Anatomy of Labrador Sea Heinrich layers
Heinrich layers (H-layers) are distinct, decimetre to centimetre thick layers of ice-rafted debris (IRD) that were deposited in the North Atlantic during the Late and middle Pleistocene. H-layers (H-layers) are characterized by high detrital carbonate and low foraminifera contents. In the Labrador S...
Published in: | Marine Geology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier Science Bv
2016
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00341/45214/44639.pdf https://archimer.ifremer.fr/doc/00341/45214/44640.csv https://archimer.ifremer.fr/doc/00341/45214/44641.pdf https://doi.org/10.1016/j.margeo.2016.05.019 https://archimer.ifremer.fr/doc/00341/45214/ |