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作 者:金民东 李毕松[1] 朱祥[1] 代林呈 姜智利 吴浩[1] 李辉[1] 杨佩芸 JIN Mindong;LI Bisong;ZHU Xiang;DAI Lincheng;JIANG Zhili;WU Hao;LI Hui;YANG Peiyun(SINOPEC Exploration Company,Chengdu 610041,China)
出 处:《石油勘探与开发》2020年第6期1090-1099,共10页Petroleum Exploration and Development
基 金:国家科技重大专项(2017ZX05005-003-06)。
摘 要:基于四川盆地东北部元坝及周缘地区野外露头和三维地震资料,对震旦系灯影组四段(简称灯四段)储集层基本特征、主控因素和发育规律进行综合分析。结果表明,灯四段储集层主要发育于与微生物丘建造相关的微生物白云岩和与颗粒滩建造相关的砂屑白云岩中,储集空间以粒间溶孔、格架间溶孔和溶洞为主,储集层整体呈现大规模发育、非均质性较强的特征。储集层成因机理分析表明,灯四段储集层为丘滩相叠加桐湾Ⅱ幕岩溶作用改造而成,岩溶作用具有花斑状岩溶系统和半离解带等早成岩期岩溶作用标志。储集层受到沉积相带控制,丘滩相是有利储集层发育的决定性因素。进一步分析认为,元坝地区具有台缘丘滩发育的地质背景,丘滩体可作为有利勘探对象。Based on the abundant outcrops and 3D seismic data in Yuanba and its surrounding areas in northeastern Sichuan Basin,the characteristics,main controlling factors and development regularities of reservoirs in the fourth member of Sinian Dengying Formation(shortened as Deng 4 Member)were analyzed comprehensively.The results show that the reservoirs were mainly developed in microbial dolomite associated with the microbial mound and dolarenite associated with grain beach,and had intergranular dissolution pores,inter-frame dissolution pores and karst caves as main storage space.The reservoirs were large in scale and strong in heterogeneity.The analysis of the reservoir genetic mechanisms shows that the reservoirs in the fourth member of Dengying Formation were the products of karstification on mound-beach facies deposited in the second episode of Tongwan movement.The karstification had the marks of eogenetic karstification such as granophyric karst system and half-dissociation zone.The reservoirs were controlled by the sedimentary facies belt,the mound beach facies was the decisive factor in reservoir development.Further analysis indicates that the Yuanba area had a geological background of well-developed platform margin mound beach facies,so mound beach bodies can be taken as a favorable exploration target.
关 键 词:储集层 丘滩相带 岩溶作用 震旦系 灯四段 元坝地区 四川盆地
分 类 号:TE122[石油与天然气工程—油气勘探]
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