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    北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义

    舒坦 续海金 章军锋 刘强

    舒坦, 续海金, 章军锋, 刘强, 2019. 北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义. 地球科学, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119
    引用本文: 舒坦, 续海金, 章军锋, 刘强, 2019. 北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义. 地球科学, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119
    Shu Tan, Xu Haijin, Zhang Junfeng, Liu Qiang, 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119
    Citation: Shu Tan, Xu Haijin, Zhang Junfeng, Liu Qiang, 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119

    北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义

    doi: 10.3799/dqkx.2018.119
    基金项目: 

    国家自然科学基金项目 41772054

    国家自然科学基金项目 41572039

    详细信息
      作者简介:

      舒坦(1991-), 男, 在读博士研究生, 主要从事构造地质学研究

      通讯作者:

      续海金

    • 中图分类号: P54

    Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton

    • 摘要: 北京西山地区广泛发育轴向近E-W向的褶皱,对理解华北克拉通东部构造演化至关重要,但目前对其形成时代和构造动力学背景却没有明确的认识.北京房山地区的太平山褶皱是轴向近E-W向褶皱的典型代表.通过精细的野外构造观察和构造年代学研究,确定太平山褶皱的空间展布特征和构造样式,厘定构造变形的时代,为该区乃至华北克拉通东部的构造演化提供重要依据.通过详细的野外构造观察和系统的β图解研究,表明太平山褶皱由直立倾伏背斜和斜歪倾伏向斜构成.通过对早期卷入褶皱变形的煌斑岩席和晚期切层侵入褶皱的闪长玢岩脉进行锆石U-Pb定年,得到煌斑岩席和闪长玢岩脉的形成时代分别为147.2±2.4 Ma和129.0±3.2 Ma,表明太平山褶皱的形成时代为燕山运动B幕.另外,北京西山地区还存在NW-SE向的伸展构造样式.代表本区NW-SE向伸展的房山穹窿(约136 Ma)晚于N-S向挤压构造,侵入切割太平山褶皱,塑造了研究区现今主体构造格架,进一步限定太平山褶皱的形成时代为147~136 Ma.因此,研究区轴向近E-W向的褶皱为早白垩世近N-S向挤压构造的产物;N-S向挤压和NW-SE向伸展的构造样式,为华北克拉通中生代构造体制的转换和动力学背景提供关键依据.

       

    • 图  1  华北克拉通地质简图(a)和北京西山南部区域地质构造略图(b)

      图a据Wang et al.(2010)修改; 图b据赵温霞(2003)修改.1.第四系; 2.白垩系; 3.侏罗系; 4.三叠系至石炭系; 5.寒武系-奥陶系; 6.新元古界青白口系; 7.中元古界蓟县系; 8.中元古界长城系; 9.太古宇官地杂岩; 10.房山花岗闪长岩体; 11.背斜轴迹; 12.向斜轴迹; 13.拆离断层; 14.逆断层产状(°); 15.正断层产状(°); 16.地质界线; 17.平行不整合及角度不整合; 18.面理产状(°); 19.城镇及居民点; 20.剖面线

      Fig.  1.  Geological sketch map of North China craton (a) and regional structural and geological sketch map of the southern part of the Western Hills of Beijing (b)

      图  2  房山地区太平山-官地地层实测剖面

      剖面A-A’见图 1b

      Fig.  2.  Measured stratigraphic section from Taipingshan to Guandi in the Fangshan area

      图  3  太平山褶皱的出露特征

      a.太平山褶皱三维示意; b.164背斜的β图解; c.太平山向斜的β图解; d.164背斜平行于轴面剖面; e.164背斜直立剖面

      Fig.  3.  Exposed features of Taipingshan fold

      图  4  闪长玢岩脉侵入至马家沟组灰岩(a)和风化的闪长玢岩(b)

      Fig.  4.  The dioritic porphyrite dyke intruded into limestone of Majiagou Formation (O2m) (a) and weathered dioritic porphyrite (b)

      图  5  164背斜布丁状煌斑岩脉显微照片

      a.煌斑结构, 斑晶主要为黑云母和斜长石; b.煌斑岩侵入时捕获围岩灰岩

      Fig.  5.  Photomicrographs of the pudding lamprophyre dyke in the 164-anticline

      图  6  煌斑岩(a)和闪长玢岩(b)锆石阴极发光图像及LA-ICP-MS测年分析点位

      Fig.  6.  Representative cathodoluminescence (CL) images of zircon grains with 206Pb/238U age (Ma) from 164-anticline lamprophyre (a) and diorite porphyrite (b) from Daliyanshan

