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青藏高原腹地长距离推覆及构造样式

吴珍汉,  赵珍,  季长军,  吴艳,  刘志伟,  李英烈,  陈云

吴珍汉,赵珍,季长军,等,2026. 青藏高原腹地长距离推覆及构造样式[J]. 地质力学学报,32(5):1004−1012 doi: 10.12090/j.issn.1006-6616.2026083
引用本文: 吴珍汉,赵珍,季长军,等,2026. 青藏高原腹地长距离推覆及构造样式[J]. 地质力学学报,32(5):1004−1012 doi: 10.12090/j.issn.1006-6616.2026083
WU Z H,ZHAO Z,JI C J,et al.,2026. Long displacement of thrusts and tectonic patterns in the central Tibetan Plateau[J]. Journal of Geomechanics,32(5):1004−1012 doi: 10.12090/j.issn.1006-6616.2026083
Citation: WU Z H,ZHAO Z,JI C J,et al.,2026. Long displacement of thrusts and tectonic patterns in the central Tibetan Plateau[J]. Journal of Geomechanics,32(5):1004−1012 doi: 10.12090/j.issn.1006-6616.2026083

青藏高原腹地长距离推覆及构造样式

doi: 10.12090/j.issn.1006-6616.2026083
基金项目: 国家科技重大专项(2025ZD1004600,2024ZD1001005);中国地质调查局地质调查项目(DD2026022104,DD20230315);陕西省煤田地质集团项目(SMDZ-2022ZD-8,SMDZ-2021-1);国家自然科学基金项目(U24A20597);西藏自治区科技计划项目(XZ202403ZY0040)
详细信息
    作者简介:

    吴珍汉(1965—),男,博士,研究员,构造地质与矿产地质专业,长期从事青藏高原区域地质调查、羌塘盆地油气地质调查、构造地质及应用研究。Email:zhenhanwu@cags.ac.cn

    通讯作者:

    吴珍汉(1965—),男,博士,研究员,构造地质与矿产地质专业,长期从事青藏高原区域地质调查、羌塘盆地油气地质调查、构造地质及应用研究。Email:zhenhanwu@cags.ac.cn

  • 中图分类号: P542

Long displacement of thrusts and tectonic patterns in the central Tibetan Plateau

Funds: This research was financially supported by the National Science and Technology Major Project (Grant Nos. 2025ZD1004600 and 2024ZD1001005), the Geological Survey Project of China Geological Survey (Grant Nos. DD2026022104 and DD20230315), the Project of Shaanxi Coal Geology Group (Grant Nos. SMDZ-2022ZD-8 and SMDZ-2021-1), the National Natural Science Foundation of China (Grant No. U24A20597), and the Science and Technology Plan Project of Xizang Autonomous Region (Grant No. XZ202403ZY0040).
More Information
    Author Bio:

    吴珍汉,中国地质科学院二级研究员,2025年荣获第十九次李四光地质科学奖科研奖。现任世界地质图委员会(CGMW)副主席,中国国际地球科学计划全国委员会秘书长,西藏自治区发展咨询委员会委员。长期从事青藏高原形成演化、构造地质及应用研究,主持完成西藏当雄幅1∶25万区域地质调查、青藏铁路沿线活动断层勘测与地应力测量及工程应用、青藏高原深部探测在矿产资源评价中的应用研究;创新提出羌塘盆地逆冲推覆构造成藏理论,发现富油裂缝型碳酸盐岩储层和厚达数百米的盐岩盖层,实现清水湖地区能源资源勘查重大突破。第一作者出版专著10部,核心期刊发表论文82篇;获国家科技进步特等奖1项、省部级一等奖1项、省部级二等奖4项,享受国务院政府特殊津贴

