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...

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Bibliographic Details
Main Authors: Knies, Jochen, Mann, Ute
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
AGE
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.746742
https://doi.org/10.1594/PANGAEA.746742