The Scotia Sea, mixed biosiliceous-terrigenous sediments deposited from the Antarctic Circumpolar Current.

John Howe, Carol J Pudsey

Research output: Chapter in Book/Report/Conference proceedingChapter

Original languageEnglish
Title of host publicationDeep-Water Contourite Systems
PublisherGeological Society of London
Pages325-338
Number of pages14
Edition22
Publication statusPublished - 2002

Cite this

Howe, J., & Pudsey, C. J. (2002). The Scotia Sea, mixed biosiliceous-terrigenous sediments deposited from the Antarctic Circumpolar Current. In Deep-Water Contourite Systems (22 ed., pp. 325-338). Geological Society of London.