Enhanced images and new models of the Wilkes Subglacial Basin help constrain the variability in geological boundary conditions for the East Antarctic Ice Sheet
The Wilkes Subglacial Basin (WSB) is a huge tectonic feature formed by Cenozoic lithospheric flexure coupled with Mesozoic to Cenozoic extension localised in sub-basins (Paxman et al., 2019, JGR). The deep northern WSB underlies the catchments of the Matusevich, Cook, Ninnis and Mertz glaciers that...
Main Authors: | , , , , , |
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Other Authors: | , , , , , |
Format: | Conference Object |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | http://hdl.handle.net/11567/1024196 |