Antarctic Crustal Motions Driven by Present Day Ice Sheet Evolution and by Isostatic Memory of the Last Glacial Maximum
作者： Erik R. Ivins , Thomas S. James
DOI:
关键词: Deglaciation 、 Ice stream 、 Geophysics 、 Ice sheet 、 Isostatic depression 、 Post-glacial rebound 、 Geology 、 Glacier 、 Last Glacial Maximum 、 Ice-sheet model
摘要: Detectable crustal motion and secular rate of change solid-surface gravity may be produced by the Earth's response to present day and/or past ice mass changes in Antarctica.
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