首页|四川盆地东南部下奥陶统桐梓组白云岩储层特征与成因机制

四川盆地东南部下奥陶统桐梓组白云岩储层特征与成因机制

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四川盆地东南部下奥陶统桐梓组白云岩具备良好的油气成藏条件,但其储层特征、成因机制及发育规模尚不明晰.为此,基于野外露头调查,通过薄片观察、阴极发光、扫描电镜与物性分析,研究了四川盆地东南部桐梓组白云岩储集岩类型、储集空间发育特征,并结合白云石有序度、碳/氧/锶同位素与稀土元素等地球化学资料,探讨了白云岩储层成因机制与主控因素,最后建立了该套白云岩储层的发育模式.研究结果表明:①桐梓组白云岩储集岩类型多样,以鲕粒白云岩、似球粒白云岩和粉细晶白云岩的储集性能最优,其次为粉晶白云岩,而泥晶白云岩和砂屑白云岩较差.②晶间(溶)孔、粒间(溶)孔、粒内溶孔与溶蚀孔洞是桐梓组白云岩的主要储集空间类型.③局限台地浅滩和潮坪沉积是桐梓组白云岩储层形成的基础,同生—准同生期溶蚀作用是形成储集空间的关键机制,其对规模性储层的发育起到决定性作用;同生—准同生期白云石化作用与埋藏期烃类充注是规模性储层得以保存的关键因素,埋藏胶结作用是储层被破坏的最主要原因.④在同生—准同生期溶蚀改造和白云石化的前提下,经历较弱的埋藏胶结作用之后随即发生烃类充注,是该区桐梓组白云岩储层发育的最有利模式.结论认为,四川盆地东南部桐梓组白云岩具备形成规模储层的条件,其中局限台地浅滩和潮坪亚相白云岩是下一步天然气勘探的首选目标.
Reservoir characteristics and genetic mechanisms of the Lower Ordovician Tongzi Formation dolostone in the southeastern Sichuan Basin
The Lower Ordovician Tongzi Formation dolostone in the southeastern Sichuan Basin has favorable conditions for hydrocarbon accumulation,but its reservoir characteristics,genetic mechanism,and development scale have not been clarified.In this paper,the reservoir rock types of Tongzi Formation dolostone and the development characteristics of storage space in the southeastern Sichuan Basin are studied by means of field outcrop investigation,thin-section observation,cathodoluminescence,scanning electron microscopy,and physical property analysis.Then,based on the geochemical data of dolostone ordering,carbonate/oxygen/strontium isotopes,and rare earth elements,the genetic mechanisms and main controlling factors of dolomite reservoir are discussed.Finally,the development model of this set of dolostone reservoir is established.The following results are obtained.First,the Tongzi Formation dolostone is diverse in reservoir rock types,among which,oolitic dolostone,peloidal dolostone,and power to fine crystalline dolostone are the best in reservoir performance,followed by powder crystalline dolostone,and micritic dolostone and sandy dolostone are poor.Second,the main types of storage space in the Tongzi Formation dolostone are intercrystalline(dissolved)pores,intergranular(dissolved)pores,intragranular dissolved pores,and vugs.Third,the restricted platform shoal and tidal flat deposits are the basis for the formation of Tongzi Formation dolostone reservoirs.Syngenetic-penesyngenetic dissolution is the key mechanism for the formation of storage space and plays a decisive role in large-scale reservoir development.Syngenetic-penesyngenetic dolomitization and burial hydrocarbon charging are the key factor for the preservation of large-scale reservoir,and the burial cementation is the major cause of reservoir destruction.Fourth,under the premise of syngenetic-penesyngenetic dissolution and dolomitization,hydrocarbon charging occured immediately after weak burial cementation is the most favorable model for the development of Tongzi Formation dolostone reservoir in this area.In conclusion,the Tongzi Formation dolostone in the southeastern Sichuan Basin has the conditions for the formation of large-scale reservoirs,and the dolostone of restricted platform shoal and tidal flat subfacies are the preferred targets for natural gas exploration in the next step.

Southeastern Sichuan BasinLower Ordovician Tongzi FormationDolostoneReservoir characteristicsGenetic mechanismSyngenetic-penesyngenetic dissolution

李文杰、施泽进、胡东风、田亚铭、王勇、王沧、肖海龙、陈钰桦、谭谦

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油气藏地质及开发工程全国重点实验室·成都理工大学

中国石化勘探分公司

四川盆地东南部 下奥陶统桐梓组 白云岩 储层特征 成因机制 同生—准同生期溶蚀作用

2024

天然气工业
四川石油管理局 中国石油西南油气田公司 中国石油川庆钻探工程公司

天然气工业

CSTPCD北大核心EI
影响因子:2.298
ISSN:1000-0976
年,卷(期):2024.44(12)