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    伸展构造盆地的平衡剖面及其构造意义——以松辽盆地南部为例

    颜丹平 田崇鲁 孟令波 张建增 周美夫

    颜丹平, 田崇鲁, 孟令波, 张建增, 周美夫, 2003. 伸展构造盆地的平衡剖面及其构造意义——以松辽盆地南部为例. 地球科学, 28(3): 275-280.
    引用本文: 颜丹平, 田崇鲁, 孟令波, 张建增, 周美夫, 2003. 伸展构造盆地的平衡剖面及其构造意义——以松辽盆地南部为例. 地球科学, 28(3): 275-280.
    YAN Dan-ping, TIAN Chong-lu, MENG Ling-bo, ZHANG Jian-zeng, ZHOU Mei-fu, 2003. Balanced Geological Section for Extensional Tectonic Basin and Its Implication: An Example from Southern Songliao Basin. Earth Science, 28(3): 275-280.
    Citation: YAN Dan-ping, TIAN Chong-lu, MENG Ling-bo, ZHANG Jian-zeng, ZHOU Mei-fu, 2003. Balanced Geological Section for Extensional Tectonic Basin and Its Implication: An Example from Southern Songliao Basin. Earth Science, 28(3): 275-280.

    伸展构造盆地的平衡剖面及其构造意义——以松辽盆地南部为例

    基金项目: 

    国家自然科学基金项目 40172070

    详细信息
      作者简介:

      颜丹平(1964-), 男, 博士, 副教授, 主要从事构造地质学、盆地构造及构造地球化学的教学与研究工作.E-mail: yandp@cugb.edu.cn

    • 中图分类号: P54

    Balanced Geological Section for Extensional Tectonic Basin and Its Implication: An Example from Southern Songliao Basin

    • 摘要: 挤压构造的平衡地质剖面分析已经广泛应用于造山带构造分析, 但伸展构造区的平衡地质剖面分析实例仍然很少.运用盆地分析的技术与方法, 分层序或阶段将地质构造依次恢复、地层逐层回剥, 并通过在松辽盆地南部吉林两井油田扶余油层4条剖面的实践, 复原出不同时代盆地构造与地层发育的连续剖面, 揭示出松辽盆地南部主要构造样式是以浅表构造层次的负花状构造及深层剥离断层发育为特征; 断层生长指数、盆地的伸展史和伸展量等参数显示, 晚白垩世是构造转型的重要阶段, 此前主要为走滑构造样式形成阶段, 此后则主要为伸展滑脱构造发育阶段.在此基础上, 提出松辽盆地具有伸展-走滑双重力学构造性质, 可能是一个弧后构造盆地.

       

    • 图  1  两井油田扶余油层顶面构造(右上角插图为松辽盆地南部构造略图, 据①修改)

      Fig.  1.  Tectonic map on the peak surface of Fuyu oil-bearing layer in Liangjing area and a tectonic outline of southern Songliao basin in the insert

      图  2  剖面1-4的平衡地质剖面(a, b, c, d) 及反演构造剖面(a1-d4)

      Fig.  2.  Balanced sections (a, b, c, d) and their developped tectonic sections (a1-d4) for sections 1-4

      表  1  各主要构造模拟层系岩石力学参数

      Table  1.   Rock mechanics parameters for the simulating beds

      表  2  平衡地质剖面1~4的伸展量

      Table  2.   Extension measures of balanced sections 1-4

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    • 收稿日期:  2002-06-18
    • 刊出日期:  2003-05-25

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