川东H气藏沙溪庙组储层特征及物性主控因素
Reservoir Characteristics and Main Controlling Factors of Physical Properties of the Shaximiao Formation in the Chuandong H Gas Reservoir
摘要: 目的:针对川东H气藏沙溪庙组储层特征及物性主控因素不明确的问题。方法:综合运用岩心观察、薄片鉴定、压汞实验等多种分析方法,对H气藏沙溪庙组储层的岩石特征、储层孔隙、孔喉特征及孔隙度和渗透率的相关性进行分析和研究。结果表明:沙溪庙组储层主要由岩屑长石砂岩及长石岩屑砂岩组成,粒径以中粒为主,分选性较差,颗粒多呈次棱–次圆状;储集空间以次生溶孔和残余原生孔为主,孔喉半径小、突破压力高,喉道细小;孔隙度和渗透率呈明显的正相关性,属于特低孔–特低渗储层;沉积微相中分支河道、水下分支河道微相砂体的粒度较粗,分选较好,杂基含量低;有利于储层原始孔隙的保存和后期孔隙演化,优势沉积微相和成岩演化是沙溪庙组储层物性发育的主控因素。
Abstract: Objective: To address the unclear issues regarding the reservoir characteristics and main controlling factors of the physical properties of the Shaximiao Formation in the Chuandong H Gas Reservoir. Methods: A comprehensive analysis was conducted on the rock characteristics, reservoir pores, pore-throat features, and the correlation between porosity and permeability of the Shaximiao Formation reservoir in the H Gas Reservoir by integrating multiple analytical methods, including core observation, thin section identification, and mercury injection test. Results show that the Shaximiao Formation reservoir is mainly composed of lithic arkose and feldspathic litharenite, with medium grain size as the dominant fraction, poor sorting, and particles mostly subangular-subrounded in shape. The reservoir spaces are dominated by secondary dissolution pores and residual primary pores, characterized by a small pore-throat radius, high breakthrough pressure, and fine throats. Porosity and permeability exhibit a significant positive correlation, indicating an ultra-low porosity and ultra-low permeability reservoir. Among the sedimentary microfacies, the sand bodies of three microfacies (distributary channel, subaqueous distributary channel, and point bar) are characterized by coarser grain size, better sorting, and low matrix content, which are conducive to the preservation of original reservoir pores and the evolution of late-stage pores. Dominant sedimentary microfacies and diagenetic evolution are the main controlling factors for the development of physical properties of the Shaximiao Formation reservoir.
参考文献
|
[1]
|
葸克来, 操应长, 蔡来星, 等. 松辽盆地梨树断陷营城组低渗透储层成因机制[J]. 现代地质, 2013, 24(1): 208-216.
|
|
[2]
|
高辉, 宋广寿, 孙卫, 等. 储层特低渗透成因分析与评价: 以安塞油田沿25区块为例[J]. 地球科学进展, 2007, 22(11): 1134-1139.
|
|
[3]
|
杨晓萍, 赵文智, 邹才能, 等. 低渗透储层成因机理及优质储层形成与分布[J]. 石油学报, 2007, 28(4): 57-61.
|
|
[4]
|
杨帆, 孙玉善, 谭秀成, 等. 迪那2气田古近系低渗透储集层形成机制分析[J]. 石油勘探与开发, 2005, 32(2): 39-42.
|
|
[5]
|
徐明星, 任洪明, 胥伟冲, 等. 川东北地区沙溪庙组致密砂岩气井产能主控因素探讨[J]. 天然气勘探与开发, 2022, 45(4): 103-110.
|
|
[6]
|
朱筱敏, 葛家旺, 吴陈冰洁, 等. 珠江口盆地陆丰凹陷深层砂岩储层特征及主控因素[J]. 石油学报, 2019, 40(S1): 69-80.
|
|
[7]
|
何仕碧, 戴鸿鸣, 王建. 四川盆地宣汉-达州地区下沙溪庙段储层特征研究[J]. 天然气勘探与开发, 2011, 34(3): 4-7, 85.
|
|
[8]
|
王少依, 张惠良, 寿建峰, 等. 塔中隆起北斜坡志留系储层特征及控制因素[J]. 成都理工大学学报(自然科学版), 2004(2): 148-152.
|
|
[9]
|
查小军. 吉木萨尔凹陷芦草沟组页岩油储层特征及分类评价[D]: [硕士学位论文]. 重庆: 重庆科技学院, 2022.
|
|
[10]
|
谭东萍. 金华地区沙溪庙组致密砂岩储层差异成因机制及储集性评价[D]: [硕士学位论文]. 重庆: 重庆科技学院, 2022.
|
|
[11]
|
Huang, Y., Deng, M., Duan, N., Jin, W., Liu, J., Niu, N., et al. (2025) Sand Body Architecture of Braided River Deltas in the Upper Triassic Xujiahe Formation, Sichuan Basin. Energy Geoscience, 6, Article ID: 100359. [Google Scholar] [CrossRef]
|