Ground ice, organic carbon and soluble cations in tundra permafrost soils and sediments near a Laurentide ice divide in the Slave Geological Province, Northwest Territories, Canada
The central Slave Geological Province is situated 450–650 km from the presumed spreading centre of the Keewatin Dome of the Laurentide Ice Sheet, and it differs from the western Canadian Arctic, where recent thaw-induced landscape changes in Laurentide ice-marginal environments are already abundant....
Published in: | The Cryosphere |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2020
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-14-4341-2020 https://noa.gwlb.de/receive/cop_mods_00054863 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00054514/tc-14-4341-2020.pdf https://tc.copernicus.org/articles/14/4341/2020/tc-14-4341-2020.pdf |