  • 摘要: 羌塘盆地广泛发育逆冲推覆构造,厘清该构造运动期次和样式对于羌塘盆地油气勘查具有重大意义。通过野外详细观测,结合二维地震综合解释表明,青藏高原腹地双湖地区晚白垩世和古近纪分别发育自北向南长距离逆冲推覆构造运动。晚白垩世形成比洛错−昂达尔错古油藏推覆体(BAPS),根部为蒂让碧错−雅曲南逆冲断裂(DST),构成DST-BAPS推覆构造,最小推覆距离为116 km,对应地壳缩短量≥54%;古近纪形成达沃错−吐错逆冲推覆构造(DTT),最小推覆距离为38 km,对应地壳缩短量≥53%。DST-BAPS和DTT均为薄皮推覆构造,中—下侏罗统厚层石膏对长距离推覆构造运动起到良好的滑脱作用。晚白垩世和古近纪逆冲推覆前锋分别发育前陆盆地及阿布山组、康托组磨拉石建造。双湖地区逆冲推覆构造对羌塘盆地中部油气成藏及保存条件具有重要控制作用。

     

  • 图  1  青藏高原构造单元及双湖地区位置图

    1—逆冲断层;2—走滑断层;SKS—南昆仑缝合带;HJS—可可西里−金沙江缝合带;BNS—班公−怒江缝合带;YZS—雅鲁藏布江缝合带;MBT—主边界断裂

    Figure  1.  Tectonic units of the Tibetan Plateau and location of the Shuanghu area

    1–thrust fault; 2–strike-slip fault; SKS–South Kunlun Suture; HJS–Hoh xil–Jinsha River Suture; BNS–Bangong–Nujiang Suture; YZS–Yaluzangbu Suture; MBT–Main Boundary Thrust

    图  2  青藏高原腹地双湖地区逆冲推覆构造纲要图

    1—逆冲断层;2—飞来峰;3—构造窗;4—背斜;5—向斜;6—古近纪火山岩;7—晚白垩世火山岩;8—古近纪花岗岩;9—晚三叠世花岗岩;10—古生代蛇绿岩套;11—现今湖泊;AB—二维地震解释剖面;BAPS—比洛错−昂达尔错古油藏推覆体;DST—蒂让碧错−雅曲南逆冲断裂;DTT—达沃错−吐错逆冲断裂;DQT—多玛−其香错逆冲断裂; Q—第四系;E3—渐新统(唢呐湖组);E1-2—古新统—始新统(康托组);K2—上白垩统(阿布山组);T—三叠系;P2—上二叠统;C-P—石炭系—二叠系;Pzm—古生界变质岩;$\gamma_5^1 $—三叠纪花岗岩;$\gamma_6^{1-2} $—古近纪花岗岩北羌塘坳陷侏罗系:J3—上侏罗统(索瓦组J3s与白龙冰河组J3b);J2—中侏罗统(夏里组J2x与布曲组J2b);J1—下侏罗统(雀莫错组)南羌塘坳陷侏罗系:J2-3—中—上侏罗统;J1q—曲色组

    Figure  2.  Schematic map of thrust nappe structures in the Shuanghu area, central Tibetan Plateau

    1–thrust fault; 2–nappe; 3–tectonic window; 4–anticline; 5–syncline; 6–Paleogene volcanic rock; 7–Late Cretaceous volcanic rock; 8–Paleogene granite; 9–Late Triassic granite; 10–Paleozoic ophiolite; 11–present lake; AB–cross-section inferred from a seismic reflection profile; BAPS– Bilo Co–Andar Co Paleo-petroliferous System; DST–Dirangbi Co–South Yaqu Thrust; DTT–Dawo Co–Tu Co Thrust; DQT–Duoma–Qixiang Co Thrust; Q–Quaternary; E3–Oligocene (Suonahu Formation); E1-2–Paleocene–Eocene (Kangtuo Formation); K2–Upper Cretaceous (Abushan Formation); T–Triassic; P2–Upper Permian; C–P–Permian–Carboniferous; Pzm–Paleozoic metamorphic rocks; $\gamma_5^1 $–Triassic granite; $\gamma_6^{1-2} $–Paleogene granite; J3–Upper Jurassic (Suowa Formation J3s and Bailongbinghe Formation J3b); J2–Middle Jurassic (Xiali Formation J2x and Buqu Formation J2b); J1–Lower Jurassic (Quemo Co Formation); J2-3–Upper–Middle Jurassic; J1q–Lower Jurassic Quse Formation

