Geochemistry of heavy minerals from the Arctic and Lomonosov Ridge off Greenland

The sediment deposited in the Arctic Ocean is transported by sea ice and icebergs, which are controlled by the Arctic surface circulations. Several cores from the central Arctic, the Lomonosov Ridge north of Greenland and the Morris Jesup Rise contain a distinct grayish, ice rafted debris (IRD)-rich...

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Bibliographic Details
Main Author: Chao, Weng-si
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Arctic
Arctic Ocean
Greenland
Dammed Lake
Morris Jesup Rise
Foraminifera*
Iceberg*
Lomonosov Ridge
Sea ice
Siberia
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.870973
https://doi.org/10.1594/PANGAEA.870973

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