Analysis of a marine core from M’Clintock Channel, NWT: micromorphological and geochemical evidence for mass flows and ice shelf grounding
Recent work in the Canadian Arctic Archipelago (CAA) has suggested that marine-based deglaciation following the Last Glacial Maximum (LGM) was marked by the formation of extensive ice shelves in the inter-island channels, with further deglaciation resulting in a series of large ice shelf readvances....
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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MacEwan Open Journals
2019
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Online Access: | https://journals.macewan.ca/studentresearch/article/view/1810 |