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四川盆地中北部DB1井区灯影组四段沉积相及储层特征

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四川盆地中北部(川中北部)灯影组四段(灯四段)储层岩性复杂,非均质性较强,限制了灯影组四段气藏的勘探.为了进一步深化川中北部DB1井区的沉积相及储层特征认识,通过钻井岩心及薄片资料的观察,并结合测井、录井、物性测试以及钻探成果等资料的综合分析,对川中北部DB1井区灯四段沉积相及储层特征进行研究.结果表明:研究区灯四段主要发育台地边缘和局限台地2种沉积亚相,进一步可识别出藻丘、颗粒滩和滩间海等沉积微相,其中藻丘微相主要发育藻凝块云岩和藻叠层云岩,颗粒滩微相主要发育砂屑云岩,滩间海微相主要发育泥晶云岩和粉晶云岩;藻丘和颗粒滩沉积主要发育在台缘一侧,向台内藻丘和颗粒滩沉积逐渐减少,以滩间海沉积为主;藻丘发育呈纵向叠置特征,横向延伸较近,且集中发育在灯四段上亚段,单体厚度较大,下亚段发育较少且厚度较薄;储集岩类型主要为藻凝块云岩、藻叠层云岩和砂屑云岩,储集空间主要为藻黏结格架孔、粒间溶孔和晶间溶孔;研究区岩心孔隙度分布在2.02%~6.03%,总体平均孔隙度为3.11%,岩心渗透率分布在0.007 04~9.78 mD,总体平均渗透率为0.692 64 mD,整体物性具有低孔特低渗透特征,部分样品由于受到裂缝的影响呈现低孔高渗透特征.
Sedimentary facies and reservoir characteristics of fourth Member of Dengying Formation in Well DB1 area,north-central Sichuan Basin
The reservoir lithology of the fourth Member of Dengying Formation in the north-central Sichuan Basin is complex with strong heterogeneity,which limits the gas reservoir exploration in the fourth Member of Dengying Formation.To further deepen the understanding of sedimentary facies and reservoir characteristics in Well DB1 area in north-central Sichuan,the sedi-mentary facies and reservoir characteristics of the fourth Member of Dengying Formation in Well DB11 area in the north-central Sichuan were studied based on the data of drilling core,thin section observation,well logging,log,physical property test,and drilling results.The results show that two sedimentary subfacies of platform margin and restricted platform are mainly developed in the fourth Member of Dengying Formation in the study area,and sedimentary microfacies such as algal mound,grain beach,and inter-beach sea were further identified.Among them,algal mound microfacies mainly develop algal clot dolomite and algal stromatolite dolomite,grain beach microfacies mainly develop calcarenite dolomite,and inter-beach sea microfacies mainly de-velop micritic dolomite and powder crystal dolomite.The algal mounds and grain beaches in the fourth Member of Dengying For-mation in the study area are mainly developed on the side of the platform margin,and the deposition of algal mounds and grain beaches in the platform gradually decreases mainly inter-beach sea deposition.The development of algal mounds in the fourth Member of the Dengying Formation in the study area is characterized by longitudinal superposition,and the horizontal extension is relatively close.Meanwhile,the algal mounds are concentrated in the Upper Submember of the fourth Member of Dengying Formation with large monomer thickness,while the Lower Submember of the fourth Member of Dengying Formation is less de-veloped and thinner.The reservoir rock types of the fourth Member of Dengying Formation in the study area are mainly algal clot dolomite,algal stromatolite dolomite,and calcarenite dolomite.The reservoir space is mainly algal binding framework pore,in-tergranular dissolved pore,and intergranular dissolved pore.The core porosity of the fourth Member of Dengying Formation in the study area is distributed between 2.02%and 6.03%with an overall average porosity of 3.11%,the core permeability is distrib-uted between 0.007 04 and 9.78 mD,and the overall average permeability is 0.692 64 mD.The overall physical properties are characterized by low porosity and ultra-low permeability,and some samples show low porosity and high permeability due to the influence of fractures.

sedimentary microfaciesdistribution characteristicreservoir characteristicfourth Member of Dengying Formationnorth-central Sichuan Basin

陈泓位、王时林、和源、王君、秦启荣、赵建民

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西南石油大学地球科学与技术学院,四川成都 610500

中国石油西南油气田公司勘探开发研究院,四川成都 610041

中国石油集团川庆钻探工程有限公司地质勘探开发研究院,四川成都 610051

大庆钻探工程公司试油测试公司,吉林松原 138000

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沉积微相 展布特征 储层特征 灯影组四段 四川盆地中北部

中国石油重大专项

2023YQX10104

2024

油气地质与采收率
中国石油化工股份有限公司胜利油田分公司

油气地质与采收率

CSTPCD北大核心
影响因子:2.177
ISSN:1009-9603
年,卷(期):2024.31(3)
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