Clay mineralogy of Cape Roberts sediment cores

The clay mineral assemblages of the ca. 1600 m thick Cenozoic sedimentary succession recovered at the CRP-1, CRP-2/2A and CRP-3 drill sites off Cape Roberts on the McMurdo Sound shelf, Antarctica, were analysed in order to reconstruct the palaeoclimate and the glacial history of this part of Antarct...

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Bibliographic Details
Main Authors: Ehrmann, Werner, Setti, Massimo, Marinoni, L
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2005
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738196
https://doi.org/10.1594/PANGAEA.738196