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Sea level change through the last glacial cycle

Chappell, John; Lambeck, Kurt


Sea level change during the Quaternary is primarily a consequence of the cyclic growth and decay of ice sheets, resulting in a complex spatial and temporal pattern. Observations of this variability provide constraints on the timing, rates, and magnitudes

CollectionsANU Research Publications
Date published: 2001
Type: Journal article
Source: Science
DOI: 10.1126/science.1059549


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