The Upper Carboniferous
sandstone reservoir is a vital replacement
area for natural gas exploration in Ordos Basin. In this study, 157
Jinci sandstone samples were selected to conduct a series of experiments
and analyses. The reservoir material composition and pore structure
analysis shows that the lithology of the reservoir is mainly quartz
arenite, followed by sublithic arenite. The detrital particles are
mainly quartz (69–97.5%), followed by rock fragments (0.1–24.5%),
and the content of feldspar is less than 0.01%. The cement consists
of siliceous material, clay minerals, and carbonate, with averages
of 2.34, 5.96, and 1.81%, respectively. Three types of pore-throat
structures (HPMI curve: types 1, 2, and 3) are identified in the Jinci
sandstone reservoir, corresponding to different pore-throat radius
distributions (RCP curves: types A, B, and C). The study of the factors
affecting reservoir pore structure and its internal mechanism shows
that the reservoir pore-throat combination, affecting the reservoir
performance, is mainly controlled by deposit composition and the subsquent
diagenetic modification. A higher rigid particle content and an appropriate
amount of siliceous cementation (2–10%) would lead to resistance
of the compaction, in favor of the preservation of primary intergranular
pores. When the content of ductile particles is more than 3%, the
original intergranular pores tend to be substantially reduced. The
deposit composition of sandstone controls the preservation of residual
intergranular pores by affecting the intensity of compaction and dissolution
controlling the amount and type of cementation. Compared with dissolution-subjected
quartz arenites, the sublithic arenites are characterized by a common
occurrence of altered kaolinite and recrystallized illite, which would
destroy the reservoir property. The early diagenetic carbonate cementation,
as well as the strong siliceous cementation in “sedimentary
quartz arenite”, are unfavorable to the formation of high-quality
reservoirs. Then, on the basis of the characteristics of various diagenesis
and their interaction and internal relationship, the diagenetic sequence
and diagenetic-pore evolution patterns of different types of reservoirs
were established. Finally, according to the lithological characteristics
and the diagenetic-controlled pore-throat evolution patterns of different
types of reservoirs, the reservoir quality in the study area was predicted.