Origin of Clay Minerals of Core RS14-GC2 in the Continental Slope to the East of the Pennell-Iselin Bank in the Ross Sea, Antarctica
A gravity core (RS14-C2) was collected at site RS14-C2 in the continental slope to the east of Pennell-Isellin Bank of the Ross Sea (Antarctica) during PNRA XXIX (Rosslope II Project) Expedition. In order to trace the sediment source, magnetic susceptibility (MS), sand fraction, and clay mineral com...
Published in: | Journal of the mineralogical society of korea |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | Korean |
Published: |
2018
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Subjects: | |
Online Access: | http://hdl.handle.net/11368/2941790 https://doi.org/10.9727/jmsk.2018.31.1.1 |