Organic carbon chemistry of ODP Hole 151-909C (Table 1)
Organic-rich sediments were recognized in early Miocene strata from the Norwegian-Greenland Sea during ODP Leg 151. Three organic-geochemical subunits were distinguished in Hole 909C using detailed organic-geochemical and microscopic analyses. TOC (up to 3 wt%), HI (up to 200 mg HC/g TOC), and d13Co...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2002
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.746742 https://doi.org/10.1594/PANGAEA.746742 |