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    库车盆地中新生代构造演化: 磷灰石裂变径迹证据

    罗梦 朱文斌 郑碧海 朱晓青

    罗梦, 朱文斌, 郑碧海, 朱晓青, 2012. 库车盆地中新生代构造演化: 磷灰石裂变径迹证据. 地球科学, 37(5): 893-902. doi: 10.3799/dqkx.2012.098
    引用本文: 罗梦, 朱文斌, 郑碧海, 朱晓青, 2012. 库车盆地中新生代构造演化: 磷灰石裂变径迹证据. 地球科学, 37(5): 893-902. doi: 10.3799/dqkx.2012.098
    LUO Meng, ZHU Wen-bin, ZHENG Bi-hai, ZHU Xiao-qing, 2012. Mesozoic-Cenozoic Tectonic Evolution of the Kuqa Basin: Evidence from Apatite Fission-Track Data. Earth Science, 37(5): 893-902. doi: 10.3799/dqkx.2012.098
    Citation: LUO Meng, ZHU Wen-bin, ZHENG Bi-hai, ZHU Xiao-qing, 2012. Mesozoic-Cenozoic Tectonic Evolution of the Kuqa Basin: Evidence from Apatite Fission-Track Data. Earth Science, 37(5): 893-902. doi: 10.3799/dqkx.2012.098

    库车盆地中新生代构造演化: 磷灰石裂变径迹证据

    doi: 10.3799/dqkx.2012.098
    基金项目: 

    国家自然科学基金项目 40972133

    国家科技重大专项 2011zx05035-005-001hz

    详细信息
      作者简介:

      罗梦(1987-), 女, 硕士在读, 从事低温热年代学研究.E-mail: luomeng_08@126.com

    • 中图分类号: P546

    Mesozoic-Cenozoic Tectonic Evolution of the Kuqa Basin: Evidence from Apatite Fission-Track Data

    • 摘要: 通过对库车河剖面14个样品磷灰石裂变径迹的测试, 研究了库车盆地及其源区的构造演化.根据表观年龄和地层年龄关系, 将结果分成8个退火样品和6个碎屑样品.退火样品年龄从北向南从136~93.7 Ma, 记录了构造发育自造山带向盆地扩展的运动样式.其中09dk-6, 09dk-7, 09dk-8和09dk-11未通过X2检验, 分析认为与后期构造活动有关, 分解得到最年轻的年龄组记录了库如力向斜, 捷斯德里克背斜和阿合断层分别在74.4 Ma、24.2 Ma和50.8 Ma的最新一期活动.碎屑磷灰石得到了250 Ma、160 Ma和100 Ma3个明显的静态峰.结合热模拟研究表明, 研究区存在250 Ma、160 Ma、100 Ma和20 Ma四期构造隆升, 是对亚洲南缘多期地体碰撞增生的响应.

       

    • 图  1  库车再生前陆盆地前陆变形带构造单元(据卢华复等,1999修改)

      构造带:Ⅰ.北部单斜带;Ⅱ.斯的克背斜带;Ⅲ.克-依构造带;Ⅳ.拜城-阳霞凹陷带;Ⅴ.秋里塔格构造带

      Fig.  1.  Structures in the deformation belt of the Kuqa rejuvenation foreland basin

      图  2  库车河地质构造略图(a)和A-A'剖面图(b)

      Q1x.西域组;(N2-Q1)k.库车组;N2k.库车组;N1k.康村组;N1j.吉迪克组;E2-3s.苏维依组;E1-2km.库姆格列木组;K1bs.巴什基奇克组;K1b.巴西盖组;K1s.舒善河组;K1y.亚格列木组;J2q.恰克马克组;J2k.克孜勒努尔组;J1y.阳霞组;J1a.阿合组;T3t.塔里奇克组;T3h.黄山街组;T2kl.塔里奇克组;T1e.俄霍布拉克组;P1x.小铁里干克群;P3by.比尤勒包谷孜组;09dk-1~ 09dk-27示采样位置

      Fig.  2.  Geological map of the Kuqa River area (a) and A-A' cross-section (b)

      图  3  样品的单颗粒年龄雷达图(a)和径迹长度分布(b)

      a图左侧纵坐标为标准差,右侧纵坐标为年龄(Ma)

      Fig.  3.  Single-grain age distribution (a) and track length histograms (b)

