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    苏鲁造山带东段新生代两阶段剥露事件的磷灰石(U-Th)/He热年代学证据

    林旭 吴林 MarcJolivet 李长安 刘海金

    林旭, 吴林, MarcJolivet, 李长安, 刘海金, 2022. 苏鲁造山带东段新生代两阶段剥露事件的磷灰石(U-Th)/He热年代学证据. 地球科学, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083
    引用本文: 林旭, 吴林, MarcJolivet, 李长安, 刘海金, 2022. 苏鲁造山带东段新生代两阶段剥露事件的磷灰石(U-Th)/He热年代学证据. 地球科学, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083
    Lin Xu, Wu Lin, Marc Jolivet, Li Chang’an, Liu Haijin, 2022. Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt. Earth Science, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083
    Citation: Lin Xu, Wu Lin, Marc Jolivet, Li Chang’an, Liu Haijin, 2022. Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt. Earth Science, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083

    苏鲁造山带东段新生代两阶段剥露事件的磷灰石(U-Th)/He热年代学证据

    doi: 10.3799/dqkx.2021.083
    基金项目: 

    国家自然科学基金 41972212

    湖南省自然科学基金项目 2019JJ40198

    详细信息
      作者简介:

      林旭(1984-),男,副教授,主要从事造山带隆升和中国大河演化研究.ORCID:0000-0001-7022-6708. E-mail:hanwuji-life@163.com

      通讯作者:

      李长安,E-mail:chanli@cug.edu.cn

    • 中图分类号: P542

    Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt

    • 摘要: 苏鲁造山带位于华北和华南板块之间,是中国东部最显著的陆内造山带之一,约束其新生代剥露过程对于理解中国东部盆山格局分布及其动力学机制具有重要意义.低温热年代学方法由于封闭温度较低,能更准确地约束上地壳地质体的剥露过程.利用磷灰石(U-Th)/He方法,对苏鲁造山带东部的多福山和锯齿山开展研究.磷灰石(U-Th)/He年龄-高程和热历史模拟结果显示,多福山和锯齿山在早-中始新世(54~43 Ma)和渐新世(35~27 Ma)发生剥露.这与苏鲁造山带西段的剥露时间同步.结合区域内已报道的研究结果,表明中国东部造山带受太平洋板块、印度板块向欧亚大陆俯冲的影响,在早新生代出现广泛的阶段性剥露过程,从而奠定了中国东部的盆山分布格局.

       

    • 图  1  苏鲁造山带位置图(a),胶东半岛地质简图(b),地震反射剖面(c)

      图a底图据自然资源部标准地图无修改(审图号:GS(2016)1600号),造山带位置修改自潘桂棠等(2017);图b修改自马丽芳等(2002);图c中AA’代表渤海湾盆地地震反射剖面,据Qi and Yang(2010),BB’代表南黄海盆地地震反射剖面,据Qi and Yang(2010)和Zhu et al.(2020

      Fig.  1.  Location map of Sulu orogenic belt (a), geological map of Jiaodong Peninsula (b); seismic reflection profiles (c)

      图  2  多福山和锯齿山地质图(a)和样品野外采集点照片(b~c)

      图a底图修改自郭敬辉等(2005

      Fig.  2.  Geological map of Duofu and Juchi mountains (a) and photos of sample collection sites in field (b-c)

      图  3  磷灰石He年龄和颗粒半径(Rs) (a)、有效铀浓度(eU) (b) 二维散点图

      Fig.  3.  Scatter diagram of apatite He age, grain radius (Rs) (a) and effective uranium concentration (eU) (b)

      图  4  年龄-海拔关系

      a.多福山剖面;b.锯齿山剖面

      Fig.  4.  Age-elevation relationship

      图  5  多福山(D1~D3)和锯齿山(L1~L5)单颗粒磷灰石(U-Th)/He年龄模拟结果

      Fig.  5.  The modeled thermal histories of samples from Duofu (D1—D3) and Juchi (L1—L5) mountains

      图  6  苏鲁造山带及其邻近区域早新生代构造隆升事件位置分布(a)和时间汇总图(b)

      图a中数字代表研究位置:(1)Wu et al.(2016);(2)Zhao et al.(2018);(3)胡圣标等(2005);(4)Liu et al.(2009);(5)Liu et al.(2009);(6)唐智博等(2011);(7)李理等(2018);(8)许立青等(2016);(9)Liu et al.(2013);(10)Wang et al.(2013);(11)Zhang et al.(2020);(12)Yang et al.(2017);(13)Hu et al.(2006);(14)Cao et al.(2015),Chang et al.(2019),Zhang et al.(2021);(15)Wu et al.(2020);(16)Clinkscaleset al.(2021);(17)吴中海和吴珍汉(2003);(18)Wang et al.(2018);(19)Chang et al.(2018),Xu et al.(2020

      Fig.  6.  Location distribution (a) and time summary map (b) of Early Cenozoic tectonic uplifting events in Sulu orogenic belt and its adjacent areas (the numbers represent research locations)

