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Sea-level change through the last glacial cycle: geophysical, glaciological and palaeogeographic consequences

Lambeck, Kurt


Sea-level fluctuations in recent geological time are primarily the result of climate change with its associated glacial cycles. Observations reveal a complex spatial and temporal pattern of change that contains a record of the timing of the glacial cycles, of the locations and dimensions of the past ice sheets, of the earth's response function to long-term loading and of tectonic events. By analysing data from different locations and different epochs these different contributions can be...[Show more]

CollectionsANU Research Publications
Date published: 2004
Type: Journal article
Source: Academie des Sciences Comptes Rendus: Geoscience
DOI: 10.1016/j.crte.2003.12.017


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