四川盆地丹凤场地区二叠系茅口组岩溶储层主控因素和有利区评价OA
Main controlling factors and favorable area evaluation of Permian Maokou Formation karst reservoir in Danfengchang area of Sichuan Basin
由于四川盆地丹凤场地区茅口组岩溶储层的系统性研究不足,制约了油气勘探开发进展,亟需厘清储层发育特征和产能主控因素.基于岩心、测录井、地震资料,通过开展岩溶储层岩石类型、储集空间、物性特征、分布情况及主控因素分析,结合主控因素平面叠合,划分储层有利区.结果表明:茅口组岩溶储层以生屑灰岩、藻屑灰岩为主,储集空间以溶洞、粒间溶孔、构造裂缝及溶蚀缝为主,为特低孔-特低渗储层;岩溶储层分为上、下2段,上段储层主要发育在茅三段、茅二段a亚段,下段储层主要发育在茅二段b亚段,上段储层厚度最大达19 m,其规模优于下段;岩溶储层发育主要受高能颗粒滩发育程度、岩溶古地貌类型及断裂组合样式3个因素控制,其中断裂组合样式对于储层改造具有主要影响;共划分出2类有利区,Ⅰ类有利区具有最好的勘探潜力,高产井主要分布在该区域,且距离断层200~1 000 m,Ⅱ类有利区具有一定的勘探潜力.研究成果可有效指导该区下一步勘探开发.
The lack of systematic research on Maokou Formation karst reservoirs in Danfengchang area of Sichuan Basin constrains the progress of oil and gas exploration and development,and urgently needs determination of reser-voir development characteristics and main controlling factors of productivity.Based on cores,logging and seismic data,the rock types,reservoir space,properties,distribution and main controlling factors of karst reservoirs are an-alyzed,and reservoir favorable areas are divided by areally overlapping main controlling factors.The results show that karst reservoir of Maokou Formation is mainly composed of bioclastic limestone and algal limestone,with reser-voir space dominated by vugs,intergranular dissolved pores,structural fractures and dissolution fractures,being ultra-low porosity-ultra-low permeability reservoir.Karst reservoir is divided as upper member and lower member.Upper reservoir mainly developed in Mao3 member and Mao2a sub-member,while lower reservoir mainly devel-oped in Mao2b sub-member.With maximum thickness up to 19 m,upper reservoir is superior to lower reservoir in scale.The development of karst reservoirs is mainly controlled by 3 factors,including development degree of high-energy grain-beach,karst paleogeomorphology types and faults assemblage styles.Among them,faults assemblage style has major impact on reservoir karstification.2 types of favorable areas are defined.Class Ⅰ favorable area has the best exploration potential,and high-production wells mainly distribute in this area,located 200~1 000 m away from fault.Class Ⅱ favorable area has certain exploration potential.The research can effectively guide further explo-ration and development in this area.
兰雨龙;李洪玺;吴畏;欧阳明华;文华国;徐文礼;陈仕臻;莫博文;全豪
中国石油川庆钻探工程公司地质勘探开发研究院,四川 成都 610051中国石油川庆钻探工程公司地质勘探开发研究院,四川 成都 610051中国石油川庆钻探工程公司地质勘探开发研究院,四川 成都 610051中国石油川庆钻探工程公司地质勘探开发研究院,四川 成都 610051油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059
能源科技
四川盆地丹凤场构造茅口组岩溶储层储层特征高产井主控因素
Sichuan BasinDanfengchang structureMaokou Formationkarst reservoirreservoir characteris-ticshigh-production wellsmain controlling factors
《大庆石油地质与开发》 2026 (2)
22-34,13
国家自然科学基金项目"川东地区下三叠统嘉陵江组白云岩分布规律及形成机理"(41972109).
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