中国地质调查局西安地质调查中心主办
高级检索

武威盆地儿马湖凹陷构造演化与热史模拟

,  ,  ,  , 

文章导航 > 西北地质 > 2022 > 55(4): 194-203

上一篇

下一篇

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
shu
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
shu

武威盆地儿马湖凹陷构造演化与热史模拟

  • 1. 西安石油大学地球科学与工程学院, 陕西 西安 710065;

  • 2. 陕西省油气成藏重点实验室, 陕西 西安 710065;

  • 3. 中国冶金地质总局中南局, 湖北 武汉 430081;

  • 4. 长庆油田分公司勘探开发研究院, 陕西 西安 710018

  • 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

  • 1. School of Earth Science and Engineering, Xi'an Shiyou University, Xi'an 710065, Shaan Xi, China;

  • 2. Shaanxi Provincial Key Laboratory of Oil and Gas Accumulation, Xi'an Shiyou University, Xi'an 710065, ShaanXi, China;

  • 3. Central South Bureau, General Administration of Metallurgy and Geology of China, Wuhan 430081, Hubei, China;

  • 4. Research Institute of Exploration and Development, Changqing Oilfield Company, Xi'an 710018, ShaanXi, China

More Information

    摘要
  • 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。
    Ermahu depression is located in a secondary structural unit in the west of the northern depression of Wuwei Basin. The Carboniferous coal measure strata are developed in this depression, and there is a certain potential for CBM exploration. However, for a long time, the structural evolution process and the maturity history of organic matter in this depression have not been studied. In this paper, the structural evolution and thermal history of this area have been studied by using the balanced profile technique and reservoir forming simulation technique. The results show that:①Erma Lake depression is a compound fault depression controlled by several NE trending normal faults; ②The depression experienced four stages: Carboniferous-Permian rifting stage, Triassic-Early-Middle Jurassic uplifting and denudation stage, Late Jurassic-Early Cretaceous secondary rifting stage and Tertiary-Quaternary depression stage; ③The thermal evolution of the Carboniferous source rocks in the Ermahu Sag is relatively high. The Carboniferous source rocks entered the stage of oil generation at the end of Permian, and entered the stage of gas generation at the end of Triassic, and are currently in the stage of high maturity-over-maturity.
    • HTML全文
  • 加载中
    • 参考文献(33)

  • 陈文彬.河西走廊及邻近地区最新构造变形基本特征及构造成因分析[D].北京：中国地震局地质研究所,2003.

    CHEN Wenbin. Basic characteristics of latest tectonic deformation and analysis of tectonic genesis in Hexi Corridor and its adjacent areas [D]. Beijing: Institute of Geology, China Earthquake Administration, 2003.

    杜治利,陈夷,田亚,等.武威盆地北部坳陷致密气勘探前景[J].中国矿业,2018,27(S1):92-97.

    DU Zhili, CHEN Yi, TIAN Ya,et al. Exploration prospect of tight gas in northern depression of Wuwei Basin [J]. China Mining Industry, 2018,27(S1):92-97.

    胡峰,龙思萍,王雪梅,等.武威盆地儿马湖凹陷石炭系页岩气资源潜力及沉积相分析[J].复杂油气藏,2019,12(04):19-23.

    HU Feng, LONG Siping, WANG Xuemei, et al. Analysis of Carboniferous shale gas resource potential and sedimentary facies in Ermahu Sag, Wuwei Basin [J]. Complex Oil and Gas Reservoir, 2019,12(04):19-23.

    龚全胜,刘明强,梁明宏,等.北山造山带大地构造相及构造演化[J].西北地质,2003,(01):11-17.

    GONG Quansheng, LIU Mingqiang, LIANG Minghong, et al. Tectonic facies and tectonic evolution of Beishan orogenic belt [J]. Northwestern Geology,2003,(01):11-17.

    黄汲清.对中国大地构造特点的一些认识并着重讨论地槽褶皱带的多旋回发展问题[J].地质学报,1979,(02):99-111.

    HUANG Jiqing. Some understandings of China's geotectonic characteristics with emphasis on the multicycle development of geosynclinal fold belt [J]. Acta Geologica Sinica, 1979,(02):99-111.

    裴先治,吴汉泉,左国朝.北祁连早古生代俯冲杂岩带的变形特征与构造演化[J].西安工程学院学报,1999,(01):11-14+19.

