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...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2001
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.57817 https://doi.org/10.1594/PANGAEA.57817 |