1. 中国地质大学(武汉)资源学院
2. 中国地质大学(武汉)构造和油气资源教育部重点实验室
3. 中国石油塔里木油田公司勘探开发研究院
纸质出版:2025
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姜潇俊, 史玲玲, 莫涛, 等. 深层-超深层致密砂岩储层特征及物性差异成因:以库车坳陷博孜地区巴什基奇克组为例[J]. 地质科技通报, 2025,44(3):151-164.
姜潇俊, 史玲玲, 莫涛, et al. 深层-超深层致密砂岩储层特征及物性差异成因:以库车坳陷博孜地区巴什基奇克组为例[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 151-164.
姜潇俊, 史玲玲, 莫涛, 等. 深层-超深层致密砂岩储层特征及物性差异成因:以库车坳陷博孜地区巴什基奇克组为例[J]. 地质科技通报, 2025,44(3):151-164. DOI: 10.19509/j.cnki.dzkq.tb20230567.
姜潇俊, 史玲玲, 莫涛, et al. 深层-超深层致密砂岩储层特征及物性差异成因:以库车坳陷博孜地区巴什基奇克组为例[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 151-164. DOI: 10.19509/j.cnki.dzkq.tb20230567.
库车坳陷博孜地区在8 000 m以深仍发育优质储层且高产工业气流,但其巴什基奇克组致密砂岩储层物性平面上存在着明显的差异。为明确此类储层发育的特征,降低深层-超深层油气勘探的风险,基于测录井、铸体薄片、高压压汞及PVT相图等实验分析结果,探讨了致密砂岩储层特征及物性差异成因。研究结果表明:博孜地区巴什基奇克组储层岩石类型为中-细粒岩屑长石砂岩和长石岩屑砂岩,碳酸盐胶结物含量平面分布差异大;中-细粒砂岩储层原始孔隙度介于32.4%~38.1%,颗粒间压实强度相似,以点-线接触为主;南部储层平均孔隙度为8.6%,平均渗透率为3.4×10
-3
μm
2
;中部储层平均孔隙度为6.53%,平均渗透率为0.65×10
-3
μm
2
;北部储层平均孔隙度为4.9%,平均渗透率为0.62×10
-3
μm
2
;南部储层储集空间以原生粒间孔为主,北部和中部储层以残余粒间孔和溶蚀孔隙为主;南部储层较北部和中部储层孔喉结构更好。博孜地区砂岩储层物性受沉积、成岩和构造作用(裂缝)共同控制,其中碳酸盐胶结是后期储层物性改造的主要因素。超压、烃类流体充注及裂缝发育影响了碳酸盐胶结,进而造成储层物性差异。超压较强,油气充注时间较早及裂缝充填较低导致博孜南部储层物性好于北部与中部。
Du Hao,Shi Wanzhong,Wang Ren,Maselli Vittorio,Liang Jinqiang,Ren Jinfeng,Kuang Zengui,He Yulin,Xu Litao,Zuo Tingna.Dynamic evolution of gas hydrate systems affected by magmatism and Quaternary mass-transport deposits in the Qiongdongnan Basin, South China Sea, and implications for the global carbon cycle[J].Marine Geology,2024.
Qin Shuo,Wang Ren,Shi Wanzhong,Geng Feng,Luo Fusong,Li Gupan,Li Jiarui,Zhang Xiao,Ostadhassan Mehdi.Integrated controls of tectonics, diagenesis and sedimentation on sandstone densification in the Cretaceous paleo-uplift settings, north Tarim Basin[J].Geoenergy Science and Engineering,2024.
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Lai Jin,Li Dong,Bai Tianyu,Zhao Fei,Ai Yong,Liu Hongkun,Cai Deyang,Wang Guiwen,Chen Kangjun,Xie Yuqiang.Reservoir quality evaluation and prediction in ultra-deep tight sandstones in the Kuqa depression, China[J].Journal of Structural Geology,2023.
Liu Kai,Wang Ren,Shi Wanzhong,Travé Anna,Martín-Martín Juan Diego,Baqués Vinyet,Qi Rong,Lin Jianwei,Ye Hui.Diagenetic controls on reservoir quality and heterogeneity of the Triassic Chang 8 tight sandstones in the Binchang area (Ordos Basin, China)[J].Marine and Petroleum Geology,2022.
