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The Influence of 5000 year-old and Younger Glacial Mass Variability on Present-day Crustal Rebound in the Antarctic Peninsula

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dc.contributor.author Ivins, E. en_US
dc.contributor.author Raymond, C. en_US
dc.contributor.author James, T. en_US
dc.date.accessioned 2004-11-10T16:18:24Z
dc.date.available 2004-11-10T16:18:24Z
dc.date.issued 1999 en_US
dc.identifier.citation Earth, Space Planets en_US
dc.identifier.citation USA en_US
dc.identifier.clearanceno 99-2190 en_US
dc.identifier.uri http://hdl.handle.net/2014/37405
dc.description.abstract Much of the late-Quaternary ice sheet history in the northern hemisphere is now relatively well-constrained, with the total contributions to eustatic sea level change from North America and Eurasia estimated at roughly 60 (+-12) and 20 (+-7) m, respectively, and with deglaciation bracketed at 22 to 8.5 kyr BP. en_US
dc.format.extent 1504019 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other GPS geodesy glacial rebound sea-level change earth structure en_US
dc.title The Influence of 5000 year-old and Younger Glacial Mass Variability on Present-day Crustal Rebound in the Antarctic Peninsula en_US


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