Polar heterocompounds in oil-
source
rock
correlation
studies
Christian Hallmann, Geological Institute,
The purpose of this study is to monitor carbazole distributions in oils,
source
rock
extracts and
source
rock
pyrolysates in order to establish a
molecular marker in the polar petroleum fraction, indicative for
source
facies.
The Cooper/Eromanga Basins,
source
rocks. Their highly similar
source
facies precludes a detailed oil-
source
rock
correlation. Jurassic-sourced oils can be discriminated from Paleozoic-sourced
oils by aromatic hydrocarbon biomarkers that were produced exclusively by
post-Triassic Araucariacea conifers. Preliminary results indicate that
distribution patterns of nitrogen-containing carbazole compounds allow a
precise discrimination of all three
source
rock
units (Jurassic/Permian/pre-Permian)
present in the study area.
We plan to subject immature, unaltered
source
rock
samples from all three aforementioned
source
units to hydrous pyrolysis.
Pyrolysates will be analysed for carbazole and hydrocarbon biomarker
compositions by molecular geochemistry. Molecular compositions of hydrous
pyrolysates are comparable to those of naturally generated oils. Pyrolysates,
however, are unaffected by secondary alteration and oil mixing processes. Thus
they should exhibit pristine end-member oil compositions. If the molecular
composition of
source
rock
pyrolysates supports our earlier observations, we
can provide a powerful new tool for correlating oils and
source
rocks based on
heterocompound compositions.
The anticipated results will not only enhance our
understanding of the Cooper/Eromanga Basin oil play, but also aid in future
exploration activities, elsewhere. Furthermore, the finding of facies-dependent
markers in polar petroleum fractions is a positive motivation for further
research into the geochemistry of petroleum heterocompounds.