首页|济阳坳陷下古生界潜山储层形成机制与发育模式

济阳坳陷下古生界潜山储层形成机制与发育模式

扫码查看
下古生界潜山是目前济阳坳陷深层油气勘探聚焦的重点领域,但其储层具有强非均质性、难以有效预测的特点.本次研究基于钻井岩心、铸体薄片、测井资料,结合部分水-岩实验,分析储层的发育特征,明确增储机制,建立发育模式.研究表明,济阳坳陷下古生界潜山储层以次生孔隙为主,发育溶蚀孔、洞和裂缝,受岩性、裂缝、大气淡水、热液及有机酸流体共同控制,纵向上形成风化壳及内幕两套储集系统,两者之间以致密不渗透层相隔.风化壳储集系统灰岩较发育,在构造裂缝连通的情况下,受多期大气淡水淋滤改造,形成岩溶-缝洞型储层;内幕储集系统白云岩发育,受构造运动影响更易于破裂产生裂缝,在构造裂缝连通的情况下,受有机酸流体溶蚀,形成裂缝-孔隙型储层;燕山期热液流体沿构造裂缝也可对两套储集系统进行溶蚀改造.由此可见,岩石类型是溶蚀的基础,构造裂缝是桥梁,流体溶蚀与构造裂缝的有效匹配是优质储层形成的关键.研究成果对研究区及华北地台其他具有相似构造背景的碳酸盐岩潜山的储层预测及油气勘探具有重要的借鉴意义.
Formation mechanism and development model of the Lower Paleozoic buried hill reservoirs in the Jiyang Depression
The Lower Paleozoic buried hill is key target for the exploration of oil and gas in depth in the Jiyang Depression,however,the reservoir is characterized with strong heterogeneity and hardly effective prediction.Based on observations of drilling cores and their thin sections,and logging data of drilling holes,combined with data of water-rock experiments,we have analyzed development characteristics of the reservoir,clarified the mechanism how to make the reserve of oil and gas in the reservoir be increased,and established the development model of the reservoir.The research shows that the Lower Paleozoic buried hill reservoirs in the Jiyang Depression are characterized with dominent secondary pores including dissolution pores,holes and cracks which were controlled by lithology,cracks,atmospheric fresh water,hydrothermal fluid and organic acid fluid.There are two sets of reservoir systems including the weathering crust and the internal ones distributed vertically.These two reservoir systems are separated by densely impermeable layers.Due to the reworking of relatively developed limestone in the weathering crust reservoir system by the leaching of multi-stage atmospheric freshwaters through the communicated structural cracks and fissures,the karst-fracture-cavity reservoir was formed in the weathering crust.The relatively developed dolomite of the internal reservoir system is more susceptibly ruptured and fractured by the structural movement.In the case of structural crack communication,the dissolution of cracked dolomite by organic acid fluid resulted in the formation of fracture-pore type reservoir in the internal system.These two reservoir systems could be also reworked by the dissolution of the Yanshanian hydrothermal fluid along the structural cracks.Therefore,the rock type is the basis of dissolution,the structural crack is the bridge of fluid,and the effective matching of fluid dissolution with structural cracks is the key factor to the high quality reservoir formation.The research results have important reference significance for the reservoir prediction and oil and gas exploration in the carbonate buried hills in the study area and other areas with similar structural background in the North China platform.

carbonate rockstructural crackdiagenetic fluidformation mechanismdevelopment modelthe Lower PaleozoicJiyang Depression

王永诗、田雯、王学军、景安语、马立驰、马帅

展开 >

中国石油化工股份有限公司胜利油田分公司,山东东营 257000

中国石油化工股份有限公司胜利油田分公司勘探开发研究院,山东东营 257015

中国石油化工股份有限公司勘探开发研究院,北京 100083

碳酸盐岩 构造裂缝 成岩流体 形成机制 发育模式 下古生界 济阳坳陷

2024

矿物学报
中国矿物岩石地球化学学会 中国科学院地球化学研究所

矿物学报

CSTPCD北大核心
影响因子:1.2
ISSN:1000-4734
年,卷(期):2024.44(6)