Clay mineralogy of sediment core CRP-1

Clay mineral assemblages in lower Miocene and Quaternary sediments recovered at the CRP-1 drillsite, McMurdo Sound shelf, Antarctica, were analysed in order to reconstruct source areas of the sediments and late Cenozoic Antarctic icedynamics. The assemblages are dominated by smectite, illite and chl...

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Bibliographic Details
Main Author: Ehrmann, Werner
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.54627
https://doi.org/10.1594/PANGAEA.54627