Although abundant unconventional oil resources have been
discovered
in conglomerate and sandstone reservoirs in rift basins, the mechanism
of differential pore evolution in conglomerates and sandstone reservoirs
within different secondary structural zones of rift basins is not
yet clear. The pore structures of conglomerate and sandstone reservoirs
in the distinct secondary structural zones in the Chezhen Sag were
quantified in three dimensions using high-resolution microcomputed
tomography (micro-CT). Thin section and scanning electron microscopy
observations were used to investigate the differential evolution mechanisms
of conglomerate and sandstone reservoirs. Micro-CT analysis of the
pore structures of conglomerate and sandstone reservoirs revealed
that sandstone reservoirs are superior to conglomerate reservoirs
with regard to the pore number and pore connectivity and that sandstone
reservoirs are more heterogeneous than conglomerate reservoirs. Triangles
dominate the pore and pore throat geometries of sandstone and conglomerate
reservoirs, while the sandstone reservoir pores are more regular than
conglomerate reservoir pores. The depositional environment, mineral
composition, and diagenetic intensity jointly control the quality
of the reservoirs. Because of the lengthy transportation distance
of their parent rocks, the compositional maturity and sorting behavior
of sandstone reservoirs in depression and gentle slope zones are better
than those of conglomerate reservoirs in steep slope zones, and thus
sandstone reservoirs have a higher initial porosity than conglomerate
reservoirs. The rapid compaction experienced by the conglomerate reservoirs
in steep slope zones in their early stages creates a closed diagenetic
environment, making it difficult to effectively improve reservoir
porosity through dissolution. However, the widely developed microfractures
in the reservoirs provide channels for fluid migration, promote the
development of dissolution pores, and form a tight reservoir dominated
by secondary pores. With weak compaction and an open diagenetic environment,
the primary pores in sandstone reservoirs in the gentle slope zone
are preserved in large quantities. Meanwhile, dissolution expands
the secondary pores of the reservoir, resulting in a high-quality
reservoir having both primary and secondary pores. In addition, an
approach based on primary, secondary, and total porosity was proposed
in the study to efficiently evaluate reservoir quality and identify
reservoir evolution mechanisms.