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川东北地区长兴组-飞仙关组礁滩相储层预测

刘殊  唐建明  马永生  赵爽 

摘 要:普光气田有典型的台地边缘斜坡相沉积,在斜坡上沉积大型礁滩相储层,礁滩相储层出现比较明显的烟囱效应--地震剖面表现为波阻杂乱和中断,出现下拉.通过对已知气田分析建立起储层预测方法,在川东北地区进行全面的储层预测应用.研究发现,通南巴构造带上的马路背构造和苍溪九龙山构造存在典型的台地边缘相层序地层特征.预测的苍溪礁滩相具有典型的进积型层序地层特征,在地震剖面上并且具有可靠的波组下拉现象.预测苍溪一带有可能存在一个特大型长兴组-飞仙关组礁滩相气田.马路背礁滩相层序地层特征和普光气田基本上相同,为一个斜坡带,其上可能发育大型礁滩相储层,预测可能为一个大型气藏.
关键词:烟囱效应;下拉现象;地震相;层序地层;鲕粒滩;生物礁滩相;川东北地区
分类号:TE111.3  文献标识码:A

文章编号:0253-9985(2006)03-0332-08

Prediction of reef and shoal facies reservoirs in Changxing- Feixianuan Formations in northeastern Sichuan basin

Liu Shu  Tang Jianming   Ma Yongsheng   Zhao Shuang 

 

基金项目:国家自然科学基金项目(40472110)
作者简介:刘殊(1962-),男,高级工程师、博士生,油气地震勘探
作者单位:刘殊(中国地震局地质研究所,北京,100021;中国石油化工股份有限公司,西南分公司,四川,德阳,618000) 
     唐建明(中国石油化工股份有限公司,西南分公司,四川,德阳,618000) 
     马永生(中国石油化工股份有限公司南方勘探开发分公司,云南,昆明,650200) 
     赵爽(成都理工大学,能源学院,四川,成都,610059) 

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