Geochemistry and mineralogy of selected carbonaceous claystones at DSDP Hole 76-534
Four dominant depositions of carbonaceous claystones are recognized to have occurred during the early Aptian to middle Albian at Site 534. There are correlations of stable isotope ratios with organic carbon content and of clay content with clay mineralogy of the samples. Almost all organic carbon in...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1983
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.809830 https://doi.org/10.1594/PANGAEA.809830 |