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State Key Laboratory of Petroleum Resources and Prospecting, ChinaUniversity of Petroleum, Beijing, 102249, China,College of Geosciences, China University of Petroleum, Beijing,102249, China,State Key Laboratory of Petroleum Resources and Prospecting, ChinaUniversity of Petroleum, Beijing, 102249, China,Research Institute of Petroleum Exploration and Development,PetroChina, Beijing, 100083, China,College of Geosciences, China University of Petroleum, Beijing,102249, China,Department of Earth Sciences, University College London, Gower Street,London, WC1E 6BT, UK,State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms andEffective Development, SINOPEC Exploration and Production ResearchInstitute, Beijing, 100083, China,College of Geosciences, China University of Petroleum, Beijing,102249, China,Department of Geosciences and Engineering, Delft University ofTechnology, Stevinweg 1, 2628 CN Delft, the Netherlands,State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms andEffective Development, SINOPEC Exploration and Production ResearchInstitute, Beijing, 100083, China,Bureau of Economic Geology, University of Texas at Austin, Austin, TX 78713, USA,College of Geosciences, China University of Petroleum, Beijing,102249, China,State Key Laboratory of Petroleum Resources and Prospecting, ChinaUniversity of Petroleum, Beijing, 102249, China,College of Geosciences, China University of Petroleum, Beijing,102249, China,College of Geosciences, China University of Petroleum, Beijing,102249, China.The dead line for oil and gas and implication for fossil resource prediction[J].Earth System Science Data,2020.
Siccar Point Energy Limited, H1 Hill of Rubislaw, Aberdeen, AB15 6BY, UK,Stable Isotope Laboratory, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK,Siccar Point Energy Limited, H1 Hill of Rubislaw, Aberdeen, AB15 6BY, UK,Stable Isotope Laboratory, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK.The origin of carbonate cements in the Hildasay reservoir, Cambo Field, Faroe-Shetland Basin; clumped isotopic analysis and implications for reservoir performance[J].Marine and Petroleum Geology,2020.
Jin Lai,Dong Li,Guiwen Wang,Chengwen Xiao,Juntao Cao,Chun Wu,Chuang Han,Xinjian Zhao,Ziqiang Qin.Can carbonate cementation be inhibited in continental red bed sandstone?[J].Journal of Petroleum Science and Engineering,2019.
Shuangfeng Zhao,Wen Chen,Lu Zhou,Peng Zhou,Jie Zhang.Characteristics of fluid inclusions and implications for the timing of hydrocarbon accumulation in the cretaceous reservoirs, Kelasu Thrust Belt, Tarim Basin, China[J].Marine and Petroleum Geology,2019.
Wei Duan,Chun-Feng Li,Chengfei Luo,Xue-Gang Chen,Xiaohuan Bao.Effect of formation overpressure on the reservoir diagenesis and its petroleum geological significance for the DF11 block of the Yinggehai Basin, the South China Sea[J].Marine and Petroleum Geology,2018.
Zhiyao Zhang,Guangyou Zhu,Yijie Zhang,Jianfa Han,Tingting Li,Enze Wang,Paul Greenwood.The origin and accumulation of multi-phase reservoirs in the east Tabei uplift, Tarim Basin, China[J].Marine and Petroleum Geology,2018.
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杨博伟,石万忠,张晓明,徐笑丰,刘俞佐,白卢恒,杨洋,陈相霖.黔南地区下石炭统打屋坝组页岩气储层孔隙结构特征及含气性评价[J].岩性油气藏,2024(01).
叶慧,石万忠,王任,齐荣,刘凯,贾会冲,林建炜.鄂尔多斯盆地南部玉都走滑断裂带构造特征及其对油气成藏的控制[J].地球科学,2023(06).
王志民,王翠丽,徐珂,张辉,陈乃东,邓虎成,胡笑非,杨宇勇,冯信荦,杜宇,雷思凡.超深层致密砂岩构造裂缝发育特征及控制因素——以塔里木盆地库车坳陷博孜—大北地区下白垩统储集层为例[J].天然气地球科学,2023(09).
李斌,姜潇俊,赵星星,邬光辉,韩剑发,刘强,汪如军.塔里木盆地台盆过渡带多相态油气藏成因及差异富集模式——以玉科地区奥陶系为例[J].石油学报,2023(05).
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赖锦,肖露,赵鑫,赵飞,黎雨航,朱世发,王贵文,刘宏坤.深层—超深层优质碎屑岩储层成因与测井评价方法——以库车坳陷白垩系巴什基奇克组为例[J].石油学报,2023(04).
刘宏坤,艾勇,王贵文,陈康军,蔡德洋,曹军涛,解宇强,李栋,赖锦.深层、超深层致密砂岩储层成岩相测井定量评价:以库车坳陷博孜-大北地区为例[J].地质科技通报,2023(01).
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杨学文,王清华,李勇,吕修祥,谢会文,吴超,王翠丽,王祥,莫涛,汪瑞.库车前陆冲断带博孜—大北万亿方大气区的形成机制[J].地学前缘,2022(06).
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史超群,张慧芳,周思宇,王佐涛,蒋俊,章学岐,左小军,娄洪,王振鸿,陈常超.塔里木盆地库车坳陷克拉苏构造带—秋里塔格构造带白垩系巴什基奇克组深层、高产储层特征及控制因素[J].天然气地球科学,2020(08).
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