedimentologists.org/repository/newsletters/4477dea4701011e9a9231255Licens: Ikke-specificeret

Citationsformater

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abstract = " The Scotia Sea is located to the east of the Drake Passage, which is in between the southern tip of South America and the northern end of the Antarctic Peninsula (Fig. 1). It is usually considered the last barrier for complete establishment of circum-Antarctic deepwater flow and the determination of the Antarctic Continent isolation (Lawver et al., 1992).",

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AB - The Scotia Sea is located to the east of the Drake Passage, which is in between the southern tip of South America and the northern end of the Antarctic Peninsula (Fig. 1). It is usually considered the last barrier for complete establishment of circum-Antarctic deepwater flow and the determination of the Antarctic Continent isolation (Lawver et al., 1992).

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EP - 30

JO - International Association of Sedimentologists Newsletter

JF - International Association of Sedimentologists Newsletter

IS - 255