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    巴里坤盆地地层展布规律和构造格架的综合地球物理认识

    杨小鹏 梅岩辉 李世超 姜鹍鹏 赵庆英

    杨小鹏, 梅岩辉, 李世超, 姜鹍鹏, 赵庆英, 2019. 巴里坤盆地地层展布规律和构造格架的综合地球物理认识. 地球科学, 44(12): 4222-4234. doi: 10.3799/dqkx.2019.169
    引用本文: 杨小鹏, 梅岩辉, 李世超, 姜鹍鹏, 赵庆英, 2019. 巴里坤盆地地层展布规律和构造格架的综合地球物理认识. 地球科学, 44(12): 4222-4234. doi: 10.3799/dqkx.2019.169
    Yang Xiaopeng, Mei Yanhui, Li Shichao, Jiang Kunpeng, Zhao Qingying, 2019. Comprehensive Geophysical Study on Stratigraphic Distribution Regularities and Tectonic Frameworks in Barkol Basin. Earth Science, 44(12): 4222-4234. doi: 10.3799/dqkx.2019.169
    Citation: Yang Xiaopeng, Mei Yanhui, Li Shichao, Jiang Kunpeng, Zhao Qingying, 2019. Comprehensive Geophysical Study on Stratigraphic Distribution Regularities and Tectonic Frameworks in Barkol Basin. Earth Science, 44(12): 4222-4234. doi: 10.3799/dqkx.2019.169

    巴里坤盆地地层展布规律和构造格架的综合地球物理认识

    doi: 10.3799/dqkx.2019.169
    基金项目: 

    中国地质调查局项目 121201229000160018

    国家自然科学基金项目 41872234

    详细信息
      作者简介:

      杨小鹏(1993-), 男, 硕士研究生, 主要从事地球物理和石油地质研究

      通讯作者:

      李世超

    • 中图分类号: P581

    Comprehensive Geophysical Study on Stratigraphic Distribution Regularities and Tectonic Frameworks in Barkol Basin

    • 摘要: 巴里坤盆地夹持于麦钦乌拉岛弧和哈尔里克岛弧之间,其地层展布、断裂构造、油气成藏、盆山关系均不明确.使用大地电磁测深、航磁、地震等方法对其开展综合研究.研究表明:新生界沉积较薄,中生界及上二叠统地层从盆地中心向四周逐渐减薄,下二叠统和石炭系地层山前沉积略厚、向南逐渐变薄;盆地内部存在12条断裂,大多数为近东西走向的逆冲断裂,这些断裂构成研究区的基本构造格架;盆地可划分为北部斜坡、哈尔里克逆冲带、巴里坤坳陷三个二级构造单元;巴里坤坳陷大河构造为油气成藏的有利区域;南边哈尔里克山呈北西向向盆地内逆冲推覆,与盆地以哈尔里克断裂为界,盆地与北边麦钦乌拉山与以麦钦乌拉断裂为界,与西边博格达山以冬屋断裂为界.

       

    • 图  1  巴里坤盆地构造位置图

      Fig.  1.  Location map of the Barkol basin

      图  2  巴里坤盆地地质简图

      Fig.  2.  Geological map of the Barkol Basin

      图  3  巴里坤盆地航磁ΔT等值线平面图

      Fig.  3.  Aeromagnetic ΔT contour map of the Barkol basin

      图  4  巴里坤盆地地震反射剖面解释图

      Fig.  4.  The seismic reflection section interpretation map of the Barkol basin

      图  5  巴里坤盆地CEMP测线部署图

      Fig.  5.  CEMP line deployment map of the Barkol basin

      图  6  CEMP05线测线综合解释剖面图

      Fig.  6.  Comprehensive interpretation section of line CEMP05

      图  7  CEMPL01线测线综合解释剖面

      Fig.  7.  Comprehensive interpretation section of line CEMPL01

      图  8  巴里坤盆地新生界底界面海拔埋深

      Fig.  8.  Elevation depth map of the Cenozoic bottom boundary in the Barkol basin

      图  9  巴里坤盆地中生界-上二叠统地层厚度分布

      Fig.  9.  Distribution of the Mesozoic-Upper Permian stratum thickness in the Barkol basin

      图  10  巴里坤盆地下二叠统-石炭系地层厚度分布

      Fig.  10.  Distribution of the Lower Permian-Carboniferous strata in the Barkol basin

      图  11  巴里坤盆地石炭系底界面埋深厚度

      Fig.  11.  Thickness map of the Carboniferous bottom boundary interface in the Barkol basin

      图  12  巴里坤盆地断裂展布

      Fig.  12.  Distribution of faults in the Barkol basin

      图  13  巴里坤盆地构造单元划分和石炭系油气远景预测图

      Fig.  13.  Block diagram of the structural unit and carbonate prospective map of the Carboniferous in the Barkol basin

      图  14  哈尔里克山和麦钦乌拉山电法剖面

      Fig.  14.  Electrical section map of Mt. Harlic and Mt. Maqinwula

      表  1  巴里坤盆地构造单元划分

      Table  1.   Structural units in the Barkol basin

      构造单元 面积(km2) 石炭系底界最大埋深(m) P1+C厚度(m)
      Ⅰ级 Ⅱ级 Ⅲ级
      北部斜坡 825 0 0~1 700
      巴里坤盆地 巴里坤坳陷 冬屋断隆 221 0 1 200~2100
      萨尔乔克斜坡 373 0 500~1500
      巴里坤凹陷 426 -2 400 900~2100
      大河构造(隆起) 402 -600 1 200~1800
      奎苏断凹 426 -2 000 1 200~1800
      哈尔里克逆冲带 417 0 0~900
      注:(1)构造单元面积通过Suffer和奥维地图软件测量;(2)石炭系底界最大埋深和P1+C厚度是通过Suffer(二维)和Geosoft(三维)软件相结合测量11条电法剖面所得;(3)石炭系底界最大埋深测量误差为±300 m,P1+C厚度测量误差为600 m.
      下载: 导出CSV
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