海拉尔—塔木察格盆地中部断陷带构造演化与富油构造带成因机制分析

孙永河, 史盼盼, 杨帆, 袁红旗, 杨勉. 海拉尔—塔木察格盆地中部断陷带构造演化与富油构造带成因机制分析[J]. 地质科学, 2012, 47(3): 700-713.
引用本文: 孙永河, 史盼盼, 杨帆, 袁红旗, 杨勉. 海拉尔—塔木察格盆地中部断陷带构造演化与富油构造带成因机制分析[J]. 地质科学, 2012, 47(3): 700-713.
Sun Yonghe, Shi Panpan, Yang Fan, Yuan Hongqi, Yang Mian. Analysis on tectonic evolution and genetic mechanism of oil-rich structural belt at middle fault depression belt in Hailer-Tamtsag Basin[J]. Chinese Journal of Geology, 2012, 47(3): 700-713.
Citation: Sun Yonghe, Shi Panpan, Yang Fan, Yuan Hongqi, Yang Mian. Analysis on tectonic evolution and genetic mechanism of oil-rich structural belt at middle fault depression belt in Hailer-Tamtsag Basin[J]. Chinese Journal of Geology, 2012, 47(3): 700-713.

海拉尔—塔木察格盆地中部断陷带构造演化与富油构造带成因机制分析

详细信息
    作者简介:

    孙永河, 男, 1979年1月生,博士,副教授,矿产普查与勘探学专业。E-mail: syh79218@163.com

  • 中图分类号: P542, TE122

Analysis on tectonic evolution and genetic mechanism of oil-rich structural belt at middle fault depression belt in Hailer-Tamtsag Basin

  • 海拉尔盆地和塔木察格盆地分属于中国和蒙古国,构造上具有统一的构造背景和成盆演化过程。为了整体剖析海拉尔—塔木察格盆地构造演化过程及其对油气运聚成藏的控制作用,本文在明确成盆背景基础上,立足中部断陷带,系统研究了盆地的沉积充填结构、盆地的性质及其叠加演化过程,进而分析了不同演化阶段富油构造带的形成机制及构造演化对油气成藏的控制作用。研究表明,海塔盆地分别由铜钵庙组构成的残留盆地和由南屯组—青元岗组构成的被动裂陷盆地两种不同性质盆地叠加而成,被动裂陷盆地可进一步划分为4个演化阶段,即南一段下、中亚段构成的初始裂陷演化阶段、南一段上亚段—南二段构成的强裂陷演化阶段、大磨拐河组—伊敏组构成的断坳转化演化阶段以及青元岗组构成的坳陷演化阶段。初始裂陷阶段简单剪切走滑变形控制形成的掀斜隆起带,为下部油气系统即南一段下亚段和中亚段的有利勘探方向; 强裂陷阶段的纯剪切伸展变形控制形成的中央隆起带和中央背斜带,为中部油气系统即南一段上亚段和南二段的有利勘探方向; 断坳转化阶段伊二、三沉积晚期的纯剪切张扭变形控制断裂密集带的形成,并指示下部和中部油气系统的油气运聚成藏及富集部位; 伊二、三段末期及坳陷演化阶段的挤压反转变形主要控制了多类型反转构造带的形成,并指示上部次生油气系统即大磨拐河组的油气调整聚集成藏及富集部位。
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出版历程
收稿日期:  2012-04-10
修回日期:  2012-05-24
刊出日期:  2012-07-25

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