      图  7  南黄海盆地(a)和渤海湾盆地(b)沉积柱状图(修改自邱燕等, 2016)

      Fig.  7.  Sedimentary columnar map of South Yellow Sea basin (a) and Bohai Bay basin (b) (modified from Qiu et al., 2016)

      图  8  早新生代中国东部盆山分布复原图

      Fig.  8.  Reconstruction map of basin and mountain distribution in eastern China in Early Cenozoic

      表  1  采样位置、高程、岩性数据

      Table  1.   Data of sample location, elevation, and lithologic character

      样品号 海拔(m) 经度 纬度 岩性
      D1 350 36°53′03″ 121°43′12″ 闪长岩
      D2 253 36°52′59″ 121°43′06″ 闪长岩
      D3 126 36°52′51″ 121°43′02″ 闪长岩
      L1 383 36°56′14″ 121°40′09″ 花岗岩
      L2 293 36°55′53″ 121°40′08″ 花岗岩
      L3 179 36°55′47″ 121°39′53″ 花岗岩
      L4 123 36°55′32″ 121°39′40″ 花岗岩
      L5 65 36°55′22″ 121°39′20″ 花岗岩
      下载: 导出CSV

      表  2  多福山和锯齿山垂直剖面磷灰石(U-Th)/He年龄结果

      Table  2.   (U-Th)/He analytical results for samples in the vertical transect in the Duofu and Juchi mountains

      样品号 质量(μg) Rs(μm) U(10-6) Th(10-6) [eU] (10-6) 初始年龄(Ma) ± σ (Ma) FT 校正年龄(Ma) ± σ (Ma)
      D1-A1 8.31 70.1 6.0 1.8 6.4 35.57 1.89 0.805 44.19 3.22
      D1-A2 15.12 84.8 2.2 2.0 2.7 37.76 1.76 0.834 45.28 3.09
      D1-A3 9.40 72.7 9.3 2.0 9.8 39.68 2.12 0.812 48.87 3.58
      平均年龄 45.90 3.80
      D2-A1 3.31 50.3 2.0 1.2 2.3 38.77 1.98 0.730 53.11 3.80
      D2-A2 2.74 48.9 3.8 5.0 5.0 27.78 1.60 0.720 38.58 2.94
      D2-A3 4.02 54.7 3.0 2.0 3.5 34.78 1.82 0.750 46.37 3.36
      D2-A4 4.58 56.2 3.8 2.2 4.3 34.02 1.72 0.756 45.00 3.20
      平均年龄 44.80 3.30
      D3-A2 22.29 97.3 2.4 0.5 2.5 47.07 2.53 0.857 54.92 4.03
      D3-A3 17.89 87.2 10.5 2.5 11.0 36.10 1.92 0.842 42.87 3.13
      D3-A4 15.38 85.8 16.5 1.6 16.9 30.90 1.67 0.840 36.79 2.71
      平均年龄 42.60 3.70
      L1-A1 1.83 41.1 14.2 91.7 35.7 35.84 1.16 0.650 55.14 3.28
      L1-A4 3.49 50.8 13.3 83.1 32.8 46.02 1.49 0.713 64.54 3.84
      L1-A5 1.54 40.0 10.3 60.2 24.5 30.52 1.01 0.645 47.32 2.84
      平均年龄 54.00 3.70
      L2-A1 2.58 46.6 8.0 46.9 19.0 31.00 1.02 0.690 44.93 2.69
      L2-A2 2.54 46.5 12.7 85.2 32.7 36.90 1.19 0.688 53.63 3.19
      L2-A4 4.20 55.6 12.6 80.8 31.6 42.65 1.37 0.736 57.95 3.44
      平均年龄 51.00 3.50
      L3-A1 5.99 61.5 11.6 75.2 29.3 31.17 1.00 0.759 41.07 2.44
      L3-A2 7.54 65.6 10.9 61.1 25.2 35.21 1.15 0.775 45.43 2.71
      L3-A3 4.06 54.5 16.1 91.6 37.7 34.86 1.13 0.732 47.62 2.84
      平均年龄 44.40 3.10
      L4-A1 1.52 38.3 17.1 115.3 44.2 19.76 0.65 0.627 31.52 1.89
      L4-A2 1.31 36.3 18.0 114.6 44.9 24.33 0.79 0.610 39.89 2.38
      平均年龄 34.70 3.00
      L5-A1 9.33 70.6 5.8 2.6 6.4 18.74 0.96 0.805 23.28 1.67
      L5-A2 7.93 70.1 1.4 0.5 1.5 30.44 1.65 0.804 37.86 2.79
      L5-A3 10.86 75.0 9.2 1.2 9.4 19.42 1.05 0.818 23.74 1.75
      L5-A4 16.89 89.7 18.5 2.6 19.1 30.35 1.64 0.847 35.83 2.64
      平均年龄 27.30 2.00
      下载: 导出CSV
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