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下扬子区海相盆地改造与成藏关键要素

罗开平 黄泽光 吕俊祥 彭金宁 陆永德 周凌方

罗开平, 黄泽光, 吕俊祥, 彭金宁, 陆永德, 周凌方. 下扬子区海相盆地改造与成藏关键要素[J]. 石油实验地质, 2016, 38(6): 713-720. doi: 10.11781/sysydz201606713
引用本文: 罗开平, 黄泽光, 吕俊祥, 彭金宁, 陆永德, 周凌方. 下扬子区海相盆地改造与成藏关键要素[J]. 石油实验地质, 2016, 38(6): 713-720. doi: 10.11781/sysydz201606713
Luo Kaiping, Huang Zeguang, Lü Junxiang, Peng Jinning, Lu Yongde, Zhou Lingfang. Marine basin reformations and accumulation factors in Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(6): 713-720. doi: 10.11781/sysydz201606713
Citation: Luo Kaiping, Huang Zeguang, Lü Junxiang, Peng Jinning, Lu Yongde, Zhou Lingfang. Marine basin reformations and accumulation factors in Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(6): 713-720. doi: 10.11781/sysydz201606713

下扬子区海相盆地改造与成藏关键要素

doi: 10.11781/sysydz201606713
基金项目: 中国石化重大先导项目(G5800-13-ZS-TY)资助。
详细信息
    作者简介:

    罗开平(1964-),男,博士,高级工程师,从事石油地质综合研究。E-mail:luokp.syky@sinopec.com。

  • 中图分类号: TE121.1

Marine basin reformations and accumulation factors in Lower Yangtze region

  • 摘要: 下扬子区古生界海相盆地晚中生代(T2末)以来经历了晚印支-早燕山期(T3-J2)对冲挤压、中晚燕山期(J3-K1)左行走滑错移及喜马拉雅期(K2-E)伸展拆离3期性质完全不同的构造运动的变形改造,使得海相实体的赋存状况和地质结构极其复杂。与之对应,下扬子海相成烃-成藏分为加里东期-早印支期初次生烃-早期成藏、晚印支-燕山期破坏调整、早喜马拉雅期二次生烃-晚期成藏3个阶段。对黄桥、句容含油构造及泰山古油藏等典型解剖表明,现实的油气聚集主要以晚期成藏为主,海相实体赋存状况及其地质结构、有效烃源、有效保存条件成为晚期成藏的关键要素。

     

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出版历程
  • 收稿日期:  2015-11-05
  • 修回日期:  2016-08-11
  • 刊出日期:  2016-11-28

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