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下扬子区伸展拆离构造

丁道桂 罗开平 刘光祥 吕俊祥

丁道桂, 罗开平, 刘光祥, 吕俊祥. 下扬子区伸展拆离构造[J]. 石油实验地质, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001
引用本文: 丁道桂, 罗开平, 刘光祥, 吕俊祥. 下扬子区伸展拆离构造[J]. 石油实验地质, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001
Ding Daogui, Luo Kaiping, Liu Guangxiang, Lü Junxiang. Extensional detachment structures in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001
Citation: Ding Daogui, Luo Kaiping, Liu Guangxiang, Lü Junxiang. Extensional detachment structures in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001

下扬子区伸展拆离构造

doi: 10.11781/sysydz201601001
基金项目: 中国石化导向项目(2014-ZS-YTB010)资助。
详细信息
    作者简介:

    丁道桂(1946-),男,教授级高级工程师,从事含油气盆地构造研究。E-mail:ddgwx@aliyun.com。

  • 中图分类号: TE121.2

Extensional detachment structures in the Lower Yangtze region

  • 摘要: 在郯庐断裂带以东,包括苏北-南黄海地区在内的下扬子区,晚白垩世-古近纪时期,在太平洋板块由南向北俯冲消减的运动过程中,东亚大陆被牵引,发生了由南向北的大型左行平移走滑运动和岩石圈上地壳递进减薄拉张的伸展拆离构造运动。从苏、皖南的南陵-广德、句容-常州断陷盆地开始,经苏北东台、盐阜坳陷-南黄海南部的青岛坳陷,再向北至南黄海北部的烟台坳陷,形成了3条呈NE-近EW走向的断陷盆地构造带。盆地为具有南断北超的箕状半地堑结构,呈多米诺骨牌式自南向北排列;并与其间近E-W走向的南京-南通-勿南沙和滨海-南黄海中部的崂山古生界地层的核部杂岩褶隆带,共同构成较大区域范围的盆-岭构造。这一期构造运动一方面再次改造了下扬子区海相古生代盆地,为海相古生界烃源岩系在经历了抬升剥蚀后的再次深埋,以及晚期二次生烃提供了可能性;另一方面也控制了中新生代油气的生成与聚集分布。

     

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出版历程
  • 收稿日期:  2015-08-10
  • 修回日期:  2015-11-24
  • 刊出日期:  2016-01-28

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