Uplift and tilting of the Shackleton Range in East Antarctica driven by glacial erosion and normal faulting

Unravelling the long-term evolution of the subglacial landscape of Antarctica is vital for understanding past ice sheet dynamics and stability, particularly in marine-based sectors of the ice sheet. Here we model the evolution of the bedrock topography beneath the Recovery catchment, a sector of the...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Paxman, Guy J. G., Jamieson, Stewart S. R., Ferraccioli, Fausto, Bentley, Michael J., Forsberg, René, Ross, Neil, Watts, Anthony B., Corr, Hugh F. J., Jordan, Tom A.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/e31ffcd4-e9a0-480d-8d86-1f4265490774
https://doi.org/10.1002/2016JB013841
https://backend.orbit.dtu.dk/ws/files/132029133/Uplift_and_tilting_of_the_Shackleton_Range_in_East_Antarctica.pdf