1. 中国地质大学(武汉)构造与油气资源教育部重点实验室
2. 中国石化石油勘探开发研究院
3. 宜昌市夷陵区自然资源和规划局
纸质出版:2026
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景海杰, 王琳霖, 任克雄, 等. 鄂尔多斯盆地北部新召地区山西组砂岩储层压力演化与低压成因[J]. 地质科技通报, 2026,45(1):81-94.
景海杰, 王琳霖, 任克雄, et al. 鄂尔多斯盆地北部新召地区山西组砂岩储层压力演化与低压成因[J]. Bulletin of Geological Science and Technology, 2026, 45(1): 81-94.
景海杰, 王琳霖, 任克雄, 等. 鄂尔多斯盆地北部新召地区山西组砂岩储层压力演化与低压成因[J]. 地质科技通报, 2026,45(1):81-94. DOI: 10.19509/j.cnki.dzkq.tb20240130.
景海杰, 王琳霖, 任克雄, et al. 鄂尔多斯盆地北部新召地区山西组砂岩储层压力演化与低压成因[J]. Bulletin of Geological Science and Technology, 2026, 45(1): 81-94. DOI: 10.19509/j.cnki.dzkq.tb20240130.
鄂尔多斯盆地北部新召地区上古生界砂岩储层富含天然气且普遍发育异常低压,对古压力演化以及现今异常低压形成机理认识尚不够深入,制约了致密砂岩气成藏规律的认识和增储上产。运用流体包裹体岩相学观察、显微测温和激光拉曼分析技术,综合分析山西组二段储层中油气充注历史,获取成藏关键时期的古压力;利用盆地模拟法恢复古压力演化史,建立古流体压力演化与油气充注的耦合关系,并进一步探讨异常低压成因与致密气成藏的成因联系。研究表明:(1)研究区山二段CO
2
包裹体捕获于距今180~170 Ma,此时烃源岩处于中-低成熟阶段,甲烷包裹体捕获于距今138~121 Ma的生烃高峰期;(2)山二段储层在早侏罗世开始发育超压,并在早白垩世末规模达到最大,古压力及古压力系数约为50 MPa和1.31;(3)由于温度降低、孔隙反弹和气体扩散等因素造成山二段地层压力降低分别约占总地层压力下降幅度的49%
14.5%和36.5%。山二段储层经历了常压-中等超压-常压-低压的演变过程,生烃增压与压力传导是古超压形成的主要原因,温度降低和天然气扩散是山二段异常低压形成的主控因素。
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李勇,高爽,吴鹏,徐立富,马立涛,胡维强,杨江浩.深部煤层气游离气含量预测模型评价与校正——以鄂尔多斯盆地东缘深部煤层为例[J].石油学报,2023(11).
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曾宇,侯宇光,胡东风,何生,刘若冰,董田,杨锐,李欣诚,叶云飞.川东南盆缘常压区页岩裂缝脉体特征及古压力演化[J].地球科学,2022(05).
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