Te. Ruble et al., New insights on the Green River petroleum system in the Uinta basin from hydrous pyrolysis experiments, AAPG BULL, 85(8), 2001, pp. 1333-1371
The Tertiary Green River petroleum system in the Uinta basin generated abou
t 500 million bbl of recoverable, high pour-point, paraffinic crude oil fro
m lacustrine source rocks. A prolific complex of marginal and open-lacustri
ne source rocks, dominated by carbonate oil shales containing up to 60 wt.
% type I kerogen, occur within distinct stratigraphic units in the basin. P
etroleum generation is interpreted to originate from source pods in the bas
al Green River Formation buried to depths greater than 3000 m along the ste
eply dipping northern margin of the basin. Producing fields in the Altamont
-Bluebell trend have elevated pore-fluid pressures approaching 80% of litho
static pressure and are completed in strata where open fractures provide pe
rmeability. Active hydrocarbon generation is one explanation for the origin
of the overpressured reservoirs.
In this study, experiments were undertaken to examine the mechanisms of hyd
rocarbon generation and accumulation in the Uinta basin. We combined analys
es of representative source rocks from the entire Green River stratigraphic
section with detailed laboratory simulation experiments using both open- a
nd closed-system pyrolysis. This information provides new insights on lacus
trine source rock lithofacies, gas-oil-source rock correlations, hydrocarbo
n generation kinetics, and basin modeling. The results show that the basal
Green River Formation contains a unique type I source facies responsible fo
r generation of paraffinic crude oils. The classic type I oil shales in the
upper Green River Formation correlate well with low-maturity aromatic-asph
altic samples. We determined kinetic parameters for the source rocks and us
ed them to develop basin models for hydrocarbon generation. The models show
that hydrous pyrolysis kinetic parameters are more consistent with the nat
ural data in terms of predicted timing and extent of oil generation as comp
ared to models using Rock-Eval kinetics.