    图  3  雀尔茶卡北侧古近纪推覆构造照片(观测点位置见图2)

    J2x—中侏罗统夏里组;E1-2k—古新统—始新统康托组a—达沃错—吐错逆冲前陆红层沉积(镜向北东);b—中侏罗统夏里组推覆体下伏古近系康托组磨拉石建造(镜头向北)

    Figure  3.  Photos of a Paleogene thrust north of the Queerchaka (The location where the photos were taken is marked in Fig. 2)

    (a) Foreland redbeds at the southern DTT margin (view to the northeast); (b) Paleogene molasse deposits of the Kangtuo Formation beneath the nappe of the Middle Jurassic Xiali Formation (view to the north) J2x–Middle Jurassic Xiali Formation; E1-2k–Paleocene–Eocene Kangtuo Formation

    图  4  蒂让碧错西南侧晚白垩世逆冲推覆构造照片(观测点位置见图2)

    Gyp—石膏;K2a—上白垩统阿布山组;J2x—中侏罗统夏里组a—中侏罗统夏里组飞来峰(镜头向南);b—推覆体下伏上白垩统阿布山组磨拉石建造(镜向南西);c—夏里组推覆体底部石膏片岩(镜头向西)

    Figure  4.  Photos of a Late Cretaceous thrust southwest of the Dirangbi Co (The location where the photos were taken is marked in Fig. 2)

    (a) Nappe of the Middle Jurassic Xiali Formation (view to the south); (b) Upper Cretaceous molasse deposits of the Abushan Formation beneath the nappe (view to the southwest); (c) Gypsum schist of the lower nappe of the Xiali Formation (view to the west) Gyp–gypsum; K2a–Upper Cretaceous Abushan Formation; J2x–Middle Jurassic Xiali Formation

    图  5  双湖东侧地震测线AB地质构造剖面图

    BAPS—比洛错−昂达尔错古油藏推覆体;DST—蒂让碧错−雅曲南晚白垩世逆冲推覆构造;DTT—达沃错−吐错古近纪逆冲推覆构造;DQT—多玛−其香错逆冲断裂E3—渐新统;E1-2k—古新统—始新统康托组;K2a—上白垩统阿布山组;J3s—上侏罗统索瓦组;J2x—中侏罗统夏里组;J2b—中侏罗统布曲组;J1q—下侏罗统雀莫错组;T3nd—上三叠统那底岗日组;T2-3x—中—上三叠统肖茶卡组;C-P—石炭系—二叠系;Pz—古生界;T3—J1—上三叠统—下侏罗统;其他地质代号及剖面AB位置如图2

    Figure  5.  Geological cross-section along seismic profile AB east of Shuanghu

    BAPS–Bilo Co–Andar Co terrane bearing a paleo-oil reservoir; DST–Dirangbi Co–South Yaqu Thrust; DTT–Dawo Co–Tu Co Thrust; DQT– Duoma–Qixiang Co Thrust E3–Oligocene; E1-2k–Paleocene–Eocene Kangtuo Formation; K2a–Upper Cretaceous Abushan Formation; J3s–Upper Jurassic Suowa Formation; J2x–Middle Jurassic Xiali Formation; J2b–Middle Jurassic Buqu Formation; J1q–Lower Jurassic Quemo Co Formation; T3nd–Upper Triassic Nadigangri Formation; T2-3x–Middle–Upper Triassic Xiaochaka Formation; C–P–Permian–Carboniferous; Pz–Paleozoic; T3–J1–Upper Triassic–Lower Jurassic; The locations of the other symbols and the AB profile are shown in Fig. 2.

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出版历程
  • 收稿日期:  2026-06-30
  • 修回日期:  2026-10-04
  • 录用日期:  2026-10-05
  • 预出版日期:  2026-10-10
  • 刊出日期:  2026-10-28

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