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Establishing the pattern of Holocene-LGM changes in sediment contributions from Antarctica to the Southern Ocean
Entry ID:
Goldstein_OPP_0088054
Summary
Abstract:
Terrigenous clastic sediments are brought to the ocean from continental sources
via rivers, ice and wind, and distributed within the ocean by surface and deep currents. By investigating long-lived radioactive decay systems, the sediment sources can be traced and the geological history of those sources can be delineated. The sediments deposited along the Antarctic coast represent a mixture of ... ![]() Geographic Coverage
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Spatial coordinates
Location Keywords
Science Keywords
ISO Topic Category
Data Center
Personnel
Creation and Review Dates
DIF Creation Date:
2005-04-26
Last DIF Revision Date:
2005-12-21
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