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 th...
| Main Authors: | , , , , , , , , |
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| Format: | Journal article |
| Published: |
Wiley
2017
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