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巫山坎区块嘉二1亚段储层控制因素研究

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川东巫山坎区块下三叠统嘉二1亚段云岩油气资源潜力大.对嘉二1亚段沉积、储层特征及控制因素的研究表明,巫山坎区块位于局限台地的台内点滩上,受较强水动力影响,具备储层形成和演化的基础.嘉二1亚段储集岩以泥-细粉晶云岩、粗粉晶云岩为主,镜下溶孔、裂缝发育.由于该区的获气井位于构造顶部,后期溶蚀作用较强,在云岩中产生了一定的溶蚀孔,而构造作用改造形成的裂缝是储层中油气渗流的主要通道.因此,在巫山坎区块嘉二1亚段储层的形成与演化过程中,台内点滩是储层发育的有利沉积环境;白云岩化及溶蚀作用控制着储层孔隙的发育程度;构造作用改善了储层的渗透能力,储层有沿构造高点和轴线分布的趋势.
Reservoir Control Factors of T1j12 Subsegment in Wushankan Block
There is a great potential for oil and gas resources in the lower Triassic series T1j12 subsegment of the Wushankan block in the eastern part of Sichuan.Through research on the sedimentation,reservoir characteristics,and control factors of the T1j12 subsegment,it is shown that the Wushankan block is located on a limited platform within a point beach,affected by strong hydrodynamic forces,having the foundation for reservoir formation and evolution.The reservoir rocks in the T1j12 subsegment are mainly composed of mud-fine powder crystal dolomite and coarse powder crystal dolomite,microscopic dissolution pores and crack development.Due to the fact that the gas well in this area is located at the top of the structure,strong dissolution in the later stage resulted in the formation of certain dissolution pores in the dolomite,the fractures formed by tectonic transformation are the main channels for oil and gas seepage in reservoirs.Therefore,in the process of formation and evolution of reservoirs in the T1j12 subsegment of the Wushankan block,point beach is a favorable sedimentary environment for the development of reservoirs;dolomitization and dissolution control the development of reservoir pores;tectonism improves the permeability of the reservoir,the reservoir has a trend of distribution along structural highs and axes.

T1j12 subsegmentWushankan blockdolomitereservoircontrol factor

刘菲、陈家文、易娟子、罗妮娜、黎李、徐露

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中国石油西南油气田分公司重庆气矿,重庆 400021

重庆相国寺储气库有限公司,重庆 401120

嘉二1亚段 巫山坎区块 云岩 储层 控制因素

2024

能源与节能
山西省能源研究会 山西省节能研究会

能源与节能

影响因子:0.561
ISSN:2095-0802
年,卷(期):2024.(9)