(Table 1) Organic geochemical results for the samples from DSDP Hole 41-368

DSDP site 41–368 in the eastern Atlantic represents an unusual locality, where the behaviour of a short column of organic-rich shale can be studied in relation to the steep thermal gradient imposed by basaltic intrusions. This study indicates that the dominant effects on the measured parameters of t...

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Bibliographic Details
Main Authors: Simoneit, Bernd R T, Brenner, Shmuel, Peters, K E, Kaplan, I R
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
41-368
Calcium carbonate
Carbon
organic
total
Deep Sea Drilling Project
Depth
bottom/max
relative
sediment/rock
top/min
uncorrected
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Glomar Challenger
Hydrocarbon yield
S2 per unit sediment mass
Hydrogen/Carbon ratio
Kerogen
Ro
Leg41
Nitrogen/Carbon ratio
North Atlantic/CONT RISE
Number
Pristane/Phytane ratio
Sample code/label
δ13C
δ Deuterium
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.770141
https://doi.org/10.1594/PANGAEA.770141
Description
Summary:DSDP site 41–368 in the eastern Atlantic represents an unusual locality, where the behaviour of a short column of organic-rich shale can be studied in relation to the steep thermal gradient imposed by basaltic intrusions. This study indicates that the dominant effects on the measured parameters of the organic matter were thermal and that compositional variations in the original matter were minor in comparison.

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