川东北地区中—上二叠统海相页岩储层特征 及其地质意义——以孤峰组—大隆组页岩为例

作    者:张 琴1,2,3,邱 振1,2,3,梁 峰1,2,3,刘 雯1,2,3,孔维亮1,2,3,王玉满1,2,3, 庞正炼1,高万里1,4,蔡光银1,2,3,曲天泉1,4,江 冲1,4
单    位:中国石油勘探开发研究院;2 国家能源页岩气研发(实验)中心; 3 中国石油天然气集团有限公司煤岩气重点实验室;4 中国矿业大学(北京)地球科学与测绘工程学院
基金项目:
摘    要:
四川盆地东北部中—上二叠统发育孤峰组、吴家坪组三段和大隆组一段等3套海相页岩层系,是页岩气增储 上产的重要新层系。基于大量岩心测试数据,分析其地球化学特征、储层发育特征,并提出针对性开发策略,以期为 中国页岩气的勘探提供理论支撑。研究结果表明:①3套页岩有机质丰度高,有机质类型均为II1型,成熟度(Ro)均大 于2.0%,生烃潜力大。孤峰组以硅质页岩相与钙质页岩相为主,吴三段和大一段则以硅质页岩相和混合质页岩相为 主,页岩的脆性指数均分布在 70%以上。②3套页岩均以有机质孔为主要孔隙类型,且孔径以介孔为主。吴三段层 理缝发育,连通系数最好,孔隙度与含气量最高;孤峰组孔隙度高,连通系数居中,含气量较高;大一段层理缝不发育, 连通系数和孔隙度最低,但含气量较高。③相比川南龙马溪组,3套页岩具有“三高一薄一深”的特征,即高TOC、高脆 性、高含气量,但单层厚度较薄,埋深更大,需建立针对性开发技术。3套页岩层系页岩气富集有利区主要分布在开 江—梁平海槽东南段以及城口—鄂西海槽的城口—奉节—利川—石柱一带。研究成果为四川盆地二叠系页岩气勘 探提供了重要理论依据,对深层页岩气开发具有指导意义。
关键词:中—上二叠统;孤峰组;吴家坪组三段;大隆组一段;储层特征;页岩气;川东北

Characteristics and geological significance of marine shale reservoirs of the Middle-Upper Permian in northeastern Sichuan Basin: a case study of the Gufeng Formation-Dalong Formation shales

Author's Name: ZHANG Qin1,2,3, QIU Zhen1,2,3, LIANG Feng1,2,3, LIU Wen1,2,3, KONG Weiliang1,2,3, WANG Yuman1,2,3, PANG Zhenglian1, GAO Wanli1,4, CAI Guangyin1,2,3, QU Tianquan1,4, JIANG Chong1,4
Institution: 1. PetroChina Research Institute of Petroleum Exploration and Development;2. National Energy Shale Gas Research and Development (Experiment) Center;3. CNPC Key Laboratory of Coal-rock Gas;
Abstract:
Three marine shale formations of the Middle-Upper Permian—the Gufeng Formation (P2g), the 3rd member of the Wujiaping Formation (P3w3) and the 1st member of the Dalong Formation (P3d1), are well developed in the northeastern Sichuan Basin, representing promising new targets for enhancing shale gas reserves and production. Based on extensive core testing data, this study analyzes their geochemical characteristics, reservoir features and proposes corresponding development strategies to provide theoretical support for shale gas exploration in China. The key findings are as follows: (1) All three shale formations exhibit high organic matter abundance, with average total organic carbon (TOC) contents of 9.82% (P2g), 6.60% (P3w3) and 6.01%(P3d1), respectively. The organic matter is classified as type II1, and the maturity(Ro) exceeds 2.0%, indicating significant hydrocarbon generation potential. The Gufeng Formation is dominated by siliceous shale and calcareous shale facies, whereas P3w3 and P3d1 primarily consist of siliceous shale and mixed shale facies. The brittleness index of all three formations exceeds 70%. Organic pores are the dominant pore type, with mesopores serving as the primary pore category. (2) The P3w3 exhibits well-developed laminated fractures, highest pore connectivity index (average value of 5.17), high porosity and high gas content; the P2g has moderate pore connectivity index (average value of 2.57), high porosity and gas content; the P3d1 shows poor laminated fracture development, the lowest pore connectivity index(average value of 1.69), the lowest porosity value and relatively high gas content. (3) Compared to the Longmaxi Formation in southern Sichuan Basin, these three shale formations are characterized by high TOC content, high brittleness index, high gas content, thin thickness and deep burial depth. Targeted development technologies are thus required. Favorable areas for shale gas enrichment of these three formations are primarily distributed in the southeastern segment of the Kaijiang-Liangping Trough and the Chengkou-Fengjie-Lichuan-Shizhu area of the Chengkou- E'xi Trough.
Keywords: Middle-Upper Permian; Gufeng Formation; 3rd member of Wujiaping Formation; 1st member of Dalong For⁃ mation; reservoir characteristics; shale gas; northeastern Sichuan Bain
投稿时间: 2025-07-01  
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