Geochemical and petrologic comparison of solid bitumens with various origin
s from reservoirs in Zaire, Canada and Kazakhstan were studied to provide i
nsight into their formation processes and their physical and chemical prope
rties. Results of this study can help develop methods for treatment and rem
oval of solid bitumen, and evaluating producibility of associated hydrocarb
on fluids. Characterization of these solid bitumens reveals a wide range in
quantity and composition of extractables (soluble material) and in solid b
itumen reflectance, which indicate significant differences in formation pro
cesses, hydrocarbon source and thermal maturity. The Zaire and Kazakhstan s
amples represent end members of the spectrum of solid bitumens studied. Sol
id bitumens from the Motoba Field, Zaire, are highly extractable and low in
thermal maturity (0.2-0.3% bitumen reflectance). Reservoir mixing of a Cre
taceous lacustrine sourced oil and a Tertiary marine sourced oil of differe
nt thermal maturities appears to be responsible for their formation. In con
trast, solid bitumens from the Tengiz Field, Kazakhstan, are characterized
by their extremely low extractables, high bitumen reflectance (>1%)and low
atomic H/C ratios(< 1.0). Thermal alteration is an important process in the
formation of these highly mature bitumens (pyrobitumen). Petrographic text
ures of the solid bitumens complement their geochemical characterization an
d provide insight into their origin. Solid bitumens from the Mitsue Field,
Canada, which has been under miscible gas flood for sometime, are intermedi
ate in the yields of extractables and thermal maturity (similar to 0.7% bit
umen reflectance). The origin of the solid bitumen may have been gas deasph
altening originating from geological processes rather than from the recover
y process. A combination of pyrolysis gas chromatography and petrology (bit
umen reflectance and occurrence) provides distinction between production an
d geologically induced reservoir solid bitumen. (C) 1998 Published by Elsev
ier Science Ltd. All rights reserved.