Katabatic wind influence on meltwater supply to fuel glacier-substrate interactions at grounding line, Terra Nova Bay, Antarctica
The co-isotopic composition, both in δD and in δ18O, of interbedded debris-rich and clear ice layers, thought to have been formed at the grounding line of Hells Gate Ice Shelf, indicates freezing by a double-diffusion effect between continental meltwater and sea water within a subglacial sediment. A...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1999
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Subjects: | |
Online Access: | http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173121 https://dipot.ulb.ac.be/dspace/bitstream/2013/173121/3/doi_156751.pdf |