Smoothed abundance of bulk mineralogy in the Cenozoic sediments of core CRP-3

The mineralogy of the lower Oligocene (to possibly upper Eocene) sediments of core CRP-3 drilled on the continental shelf of McMurdo Sound in the Ross Sea, Antarctica, has been examined by the X-ray diffraction method. Quartz, plagioclase K- feldspar and pyroxene are the most important non-clay mine...

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Bibliographic Details
Main Authors: Neumann, M, Ehrmann, Werner
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.57817
https://doi.org/10.1594/PANGAEA.57817