Geochemistry on sediment core CRP-1 (Table 1)
The CRP-1 core penetrated 148 m of Quaternary and lower Miocene glacigenic sediments. This material complements the Eocene trhough Miocene strata that was cored previously at CIROS-1, 70 km to the south. The paleoclimatic records of CRP-1 and CIROS-1 have been examined by calculating the Chemical In...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1998
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.54732 https://doi.org/10.1594/PANGAEA.54732 |