Mineral and isotopic (Nd, Sr) signature of fine-grained deglacial and Holocene sediments from the Mackenzie Trough, Arctic Canada

Dolomites in Arctic Ocean sediments are widely attributed to erosion and transport of sediments from northern Canada and Greenland. Coarse-grained dolomite-rich ice-rafted debris is often linked to iceberg transport, but the origin of fine-grained dolomite is less well constrained. A presumed source...

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Bibliographic Details
Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Henrik Swärd, Per Andersson, Robert Hilton, Christoph Vogt, Matt O’Regan
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2022
Subjects:
Online Access:https://doi.org/10.1080/15230430.2022.2096425
https://doaj.org/article/a2f873e6455f407a8223f6ea986f003b