首页|期刊导航|大庆石油地质与开发|松辽盆地青山口组介壳滩的分布特征及控制因素

松辽盆地青山口组介壳滩的分布特征及控制因素OA

Distribution characteristics and controlling factors of shell shoal in Qingshankou Formation of Songliao Basin

中文摘要英文摘要

针对松辽盆地在青山口组介壳滩的分布规律和控制因素研究薄弱的问题,利用井震结合的研究方法,从介壳滩的测井和地震响应、纵向横向分布规律及其控制因素等方面开展了研究.结果表明:松辽盆地青山口组介壳滩主要分布在青山口组一段(青一段)上部和青山口组二段(青二段)下部的湖相泥岩、滩坝砂和席状砂环境;介壳滩总体上具有低声波时差、低自然伽马、高电阻率的测井响应特征,在地震剖面上具有透镜状"亮点"特征,在地震振幅属性及立体雕刻图上为实心圆、椭圆或不规则的团块状强振幅异常,并且多表现出一定的定向排列特点;介壳滩主要受湖平面升降变化、古地貌和水(风)动力的控制,青一段末期—青二段早期湖泊面积大,水体稳定且湖面水位较高,有利于介形虫的大量繁殖,宽缓的斜坡和水下低凸起有利于介壳滩的发育,风浪作用则控制着介壳滩的重新分配.研究成果对于夹层型页岩油的储层研究具有重要的指导意义.

In view of the problem of weak research on distribution laws and controlling factors of shell shoals in Qin-gshankou Formation of Songliao Basin,well-seismic joint research method is used to carry out the research from as-pects of well logging and seismic response,vertical and horizontal distribution laws and controlling factors of shell shoals.The results show that shell shoals in Qingshankou Formation of Songliao Basin are mainly distributed in la-custrine mudstone,beach bar sand and sheet sand environment in upper part of Qing1 Member and lower part of Qing2 Member.Shell shoals generally have logging response characteristics of low acoustic time difference,low nat-ural gamma and high resistivity,with lenticular"bright spot"characteristics on seismic profiles,solid circle,el-lipses or irregular lumpy strong-amplitude anomality in seismic amplitude attributes and 3D caving maps,and most-ly show characteristics of certain directional arrangement.Shell shoals are mainly controlled by changes in lake level,paleomorphology and hydro(wind)dynamics.Large lake area and stable water with high lake-surface water level during late Qing1 Member-early Qing2 Member are conducive to the mass reproduction of ostracods,wide and gentle slopes and underwater low uplifts are conducive to the development of shell shoals,and wind-wave action controls the redistribution of shell shoals.The research provides important guiding significance for the study of inter-bedded shale oil reservoirs.

陆加敏;杨懋新;李军辉;刘英;邵东然;邱晗;赵建芝

中国石油大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712中国石油东方地球物理公司研究院,河北 涿州 072751中国石油大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712中国石油东方地球物理公司研究院,河北 涿州 072751中国石油东方地球物理公司研究院,河北 涿州 072751中国石油东方地球物理公司研究院,河北 涿州 072751中国石油东方地球物理公司研究院,河北 涿州 072751

能源科技

松辽盆地青山口组介壳滩湖平面变化古地貌控制因素

Songliao BasinQingshankou Formationshell shoallake level changespaleomorphologycontrol-ling factors

《大庆石油地质与开发》 2026 (1)

1-8,8

10.19597/J.ISSN.1000-3754.202406014

评论