Large-scale englacial folding and deep-ice stratigraphy within the West Antarctic Ice Sheet
It has been hypothesized that complex englacial structures identified within the East Antarctic and Greenland ice sheets are generated by: (i) water freezing to the ice-sheet base, evolving under ice flow; (ii) deformation of ice of varying rheology; or (iii) entrainment of basal material. Using ice...
Main Authors: | , , |
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Format: | Text |
Language: | English |
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2019
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Online Access: | https://doi.org/10.5194/tc-2019-245 https://www.the-cryosphere-discuss.net/tc-2019-245/ |