Binfeng Cao , Xiaorong Luo , Richard H. Worden , Xiangzeng Wang , Yonghong He , Xiangyang Qiao , Likuan Zhang , Yuhong Lei , Jinsong Zhou , Chao Deng
{"title":"Contrasting diagenetic evolution and hydrocarbon charge of tight gas sandstones in the lower Permian Shanxi Formation, southeastern Ordos Basin, China","authors":"Binfeng Cao , Xiaorong Luo , Richard H. Worden , Xiangzeng Wang , Yonghong He , Xiangyang Qiao , Likuan Zhang , Yuhong Lei , Jinsong Zhou , Chao Deng","doi":"10.1016/j.jseaes.2024.106330","DOIUrl":null,"url":null,"abstract":"<div><div>Reservoir quality of, and gas production rates from, tight sandstones in the Lower Permian Shanxi Formation vary greatly across the Yan’an Gas Field, southeastern Ordos Basin, China. Effective reservoirs are significant for the economic success of tight gas exploration and production. This study examined the relationships between diagenetic evolution, porosity reduction and hydrocarbon charge to reveal the formation and distribution of effective reservoirs in this field. The sandstones are very fine- to coarse-grained, quartz arenites, sub-litharenites and litharenites. The significant variations in the texture and mineralogical composition of the sandstones exert major controls on diagenetic heterogeneity and pore distribution. Five petrofacies (petrofacies-A to -E) are classified. The various petrofacies experienced contrasting diagenetic evolution and petroleum charge histories. The medium- to coarse-grained, quartz arenites (petrofacies-A) and sub-litharenites (petrofacies-C) experienced less ductile compaction and cementation and extensive grain dissolution, and remained relatively porous before early hydrocarbon emplacement. When peak gas generation and migration occurred, petrofacies-A and -C still had moderate porosity and were able to be charged. On the contrary, the fine-grained, tuffaceous quartz arenites (petrofacies-B), ductile grain-rich sandstones (petrofacies-D) and tightly carbonate-cemented sandstones (petrofacies-E) experienced limited diagenetic alterations with ductile compaction or carbonate cementation predominating and leading to extensive loss of porosity during eodiagenesis. Petrofacies-B, -D and -E had low porosity before early petroleum charge. Petrofacies-A and -C therefore constitute the only effective reservoir rocks of tight reservoirs of the Shanxi Formation. This study indicates that petrofacies is useful for reservoir characterization and modeling in the Yan’an Gas Field and other tight gas fields worldwide.</div></div>","PeriodicalId":50253,"journal":{"name":"Journal of Asian Earth Sciences","volume":"276 ","pages":"Article 106330"},"PeriodicalIF":2.7000,"publicationDate":"2024-09-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Asian Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1367912024003250","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Reservoir quality of, and gas production rates from, tight sandstones in the Lower Permian Shanxi Formation vary greatly across the Yan’an Gas Field, southeastern Ordos Basin, China. Effective reservoirs are significant for the economic success of tight gas exploration and production. This study examined the relationships between diagenetic evolution, porosity reduction and hydrocarbon charge to reveal the formation and distribution of effective reservoirs in this field. The sandstones are very fine- to coarse-grained, quartz arenites, sub-litharenites and litharenites. The significant variations in the texture and mineralogical composition of the sandstones exert major controls on diagenetic heterogeneity and pore distribution. Five petrofacies (petrofacies-A to -E) are classified. The various petrofacies experienced contrasting diagenetic evolution and petroleum charge histories. The medium- to coarse-grained, quartz arenites (petrofacies-A) and sub-litharenites (petrofacies-C) experienced less ductile compaction and cementation and extensive grain dissolution, and remained relatively porous before early hydrocarbon emplacement. When peak gas generation and migration occurred, petrofacies-A and -C still had moderate porosity and were able to be charged. On the contrary, the fine-grained, tuffaceous quartz arenites (petrofacies-B), ductile grain-rich sandstones (petrofacies-D) and tightly carbonate-cemented sandstones (petrofacies-E) experienced limited diagenetic alterations with ductile compaction or carbonate cementation predominating and leading to extensive loss of porosity during eodiagenesis. Petrofacies-B, -D and -E had low porosity before early petroleum charge. Petrofacies-A and -C therefore constitute the only effective reservoir rocks of tight reservoirs of the Shanxi Formation. This study indicates that petrofacies is useful for reservoir characterization and modeling in the Yan’an Gas Field and other tight gas fields worldwide.
期刊介绍:
Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance.
The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.