Within geomacromolecules,
such as kerogen, asphaltene, and solid
bitumen, other compounds can be adsorbed and even occluded as free
molecules. The occluded components have been well preserved by the
macromolecular structure, and retain some of the primary geochemical
information. In this work we try to probe the geochemical evolution
of occluded hydrocarbons inside geomacromolecules associated with
the geomacromolecule evolution from kerogen → asphaltene →
solid bitumen. The results show that occluded hydrocarbons can be
transferred steadily from kerogen → asphaltene → solid
bitumen. Later-evolved geomacromolecules not only inherit the occluded
hydrocarbons from the former ones, but can also occlude some new free
molecules. Occluded hydrocarbons are subject to a relatively independent
thermal evolution, whereas the evolution of adsorbed molecules is
constrained by other factors besides thermal stress. Elucidation of
the geochemical evolution of occluded hydrocarbons inside geomacromolecules
will be helpful in oil (bitumen)–source correlation, identification
of mixed-source reservoirs, and characterization of hydrocarbon accumulation
and evolution.