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

Lara F. Pérez

Research output: Contribution to journal › Article › Communication

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).

Original language	English
Pages (from-to)	24-30
Number of pages	7
Journal	International Association of Sedimentologists Newsletter
Issue number	255
Publication status	Published - Feb 2015
Externally published	Yes

Programme Area

Programme Area 3: Energy Resources

Access to Document

https://www.sedimentologists.org/repository/newsletters/4477dea4701011e9a9231255Licence: Unspecified

Cite this

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

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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journal = "International Association of Sedimentologists Newsletter",

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publisher = "International Association of Sedimentologists",

number = "255",

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Y1 - 2015/2

N2 - 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).

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).

M3 - Article

SN - 2294-4931

SP - 24

EP - 30

JO - International Association of Sedimentologists Newsletter

JF - International Association of Sedimentologists Newsletter

IS - 255