Sea level change through the last glacial cycle
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Description
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
Collections | ANU Research Publications |
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Date published: | 2001 |
Type: | Journal article |
URI: | http://hdl.handle.net/1885/89436 |
Source: | Science |
DOI: | 10.1126/science.1059549 |
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File | Description | Size | Format | Image |
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01_Lambeck_Sea_level_change_through_the_2001.pdf | 480.79 kB | Adobe PDF | Request a copy | |
02_Lambeck_Sea_level_change_through_the_2001.pdf | 527.62 kB | Adobe PDF | Request a copy |
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