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塔里木盆地塔中隆起中北部地区断裂构造特征及演化

姜忠正 唐大卿 沙旭光 沈向存 罗少辉 董科良 古再丽努尔·艾尔肯 王玮龙 伍亮

姜忠正, 唐大卿, 沙旭光, 沈向存, 罗少辉, 董科良, 古再丽努尔·艾尔肯, 王玮龙, 伍亮. 塔里木盆地塔中隆起中北部地区断裂构造特征及演化[J]. 地质科技通报, 2024, 43(3): 120-132. doi: 10.19509/j.cnki.dzkq.tb20220663
引用本文: 姜忠正, 唐大卿, 沙旭光, 沈向存, 罗少辉, 董科良, 古再丽努尔·艾尔肯, 王玮龙, 伍亮. 塔里木盆地塔中隆起中北部地区断裂构造特征及演化[J]. 地质科技通报, 2024, 43(3): 120-132. doi: 10.19509/j.cnki.dzkq.tb20220663
JIANG Zhongzheng, TANG Daqing, SHA Xuguang, SHEN Xiangcun, LUO Shaohui, DONG Keliang, GUZAILINUER·Aierken, WANG Weilong, WU Liang. Structure and evolution of faults in central and northern parts of Tazhong Uplift, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 120-132. doi: 10.19509/j.cnki.dzkq.tb20220663
Citation: JIANG Zhongzheng, TANG Daqing, SHA Xuguang, SHEN Xiangcun, LUO Shaohui, DONG Keliang, GUZAILINUER·Aierken, WANG Weilong, WU Liang. Structure and evolution of faults in central and northern parts of Tazhong Uplift, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 120-132. doi: 10.19509/j.cnki.dzkq.tb20220663

塔里木盆地塔中隆起中北部地区断裂构造特征及演化

doi: 10.19509/j.cnki.dzkq.tb20220663
基金项目: 

中国石化科技项目 P22126

国家重点基础研究发展计划(973)项目 2012CB214804

详细信息
    作者简介:

    姜忠正, E-mail: 182351295@qq.com

    通讯作者:

    唐大卿, E-mail: tangdqcug@sina.com

  • 中图分类号: P542.3

Structure and evolution of faults in central and northern parts of Tazhong Uplift, Tarim Basin

More Information
  • 摘要:

    为系统揭示塔里木盆地塔中隆起中北部地区断裂构造特征及其成因演化, 通过对该区大连片三维地震工区精细构造解析和相干体等分析, 并结合区域动力背景, 系统论述了该区的断裂构造类型、几何学特征、差异活动机制及其构造演化过程。研究结果表明, 塔中隆起中北部发育了4类7期断裂构造, 其中逆冲断裂和走滑断裂尤其发育。平面上北西向弧形逆冲断裂与北东向、北西向及南北向走滑断裂相互交切与耦合; 垂向上断裂分层差异活动特征明显, 下奥陶统及其以下地层, 断裂发育数量多且以线形为主, 中奥陶统-中下泥盆统多呈雁列式, 上泥盆统-二叠系仅在塔中Ⅱ号断裂带、顺北5号断裂带西南端等地区发育少量断裂。研究区断裂活动受多期、多方向不同性质应力场所控制, 经历了极其复杂的演化历史: 加里东早期以塔中Ⅱ号断裂带等少量北倾正断层活动为主; 加里东中期Ⅰ幕断裂活动强烈, 表现为逆冲断裂与走滑断裂协同演化和相互耦合特征, 走滑断裂对逆冲断裂的切割或限制作用明显; 加里东中期Ⅲ幕断裂活动基本继承了加里东中期Ⅰ幕的构造格局, 但在工区北部的顺北4号、5号等断裂带张扭性断裂活动特征显著; 加里东晚期-海西早期, 部分断裂发生继承性活动且张扭断裂发育范围进一步向南扩大; 印支-燕山期, 仅有少数断裂发生继承性活动; 喜山期该区构造比较稳定, 早期形成的复杂断裂构造进入深埋阶段。

     

  • 图 1  塔中隆起中北部地区构造位置及研究工区分布图

    Figure 1.  Structural location in central and northern parts of Tazhong Uplift and distribution map of the research work area

    图 2  塔中隆起中北部典型断裂构造特征地震剖面图(剖面、断裂带位置及编号见图 1,下同)

    T.三叠系;D3-P.上泥盆统-二叠系;S-D1-2.志留系-中、下泥盆统;O2.上奥陶统;O1-2.中、下奥陶统;∈3.上寒武统;∈2.中寒武统;∈1.下寒武统;∈1-2.中、下寒武统

    Figure 2.  Seismic section of typical fault structures in central and northern parts of Tazhong Uplift

    图 3  塔中隆起中北部地区主要地震反射界面相干切片(a, c, e, g)与断裂体系(b, d, f, h)对比图

    Figure 3.  Comparison maps of coherent slices and faults systems of main surfaces in central and northern part of Tazhong Uplift

    图 4  塔中隆起中北部地区断裂构造剖面组合特征图

    Figure 4.  Combination characteristics of the fault structure section in central and northern part of Tazhong Uplift

    图 5  塔中隆起典型构造演化剖面图(Trace8308测线)

    K.白垩系;T.三叠系;D3-P.上泥盆统-二叠系;S-D1-2.志留系-中、下泥盆统;O3.上奥陶统;O1-2.中、下奥陶统;∈3.上寒武统;∈1-2.中、下寒武统

    Figure 5.  Typical structural evolution profile of Tazhong Uplift

    图 6  塔中隆起中北部地区断裂发育模式图

    F为构造应力; C, E分别为F水平和垂直方向分解力

    Figure 6.  Development models of faults in central and northern parts of Tazhong Uplift

    表  1  塔里木盆地塔中隆起区地层格架(据文献[1]修改)

    Table  1.   Brief of the stratigraphic framework in Tazhong Uplift area, Tarim Basin

    表  2  塔中隆起中北部地区断裂分期活动特征

    Table  2.   Characteristics of the fault stages and activities in central and northern parts of Tazhong Uplift

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  • 收稿日期:  2022-11-28
  • 录用日期:  2023-07-17
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