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    阿尔金造山带中-新元古代沉积地层构造变形特征及其指示意义

    郝江波 李宇科 王超 冀文斌 乔元栋 喻遵谱 孙晓奎 张帅

    郝江波, 李宇科, 王超, 冀文斌, 乔元栋, 喻遵谱, 孙晓奎, 张帅, 2025. 阿尔金造山带中-新元古代沉积地层构造变形特征及其指示意义. 地球科学, 50(9): 3679-3690. doi: 10.3799/dqkx.2025.158
    引用本文: 郝江波, 李宇科, 王超, 冀文斌, 乔元栋, 喻遵谱, 孙晓奎, 张帅, 2025. 阿尔金造山带中-新元古代沉积地层构造变形特征及其指示意义. 地球科学, 50(9): 3679-3690. doi: 10.3799/dqkx.2025.158
    Hao Jiangbo, Li Yuke, Wang Chao, Ji Wenbin, Qiao Yuandong, Yu Zunpu, Sun Xiaokui, Zhang Shuai, 2025. Structural Deformation Characteristics and Its Implications of Meso- to Neoproterozoic Sedimentary Strata in the Altyn Tagh Orogenic Belt. Earth Science, 50(9): 3679-3690. doi: 10.3799/dqkx.2025.158
    Citation: Hao Jiangbo, Li Yuke, Wang Chao, Ji Wenbin, Qiao Yuandong, Yu Zunpu, Sun Xiaokui, Zhang Shuai, 2025. Structural Deformation Characteristics and Its Implications of Meso- to Neoproterozoic Sedimentary Strata in the Altyn Tagh Orogenic Belt. Earth Science, 50(9): 3679-3690. doi: 10.3799/dqkx.2025.158

    阿尔金造山带中-新元古代沉积地层构造变形特征及其指示意义

    doi: 10.3799/dqkx.2025.158
    基金项目: 

    国家自然科学基金项目 42402202

    山西省基础研究计划项目 202403021222259

    详细信息
      作者简介:

      郝江波(1989—),男,博士,讲师,主要从事前寒武纪地质学与超大陆演化、岩石学与矿物学研究. ORCID:0009-0001-3828-0971. E-mail:jbohao@nwu.edu.cn

    • 中图分类号: P548

    Structural Deformation Characteristics and Its Implications of Meso- to Neoproterozoic Sedimentary Strata in the Altyn Tagh Orogenic Belt

    • 摘要: 为了解阿尔金造山带中-新元古代与罗迪尼亚(Rodinia)超大陆聚合与裂解相关的构造演化过程,对该地区塔昔达坂群(1 080~950 Ma)与索尔库里群(~930 Ma)进行了野外地质填图和构造解析,结果显示塔昔达坂群为一套低绿片岩相副变质岩,并经历了三期构造变形:第一期(D1)以透入性片理S1置换原生层理S0;第二期(D2)受NNE-SSW挤压形成近WNW-ESE向褶皱及褶劈理S2;第三期(D3)表现为SE-NW向挤压的逆冲断层及直立褶皱.索尔库里群不整合覆盖于塔昔达坂群之上,两者之间存在着沉积环境、构造变形的不连续性.结合两者的物质组成、变形期次以及研究区新元古代早期岩浆岩的时空分布及形成环境,提出阿尔金地区中元古代晚期-新元古代早期完成了从活动大陆边缘到后碰撞伸展的构造转换过程,为约束其与Rodinia超大陆裂解-碰撞过程及其古地理归属提供了关键证据.

       

    • 图  1  阿尔金造山带地质简图

      图据Wang et al.(2013);NA. 北阿尔金地块;NASB. 北阿尔金俯冲混杂岩带;CAM. 中阿尔金地块;SASB. 南阿尔金俯冲碰撞杂岩带

      Fig.  1.  Geological and tectonic map of Altyn Tagh Orogenic Belt

      图  2  巴什尧勒地区塔昔达坂群和索尔库里群剖面(a);塔昔达坂群和索尔库里群典型岩石野外照片与接触关系(b~g)

      Fig.  2.  Geological profile showing the Taxidaban and Suoerkuli groups in the Bashenyaole area (a) and field photographs of typical rocks and field relationship of the Taxidaban and Suoerkuli groups (b‒g)

      图  3  塔昔达坂群金雁山组红土风化壳(a)和岩石风化碎块(b);索尔库里群与塔昔达坂群呈不整合接触(c)

      Fig.  3.  Lateritic weathering crust in the Jinyanshan Formation (a) of the Taxidaban Group, and weathered rock debris (b); unconformable contact (c) between the Suoerkuli Group and the Taxidaban Group

      图  4  冰沟南地区索尔库里群剖面(a);乱石山组底部砾岩(b);乱石山组火山岩夹层(c);小泉达坂岩屑石英砂岩(d)

      Fig.  4.  Geological profile showing the Suoerkuli groups (a) in the Binggounan area; basal conglomerate and interbedded volcanic rocks (b‒c) in the Luanshishan Formation; lithic quartz sandstone (d) of the Xiaoquandaban Formation

      图  5  中阿尔金地块塔昔达坂群S0面理露头尺度构造变形特征

      Fig.  5.  Outcrop-scale structural deformation characteristics of S₀ foliation in the Taxidaban Group, Central Altyn Block

      图  6  中阿尔金地块塔昔达坂群多期构造事件的野外表现及构造要素的赤平投影结果,赤平投影结果为等角度下半球投影

      Fig.  6.  Polyphase structural style and stereographic projection results (equal-angle lower-hemisphere projections) of tectonic elements in the Taxidaban Group, Central Altyn Block

      图  7  中阿尔金地块中元古代晚期‒新元古早期构造演化模型

      Fig.  7.  Tectonic evolutionary model of the Central Altyn Block during the late Mesoproterozoic to early Neoproterozoic

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    • 收稿日期:  2025-05-03
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