Geophysical constraints on mantle viscosity and its influence on Antarctic glacial isostatic adjustment
Glacial isostatic adjustment (GIA) is the process by which the solid Earth responds to past and present-day changes in glaciers, ice caps, and ice sheets. This thesis focuses on vertical crustal motion of the Earth caused by GIA, which is influenced by several factors including lithosphere thickness...
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Other Authors: | , |
Format: | Thesis |
Language: | English |
Published: |
2012
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Online Access: | http://hdl.handle.net/1828/4001 |