      图  7  煌斑岩(a)和闪长玢岩(b)LA-ICP-MS锆石U-Pb年龄谐和图

      Fig.  7.  Zircon U-Pb concordia diagrams for lamprophyre (a) and diorite porphyrite (b)

      图  8  黄院村采石场-小东沟地层信手剖面

      剖面B-B’见图 1b

      Fig.  8.  Draft stratigraphic section of Huangyuan quarry-Xiaodonggou

      图  9  太平山褶皱的形成和演化

      a.地层沉积阶段;b.大约147 Ma,煌斑岩呈席状侵入至马家沟组灰岩中;c.147~136 Ma,近N-S的挤压形成E-W向太平山褶皱;d.大约136 Ma,房山岩体底侵形成穹窿构造并造成太平山向斜北翼陡倾、地层缺失减薄,此后在129 Ma,闪长玢岩脉形成并切层侵入至马家沟组灰岩中

      Fig.  9.  The formation and evolution of Taipingshan fold

      表  1  房山地区太平山煌斑岩和闪长玢岩LA-ICP-MS锆石U-Pb测年分析结果

      Table  1.   LA-ICP-MS zircon U-Pb isotope data for lamprophyre and diorite porphyrite from Taipingshan, Fangshan area

      点号 Pb(10-6) Th(10-6) U(10-6) Th/U 同位素比值 年龄(Ma)
      207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ
      煌斑岩(ZKD12-1),n=7
      1.1 92 904 1 584 0.570 0.047 7 0.002 5 0.149 8 0.008 0 0.022 6 0.000 3 83.4 127.8 142 7.0 144 2.0
      2.1 222 2 740 1 439 1.900 0.049 0 0.002 5 0.154 7 0.007 9 0.022 8 0.000 3 150.0 116.0 146 7.0 146 2.0
      3.1 14 448 447 1.000 0.055 2 0.003 4 0.172 9 0.010 2 0.022 9 0.000 3 420.0 137.0 162 8.9 146 2.1
      4.1 8 277 244 1.130 0.055 1 0.003 5 0.175 5 0.010 8 0.023 1 0.000 5 417.0 144.0 164 9.3 147 2.9
      5.1 31 895 1 008 0.890 0.057 1 0.002 6 0.184 3 0.008 0 0.023 2 0.000 3 494.0 100.0 172 6.9 148 1.8
      6.1 21 693 653 1.060 0.046 2 0.002 3 0.149 9 0.007 2 0.023 5 0.000 3 5.7 115.0 142 6.4 150 2.1
      7.1 12 547 302 1.810 0.054 1 0.003 3 0.177 3 0.010 6 0.023 9 0.000 4 376.0 137.0 166 9.1 152 2.4
      闪长玢岩(15ZKD-DLYS),n=9
      1.1 51.2 432.1 456.9 0.946 0.050 512 0.003 983 0.147 009 0.011 528 0.021 042 0.000 342 220.4 178.7 139.3 10.2 134.2 2.2
      2.1 88.3 800.3 545.0 1.469 0.054 716 0.003 914 0.162 340 0.011 425 0.021 547 0.000 317 466.7 161.1 152.7 10.0 137.4 2.0
      3.1 379.0 3 635.6 1 961.1 1.854 0.048 056 0.001 801 0.129 463 0.004 815 0.019 552 0.000 190 101.9 88.9 123.6 4.3 124.8 1.2
      4.1 66.3 604.3 461.0 1.311 0.061 834 0.004 928 0.159 428 0.010 747 0.019 808 0.000 367 733.3 172.2 150.2 9.4 126.4 2.3
      5.1 120.7 1 129.2 729.3 1.548 0.054 523 0.003 317 0.147 510 0.008 710 0.019 927 0.000 364 394.5 137.0 139.7 7.7 127.2 2.3
      6.1 36.2 314.8 358.8 0.877 0.052 998 0.004 461 0.152 499 0.013 333 0.020 763 0.000 346 327.8 192.6 144.1 11.7 132.5 2.2
      8.1 151.3 1 351.9 888.2 1.522 0.053 070 0.003 437 0.149 219 0.009 312 0.020 564 0.000 267 331.5 148.1 141.2 8.2 131.2 1.7
      9.1 466.9 4 612.8 1 998.7 2.308 0.049 243 0.002 286 0.138 045 0.006 256 0.020 281 0.000 204 166.8 104.6 131.3 5.6 129.4 1.3
      10.1 145.0 1 441.7 969.2 1.487 0.047 417 0.002 297 0.129 167 0.006 175 0.019 675 0.000 250 77.9 111.1 123.3 5.6 125.6 1.6
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