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...

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Bibliographic Details
Published in:Marine Geology
Main Authors: Hesse, Reinhard, Khodabakhsh, Saeed
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science Bv 2016
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/