      图  4  样品09dk-6(a)、09dk-8(b)和09dk-11(c)的Dpar值分布

      Fig.  4.  Dpar values of samples 09dk-6 (a), 09dk-8 (b) and 09dk-11 (c)

      图  5  碎屑磷灰石样品年龄峰

      Fig.  5.  Peaks of the detrital apatite samples

      图  6  样品09dk-1、09dk-2、09dk-6、09dk-8和09dk-11的热史模拟

      浅灰色区代表“可以接受的”热史拟合曲线集; 深灰色区为“高质量的”热史曲线集; 黑色曲线代表“最佳”热史拟合曲线(Ketcham, 2005)

      Fig.  6.  Thermal modelling history of samples 09dk-1, 09dk-2, 09dk-6, 09dk-8 and 09dk-11

      表  1  库车河剖面样品裂变径迹数据

      Table  1.   Apatite fission track data of the Kuqa River section

      样号 层位 N ρs
      (105 cm-2)
      Ns ρi
      (105 cm-2)
      Ni ρd
      (105 cm-2)
      Nd P(X2)(%) t(Ma) Nt L(μm)
      A 09dk-1 γ4 29 8.91 1 647 14.20 1 647 11.5 2 862 74.92 126.2±4.7 11 10.873±1.58
      09dk-2 P1x 27 10.02 1 213 16.37 1 982 11.4 2 840 17.59 128.1±7.6 46 10.789±1.78
      09dk-6 T3t 30 8.23 1 049 13.42 1 711 11.3 2 818 0.00 121.5±8.3 17 11.35±2.049
      09dk-7 T3h 31 4.42 925 18.00 3 770 11.2 2 796 0.00 49.7±3.1
      09dk-8 J1a 30 6.42 738 14.06 1 615 11.1 2 774 0.00 92.0±6.8 11 12.036±1.58
      09dk-11 J1y 30 5.79 762 17.63 2 320 11.0 2 753 0.06 62.7±4.2 8 11.21±1.84
      09dk-12 J2q 11 5.80 342 11.59 684 10.9 2 731 56.62 109.1±11.7
      09dk-27 K1b 9 5.39 216 13.39 537 12.3 3 065 5.58 88.8±10.1
      B 09dk-14 K1y 30 11.51 1 664 13.47 1 947 12.7 3 187 0.01 196.3±11.3
      09dk-15 Q1x 32 6.67 1 228 29.25 5 384 12.7 3 170 0.00 51.8±3.9
      09dk-21 N1k 30 7.39 1 252 15.65 2 650 12.5 3 135 0.61 104.3±5.2
      09dk-22 Q1x 30 7.39 836 16.79 1 899 12.5 3 117 0.00 102.0±7.8
      09dk-23 E2-3s 30 8.35 1 123 11.84 1 593 12.4 3 100 3.32 154.5±8.4
      09dk-25 E2-3s 30 16.86 2 045 26.29 3 189 12.3 3 082 0.00 140.9±8.5
      注:N=样品颗粒数;Nd=铀标准玻璃对应外探测器的诱发径迹条数;Ns=自发径迹条数;Ni =诱发径迹条数;P(X2)为卡方检测的结果;Nt=所测量的围限径迹长度数;ρs.自发径迹密度;ρi.诱发径迹密度;ρd.铀标准玻璃的诱发径迹密度;L=所测量的围限径迹长度.
      下载: 导出CSV

      表  2  砂岩屑样品二项式拟合年龄峰值统计结果

      Table  2.   Binomial analysis results of detrital samples

      样品 层位 颗粒数 P(F) 最佳拟合峰(Ma)及所占比例
      P0 P1 P2
      09dk-15 Q1x 32 0.01 35.3(46.6%) 58.4(33.3%) 86.1(20.4%)
      09dk-22 Q1x 30 0.02 71.8(30.7%) 107.9(65.9%) 445.2(3.4%)
      09dk-21 N1k 30 0.00 101.2(95.8%) 250.1(0.34%)
      09dk-25 E2-3s 30 0.02 111.7(46.5%) 163.9(47.0%) 256(6.6%)
      09dk-23 E2-3s 30 0.00 145.5(88.8%) 234.7(11.2%)
      09dk-14 K1y 30 0.02 152.5(32.1%) 216.4(64.6%) 785(3.3%)
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2012-05-19
    • 网络出版日期:  2021-11-10
    • 刊出日期:  2012-09-15

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