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

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...

Полное описание

Библиографические подробности
Главные авторы:	Watts, A, Paxman, G, Jamieson, S, Ferraccioli, F, Bentley, M, Forsberg, R, Ross, N, Corr, H, Jordan, T
Формат:	Journal article
Опубликовано:	Wiley 2017

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