“…The full pore size distribution curves of diagenetic facies A, C, and D all show a single-peak pattern, and the pore sizes corresponding to the peak positions decrease in order, with 0.1–0.2 μm, 0.07–0.1 μm, and 0.007–0.13 μm, respectively, where the diagenetic facies A is mainly dominated by residual intergranular pores due to the high content of brittle minerals. Previous studies have shown that the presence of brittle minerals makes the reservoir more difficult to be compacted under the same stress conditions . The brittle minerals effectively balance the strength of compaction, so the pore structure of diagenetic facies A is characterized by a relatively uniform pore size distribution, and the original pore morphology is well preserved.…”