Marine
Influence
on Coal-An Analytical Challenge
C. F. K. Diessel, D. J. Curry, L. C. Gammidge, R. Rigby
Coal seams which have been affected by sea water during their formation,
differ from other coals in petrographic, chemical, and physical properties.
These differences have consequences for the coal's utilisation, hydrocarbon
generation parameters, and usefulness as marker beds, for example in onshore
sequence stratigraphy. These characteristics are controlled by the duration and
timing of marine
influence
in relation to peat accumulation. There are two basic
scenarios:
1. Post-depositional (epigenetic) marine
influence
-peat accumulation is part
of the terrestrialisation process (upward shoaling of a parasequence) and the
vertical succession is from eutrophic to oligotrophic conditions. Accumulation
ceases when the mire is drowned by a marine transgression and the peat inundated
by sea water and covered by marine sediments.
2. Syndepositional (syngenetic) marine influences-plants grow and peat accumulates in contact with sea water which gradually inundates the mire and covers it with marine sediments. The vertical succession is from oligotrophic to eutrophic conditions.
While the two cases differ in their biochemical environments, they experience
the same post-depositional conditions, and develop similar, but not necessarily
identical marine signatures. In peats and most lignites, botanical evidence
commonly indicates mire conditions and the onset of marine
influence
. However,
these indicators are obliterated with increasing coal rank and age, and the
evidence for syn- versus postdepositional marine
influence
becomes equivocal. A
wide range of chemical and petrographic
analyses
is often required to solve this
problem. Using the Permian Greta Seam of the Sydney Basin as an example, this
paper discusses some of the analytical techniques which may be used to establish
the relative timing of marine
influence
on coal.
AAPG Search and Discovery Article #91020©1995 AAPG Annual Convention, Houston, Texas, May 5-8, 1995