孙雨,马世忠,姜洪福,刘云燕,刘宗堡

• 1:东北石油大学地球科学学院
• 2:大庆油田有限责任公司第八采油厂

摘要(Abstract)：

应用高分辨率层序地层学理论及其方法技术,依据22口井的钻井岩芯和4256口测井曲线资料,系统分析了松辽盆地三肇凹陷葡萄花油层各级次基准面旋回界面类型及特征,将葡萄花油层划分为2个中期、4个短期、8个超短期旋回层序,建立了以短期旋回层序为框架、超短期旋回层序为对比单元的高分辨率层序地层格架,并提出了三肇凹陷南部葡萄花油层为同沉积构造抬升控制的中部超短期基准面旋回层序向南逐渐减薄、直至缺失的层序地层模式。三肇凹陷由西北(卫星—宋北)→凹陷中心(徐家围子)→向南(肇州):葡萄花油层上部呈砂岩(非地层)退覆型尖灭,即同层砂岩逐渐尖灭为泥岩,上层砂岩尖灭线逐渐北移;葡萄花油层下部呈砂岩(非地层)超覆型尖灭,即同层砂岩逐渐尖灭为泥岩,上层砂岩尖灭线逐渐南移。

关键词(KeyWords)： 基准面旋回;高分辨率层序地层学;精细沉积学;葡萄花油层;姚家组;白垩系;三肇凹陷;黑龙江省

Abstract:

Keywords:

基金项目(Foundation): 中国石油天然气股份有限公司科学研究与技术开发项目[No.06-01C-01-01(B)]资助

作者(Author): 孙雨,马世忠,姜洪福,刘云燕,刘宗堡

DOI: 10.19839/j.cnki.dcxzz.2010.04.004

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