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...
| Glavni autori: | , , , , |
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| Format: | Članak |
| Jezik: | English |
| Izdano: |
Taylor & Francis Group
2022-12-01
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| Serija: | Arctic, Antarctic, and Alpine Research |
| Teme: | |
| Online pristup: | https://www.tandfonline.com/doi/10.1080/15230430.2022.2096425 |