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...

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Bibliographic Details
Published in:Journal of the mineralogical society of korea
Main Authors: Ha, Sangbeom, Khim, Boo-Keun, Cho, Hyen Goo, Colizza, Ester
Format: Article in Journal/Newspaper
Language:Korean
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/11368/2941790
https://doi.org/10.9727/jmsk.2018.31.1.1