ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
唐明远. 2017: 大牛地气田马五_5白云岩储层特征及分布规律研究. 石油地质与工程, 31(05): 29-32+131-132.
引用本文: 唐明远. 2017: 大牛地气田马五_5白云岩储层特征及分布规律研究. 石油地质与工程, 31(05): 29-32+131-132.
TANG Mingyuan. 2017: Dolomite reservoir characteristics and distribution regularity of Ma5-5 reservoirs in Daniudi gasfield. Petroleum Geology and Engineering, 31(05): 29-32+131-132.
Citation: TANG Mingyuan. 2017: Dolomite reservoir characteristics and distribution regularity of Ma5-5 reservoirs in Daniudi gasfield. Petroleum Geology and Engineering, 31(05): 29-32+131-132.

大牛地气田马五_5白云岩储层特征及分布规律研究

Dolomite reservoir characteristics and distribution regularity of Ma5-5 reservoirs in Daniudi gasfield

  • 摘要: 以沉积岩石学、油气地球化学、碳酸盐岩储层地质学为理论基础,通过大量钻井岩心观察、测井分析、薄片和扫描电镜鉴定、物性及压汞分析,研究了大牛地气田马五_5亚段白云岩储层特征及分布规律。结果表明,马五_5亚段储层岩石类型以粉–细晶白云岩为主;储集空间以晶间孔隙型为主,裂缝–孔隙型次之;平均孔隙度为5.41%,平均渗透率为1.05×10~(-3)μm~2,属于低孔低渗储层。马五_5白云岩是表生期向下渗流的岩溶水与地层本身沉积的泥晶灰岩交代作用形成,其分布与奥陶系风化壳岩溶古地貌密切相关,主要分布在大牛地气田西部、北部的侵蚀高地以及东部、南部的侵蚀沟槽区,中部的斜坡台丘及斜坡区白云岩欠发育。

     

    Abstract: Based on the theoretical basis of sedimentary petrology, petroleum geochemistry and carbonate reservoir geology, through a lot of drilling core observation, logging analysis, thin sections and scanning electron microscopic identification, physical property and mercury intrusion analysis, the research of dolomite reservoir characteristics and distribution regularity of Ma5-5 reservoir was carried out. The results showed the rock type of reservoir in Ma5-5 were mainly of powder-fine dolomite. The reservoir space was dominated by the intercrystalline pore type, and the fracture-pore type was secondary. The average porosity was 5.41%, and the average permeability was 1.051.05 × 10~(-3)μm~2, which was low porosity and low permeability reservoir. Ma5-5 dolomite was supergene period downward flow of karst water and formation sedimentary micritic limestone formed by the metasomatism of itself, its distribution was closely related with the ordovician weathering crust karst geomorphology, which mainly distributed in the west of Daniudi gasfield, northern karst highland and the eastern, southern karst groove area, central slope hill and slope zone of dolomite low-development.

     

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