Ice rafte debris of ODP Hole 178-1101A, supplement to: Cowan, Ellen A (2001): Identification of the glacial signal from the Antarctic Peninsula since 3.0 Ma at Site 1011 in a continental rise sediment drift. In: Barker, PF; Camerlenghi, A; Acton, GD; Ramsay, ATS (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 178, 1-22

Sediment drifts on the continental rise west of the Antarctic Peninsula received fine-grained sediment and ice-rafted debris (IRD) directly from the continental shelf and thus indirectly record the history of West Antarctic glaciation. Site 1101 contains a 218-m-thick, nearly continuous section exte...

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Bibliographic Details
Main Author: Cowan, Ellen A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735542
https://doi.pangaea.de/10.1594/PANGAEA.735542