    PEI Xianzhi, WU Hanquan, ZUO Guochao. Deformation characteristics and tectonic evolution of Early Paleozoic subduction complex belt in North Qilian [J]. Journal of Xi'an Institute of Technology, 1999,(01):11-14+19.

    彭媛媛,康志宏,李伟奇,等.武威盆地石炭系泥页岩元素地球化学特征及意义[J].现代地质,2017,31(03):574-586.

    PENG Yuanyuan, KANG Zhihong, LI Weiqi, et al. Geochemical characteristics and significance of Carboniferous shale in Wuwei Basin [J]. Modern Geology, 2017,31(03):574-586.

    何世平,周会武,任秉琛,等.甘肃内蒙古北山地区古生代地壳演化[J].西北地质,2005,(03):6-15.

    HE Shiping, ZHOU Huiwu, REN Bingchen, et al. Paleozoic crustal evolution in Beishan area of Inner Mongolia, Gansu Province [J]. Northwest Geology, 2005,(03):6-15.

    孙知明,李海兵,裴军令,等.阿尔金断裂走滑对青藏高原东北缘山脉形成的古地磁证据[J].岩石学报,2012,28(6):1928-1936.

    SUN Zhiming, LI Haibing, PEI Junling, et al. Paleomagnetic evidence of strike-slip of Altun fault on the formation of mountains in the northeastern margin of Qinghai-Tibet Plateau [J]. Acta Petrologica Sinica, 2012,28(6): 1928-1936.

    王博.武威盆地石炭系烃源岩地球化学特征研究[D].西安石油大学，2017.

    WANG Bo. Geochemical characteristics of Carboniferous source rocks in Wuwei Basin[D]. Xi'an Shiyou University, 2017.

    王同和.河西走廊拉分盆地的构造演化与油藏分布[J].石油与天然气地质,1987,(03):271-280.

    WANG Tonghe. Structural evolution and reservoir distribution of the pull-apart basin in Hexi Corridor [J]. Petroleum and Natural Gas Geology, 1987,(03):271-280.

    阎存凤,袁剑英.武威盆地石炭系沉积环境及含油气远景[J].天然气地球科学,2011,22(02):267-274.

    YAN Cunfeng, YUAN Jianying. Carboniferous sedimentary environment and petroleum prospect in Wuwei basin [J]. Natural Gas Geoscience, 2011,22(02):267-274.

    马晓军,梁积伟,李建星,等.鄂尔多斯盆地中西部中新生代构造抬升及演化[J].西北地质,2019,52(04):127-136.

    MA Xiaojun, LIANG Jiwei, LI Jianxing, et al. Mesozoic and Cenozoic tectonic uplift and evolution in the central and western Ordos Basin [J]. Northwestern Geology, 2019,52(04):127-136.

    杨振宇,袁伟,仝亚博,等.阿拉善地块前中生代构造归属的新认识[J].地球学报,2014,35(06):673-681.

    YANG Zhenyu, YUAN Wei, TONG Yabo, et al. Rebecca. New understanding of pre-Mesozoic tectonic attribution of Alashan block [J].Acta Geologica Sinica, 2014,35(06):673-681.

    左国朝,吴汉泉.北祁连中段早古生代双向俯冲-碰撞造山模式剖析[J].地球科学进展,1997,(04):13-21.

    ZUO Guochao, WU Hanquan. Analysis of Early Paleozoic bidirectional subduction-collision orogeny model in the middle part of North Qilian Mountains [J].Advances in Geosciences, 1997,(04):13-21.

    陈小慧.松辽盆地南部梨树断陷深层油气成因与成藏研究[D].荆州：长江大学,2011.

    CHEN Xiaohui. Study on deep oil and gas genesis and accumulation in Lishu fault depression in southern Songliao Basin [D].Jinzhou: Yangtze University, 2011.

    LIU Jing,YANG Zhenyu, TONG Yabo, YUAN Wei, WANG Bin.Tectonic implications of early-middle Triassic palaeo-magnetic results from Hexi Corridor, North China[J]. Geophysical Journal International, 2010,182(3):1216-1228.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  679
  • PDF下载数:  99
  • 施引文献:  0
出版历程
收稿日期:  2021-05-12
修回日期:  2021-11-01

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回