Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica

Measurements of the loss or gain of ice mass from large ice sheets are presently achieved through satellite-based techniques such as GRACE (Gravity Recovery and Climate Experiment). The accuracy of these satellite-based measurements to changes in modern ice sheet mass depends on our knowledge of pre...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: White, DA, Fink, D
Format: Article in Journal/Newspaper
Language:English
Published: AGU Publications 2015
Subjects:
Online Access:http://apo.ansto.gov.au/dspace/handle/10238/8138
https://doi.org/10.1002/2013jf002870