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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Bibliographic Details
Main Author: Troyer-Riel, Robert
Format: Article in Journal/Newspaper
Language:unknown
Published: MacEwan Open Journals 2019
Subjects:
Online Access:https://journals.macewan.ca/studentresearch/article/view/1810