The compound classes and biomarker compositions of immature Jinghan crude o
il asphaltenes and their potential respective source rock kerogens have bee
n investigated by chemolysis. The C-S-, C-O-, and C-arom-C-bound appendages
have been liberated by Ni2B reduction, BBr3 hydrolysis, and ruthenium-ions
-catalyzed oxidation. Measured were the saturate, aromatic, and polar (+ as
phaltene) compound classes and the homologous series of hydrocarbon biomark
ers: n-alkanes, regular isoprenoids, steranes, 4-methylsteranes, hopanes, g
ammacerane, their monocarboxylic acid derivatives, and alpha-omega-di-n-alk
anoic acids. The nature and distribution of the biomarkers in shallower dep
ths reveals a good correlation between the crude oil asphaltene and the ker
ogen, manifesting a crude oil-source rock relationship. In deeper strata, t
he correlation is less convincing but there is no indication of incompatibi
lity. The biomarker composition confirms the immaturity of this deposit, an
d the huge (53%) yields of C-S plus C-O bond cleavage products from the hig
h-sulfur asphaltene set this type of asphaltene aside from mature crude oil
asphaltenes. Also, the biomarker composition. points to a strongly reducin
g, lacustrine depositional environment for this deposit.