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...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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ODU Digital Commons
2008
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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 |