武威盆地儿马湖凹陷构造演化与热史模拟

雒春雨, 宋立军, 杨浩, 史婵媛, 张欢. 2022. 武威盆地儿马湖凹陷构造演化与热史模拟. 西北地质, 55(4): 194-203. doi: 10.19751/j.cnki.61-1149/p.2022.04.017
引用本文: 雒春雨, 宋立军, 杨浩, 史婵媛, 张欢. 2022. 武威盆地儿马湖凹陷构造演化与热史模拟. 西北地质, 55(4): 194-203. doi: 10.19751/j.cnki.61-1149/p.2022.04.017
LUO Chunyu, SONG Lijun, YANG Hao, SHI Chanyuan, ZHANG Huan. 2022. Tectonic Evolution and Thermal History Simulation of Ermahu Sag, Wuwei Basin. Northwestern Geology, 55(4): 194-203. doi: 10.19751/j.cnki.61-1149/p.2022.04.017
Citation: LUO Chunyu, SONG Lijun, YANG Hao, SHI Chanyuan, ZHANG Huan. 2022. Tectonic Evolution and Thermal History Simulation of Ermahu Sag, Wuwei Basin. Northwestern Geology, 55(4): 194-203. doi: 10.19751/j.cnki.61-1149/p.2022.04.017

武威盆地儿马湖凹陷构造演化与热史模拟

  • 基金项目:

    西安石油大学研究生创新实践资助项目(YCS19112023)资助。

详细信息
    作者简介: 雒春雨(1996-),女,硕士研究生,主要从事盆地分析研究。E-mail:247378921@qq.com。
    通讯作者: 宋立军(1977-),男,博士,教授,主要从事盆地分析及模拟研究。E-mail:8210954@qq.com。
  • 中图分类号: P542.1

Tectonic Evolution and Thermal History Simulation of Ermahu Sag, Wuwei Basin

More Information
  • 儿马湖凹陷位于武威盆地北部凹陷西部的一个次级构造单元,该凹陷石炭系煤系地层发育,有一定油气勘探潜力。笔者利用平衡剖面技术和盆地成藏模拟技术,对该地区的构造演化和热史进行了研究。研究揭示:①儿马湖凹陷为一个受多条北东向正断层控制发育的复式断陷;②该凹陷经历了4个阶段:石炭纪—二叠纪裂陷阶段、三叠纪—早中侏罗世抬升剥蚀阶段、晚侏罗世—白垩纪二次裂陷阶段和古近纪—新近纪—第四纪坳陷阶段。③儿马湖凹陷石炭系烃源岩热演化程度较高,二叠纪末期进入生油阶段,三叠纪末期已经进入生气阶段,现今整体处于高成熟-过成熟阶段。本研究对该凹陷、武威盆地及走廊盆地形成演化认识和油气勘探具有一定参考价值。
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出版历程
收稿日期:  2021-05-12
修回日期:  2021-11-01

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