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    鄂尔多斯盆地北部东胜气田构造变形时序及关键构造期构造特征

    刘昭茜 马立元 何新月 温立峰 唐永 郑荣臣 任玉婷 罗星

    刘昭茜, 马立元, 何新月, 温立峰, 唐永, 郑荣臣, 任玉婷, 罗星, 2023. 鄂尔多斯盆地北部东胜气田构造变形时序及关键构造期构造特征. 地球科学, 48(2): 533-552. doi: 10.3799/dqkx.2022.416
    引用本文: 刘昭茜, 马立元, 何新月, 温立峰, 唐永, 郑荣臣, 任玉婷, 罗星, 2023. 鄂尔多斯盆地北部东胜气田构造变形时序及关键构造期构造特征. 地球科学, 48(2): 533-552. doi: 10.3799/dqkx.2022.416
    Liu Zhaoqian, Ma Liyuan, He Xinyue, Wen Lifeng, Tang Yong, Zheng Rongchen, Re Yuting, Luo Xing, 2023. Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China. Earth Science, 48(2): 533-552. doi: 10.3799/dqkx.2022.416
    Citation: Liu Zhaoqian, Ma Liyuan, He Xinyue, Wen Lifeng, Tang Yong, Zheng Rongchen, Re Yuting, Luo Xing, 2023. Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China. Earth Science, 48(2): 533-552. doi: 10.3799/dqkx.2022.416

    鄂尔多斯盆地北部东胜气田构造变形时序及关键构造期构造特征

    doi: 10.3799/dqkx.2022.416
    基金项目: 

    中石化科技部项目“东胜气田精细表征及有效开发技术” P20065-2

    国家科技重大专项课题“中西部地区碎屑岩层系油气富集规律与勘探方向” 2016ZX05002-006

    中石化科技项目部“鄂尔多斯盆地中石化探区上古生界致密气富集规律与目标优选” P21088-3

    湖北省自然科学基金创新群体项目 2021CFA031

    详细信息
      作者简介:

      刘昭茜(1982-),女,副教授,从事石油与天然气地质学、构造与成藏年代学、有机地球化学研究.E-mail:liuzhaoqian@cug.edu.cn

    • 中图分类号: P618.13

    Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China

    • 摘要: 鄂尔多斯盆地北部杭锦旗地区东胜气田上古生界致密砂岩层系具有丰富的油气资源,但其三面环山,经历了多期次、多方向、多属性构造作用,具有构造改造差异性大、储层致密、非均质性强、烃类聚集与改造复杂、差异性大等油气地质特征.基于与周边构造体系关系、地层接触关系、三维地震、古地貌、构造年代学分析,对鄂北杭锦旗地区东胜气田开展构造变形时序、方式、关键构造期及其构造特征研究. 明确了3组主干断裂性质和活动时间:(1)EW-NEE向断裂晚侏罗世为压扭断层,晚白垩世-喜山早期为张扭断层;(2)NW-NWW向断裂为晚白垩世-喜山早期张扭走滑断层;(3)NE-近SN向断裂早白垩世为压扭断层,晚白垩世-喜山早期为张扭断层. 厘定了东胜气田晚侏罗世、早白垩世、晚白垩世-喜山早期三期构造变形时序及方式. 确定了燕山早期(J3-K1)和燕山晚期-喜山早期(K2-E1)是与上古生界致密砂岩天然气成藏密切相关的关键构造期,其对天然气成藏、改造的作用方式、空间影响范围、作用结果存在差异.

       

    • 图  1  鄂尔多斯盆地北部杭锦旗区块和东胜气田构造位置

      Fig.  1.  Tectonic locations of Hangjinqi area and Dongsheng gas field in the northern Ordos Basin

      图  2  杭锦旗地区上古生界底界面(T9bc)二维地震构造平面图及东胜气田30井区、72-51井区三维地震工区位置

      Fig.  2.  Structural map of the Upper Paleozoic bottom reflections (T9bc) in Hangjinqi area based on 2D seismic and the locations of 72-51 and 30 well blocks' 3D seismic areas

      图  3  杭锦旗地区主干断裂的二维地震剖面特征

      剖面位置见图 2

      Fig.  3.  2D seismic sections of the main faults in Hangjinqi area

      图  4  鄂尔多斯盆地北部地区周缘构造体系及盆地内部构造年代学数据平面分布图

      数据来源:张进江等(2009)刘建辉(2009)Davis and Darby(2010)邹和平等(2010)乔建新(2013)宋子升(2013)曹现志(2014)王少轶等(2020);东胜和杭锦旗附近6个磷灰石裂变径迹年龄为本次实测数据

      Fig.  4.  Tectonic chronology ages plotted on geologic map of the western, eastern, and northern margin tectonic systems and the northern area in Ordos Basin

