Diagenetic history and reservoir quality of tight sandstones: A case study from Shiqianfeng sandstones in upper Permian of Dongpu Depression, Bohai Bay Basin, eastern China

The upper Permian Shiqianfeng sandstones, located in the Dongpu Depression, Bohai Bay Basin, China, are fluvio-lacustrine deposits and have high content of pore-filling volcanic dust (average 7.93 vol %). This study focuses on diagenetic processes and reservoir quality of the tight sandstones based on different lithofacies. An integrated approach, such as core observation, X-ray diffraction, scanning electron microscopy, cathode luminescence, stable isotope analysis of carbon and oxygen compositions, electron microprobe analysis and fluid inclusion analysis, were utilized. The tight sandstones consist of subarkose and lithic subarkose, and have undergone significant diagenetic events, including compaction, quartz cementation, carbonate cementation (mainly calcite and ferrocalcite) and formation of authigenic clay minerals (i.e., chlorite rims, kaolinite and mixed-layer illite/smectite). The volcanic dust altered with increase of burial depth, resulting in the production of abundant silicic materials and depletion of metallic ions (i.e., Fe2+, Mg2+, Ca2+ and Mn2+). This process formed subhedral micro-quartz, pore-filling authigenic quartz, smectite and chlorite rims during the early diagenetic stage. Early-phase carbonate cements (calcite/ferrocalcite) occurred in several samples. They were also influenced by volcanic dust alteration, resulting in intrusive of Fe2+ and high contents of Mn2+ (average 12.5 mol %).