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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Bibliographic Details
Main Author: Darlington, Andrea
Other Authors: James, Thomas Sinclair, Spence, George D.
Format: Thesis
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/1828/4001