      图  5  鄂尔多斯盆地北部东缘EW向骨架剖面和东缘地层接触关系剖面图

      地质剖面据廖昌珍等(2007)修编

      Fig.  5.  EW-trend cross sections and variation characteristics of stratigraphic contact relationship in eastern margin of the northern Ordos Basin

      图  6  鄂尔多斯盆地北部西缘EW向骨架构造剖面和西缘地层接触关系剖面图

      地质剖面据马静辉和何登发(2019)修编;地震剖面据侯旭波等(2014)

      Fig.  6.  EW-trend direction cross sections and variation characteristics of stratigraphic contact relationship in western margin of the Northern Ordos Basin

      图  7  鄂尔多斯盆地北部与石拐盆地地层接触关系对比及SN向地质剖面图

      地层柱状图据王永超(2017)修编;剖面A据乔建新(2013)许传鑫(2020)修编;剖面B据刘正宏等(2009)修编

      Fig.  7.  Stratigraphic contact relationships correlation between the northern Ordos Basin and Shiguai Basin, and the SN-trend direction cross sections

      图  8  东胜气田30井区T4界面(中侏罗统直罗组底界)和T9bc界面(上古生界底界)断裂发育对比图

      Fig.  8.  Fault system comparison between the Middle Jurassic bottom (T4) and the Upper Paleozoic bottom (T9bc) of 30 well block in Dongsheng gas field

      图  9  东胜气田72-51井区T4界面(中侏罗统直罗组底界)和T9bc界面(上古生界底界)断裂发育对比图

      Fig.  9.  Fault system comparison between the Middle Jurassic bottom (T4) and the Upper Paleozoic bottom (T9bc) of 72-51 well block in Dongsheng gas field

      图  10  东胜气田上古生界及以上地层主干断裂立体图

      图a为30井区;图b为72-51井区;显示界面均为上古生界底界;井区位置见图 2

      Fig.  10.  3D stereogram of main faults in Upper Paleozoic and above strata in Dongsheng gas field

      图  11  东胜气田72-51井区EW-NEE向和NW-NWW向断裂立体图

      a 为EW-NEE向断裂侧视图;b 为EW-NEE向断裂俯视图;c 为NW-NWW向断裂俯视图;井区位置见图 2

      Fig.  11.  3D stereogram of EW-NEE-trend and NW-NWW-trend faults in 72-51 well block, Dongsheng gas field

      图  12  东胜气田72-51井区EW-NEE向断裂局部特征线描剖面图

      井区位置见图 2,备注:因浅层地震资料品质差,下白垩统仅对下部部分地层进行了线描

      Fig.  12.  Local characteristic line drawing of EW-NEE-trend faults in 72-51 well block, Dongsheng gas field

      图  13  东胜气田72-51井区NW向和NWW向断裂局部特征线描剖面图

      井区位置见图 2,备注:因浅层地震资料品质差,下白垩统仅对下部部分地层进行了线描

      Fig.  13.  Local characteristic line drawing of NW-trend and NWW-trend faults in 72-51 well block, Dongsheng gas field

      图  14  30井区近EW-NWW走向断裂局部特征线描剖面图

      井区位置见图 2;因浅层地震资料品质差,下白垩统仅对下部部分地层进行了线描

      Fig.  14.  Local characteristic line drawing of EW-NWW-trend faults in 30 well block, Dongsheng gas field

      图  15  72-51井NE-近SN向断裂局部特征线描剖面图

      井区位置见图 2;因浅层地震资料品质差,下白垩统仅对下部部分地层进行了线描

      Fig.  15.  Local characteristic line drawing of NE-SN-trend faults in 72-51 well block, Dongsheng gas field

      图  16  东胜气田72-51井区侏罗世末期和早白垩世末期古地貌特征图

      Fig.  16.  Latest Jurassic and latest Early Cretaceous Paleogeomorphic characteristics of the 72-51 well block in Dongsheng gas field

      图  17  鄂尔多斯盆地北部东胜气田SN向和EW向构造演化剖面图

      Fig.  17.  SN-trend and EW-trend tectonic evolution sections of Dongsheng gas field in the northern Ordos Basin

      图  18  鄂尔多斯盆地北部东胜气田30井区T9bc界面(上古生界底界)关键构造期古构造图

      右图上钻井显示级别为该井最高显示级别

      Fig.  18.  Critical tectonic periods paleotectonic map of the Upper Paleozoic bottom (T9bc) of 30 well block in Dongsheng gas field, northern Ordos Basin

      图  19  鄂尔多斯盆地北部东胜气田72-51井区T9bc界面(上古生界底界)关键构造期古构造图

      右图上钻井显示级别为该井最高显示级别

      Fig.  19.  Critical tectonic periods paleotectonic map of the Upper Paleozoic bottom (T9bc) of 72-51 well block in Dongsheng gas field, northern Ordos Basin

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    • 收稿日期:  2022-11-29
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