Ice-Rafted Detritus Events in the Arctic During the Last Glacial Interval, and the Timing of the Innuitian and Laurentide Ice Sheet Calving Events

Ice-rafted detritus (IRD) layers in the Arctic Ocean not only indicate the source of this detrital sediment, but give insights into the ice drift and ice sheet history. Detrital sand-sized FE oxide mineral grains that are matched to precise sources using the microprobe chemical fingerprint of each g...

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Bibliographic Details
Main Authors: Darby, Dennis A., Zimmerman, Paula
Format: Article in Journal/Newspaper
Language:unknown
Published: ODU Digital Commons 2008
Subjects:
Kya
Online Access:https://digitalcommons.odu.edu/oeas_fac_pubs/18
https://doi.org/10.1111/j.1751-8369.2008.00057
https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1026/viewcontent/Darby_2008_Ice_rafted_detritus.pdf