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    大别山北淮阳带东段石榴斜长角闪岩石炭纪变质作用的测定

    刘贻灿 王辉 杨阳 侯克斌 李洋 宋彪

    刘贻灿, 王辉, 杨阳, 侯克斌, 李洋, 宋彪, 2020. 大别山北淮阳带东段石榴斜长角闪岩石炭纪变质作用的测定. 地球科学, 45(2): 355-366. doi: 10.3799/dqkx.2019.082
    引用本文: 刘贻灿, 王辉, 杨阳, 侯克斌, 李洋, 宋彪, 2020. 大别山北淮阳带东段石榴斜长角闪岩石炭纪变质作用的测定. 地球科学, 45(2): 355-366. doi: 10.3799/dqkx.2019.082
    Liu Yican, Wang Hui, Yang Yang, Hou Ke-Bin, Li Yang, Song Biao, 2020. Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen. Earth Science, 45(2): 355-366. doi: 10.3799/dqkx.2019.082
    Citation: Liu Yican, Wang Hui, Yang Yang, Hou Ke-Bin, Li Yang, Song Biao, 2020. Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen. Earth Science, 45(2): 355-366. doi: 10.3799/dqkx.2019.082

    大别山北淮阳带东段石榴斜长角闪岩石炭纪变质作用的测定

    doi: 10.3799/dqkx.2019.082
    基金项目: 

    国家重点基础研究发展计划("973"计划)项目 2015CB856104

    国家自然科学基金项目 41773020

    详细信息
      作者简介:

      刘贻灿(1962-), 男, 教授, 主要从事变质地球化学与岩石大地构造学研究

    • 中图分类号: P542

    Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen

    • 摘要: 北淮阳带位于大别碰撞造山带北部,相对于南部三叠纪超高压变质带来说,通常被认为是一个相对低级变质的构造岩石单位.以商(城)-麻(城)为界,分为西段和东段.其中,东段未发现与西段相对应的古生代大洋俯冲记录,也缺乏相关的古生代岩浆作用和变质作用方面报道.因而严重地阻碍了对大别造山带形成和演化的深刻理解和准确认识.北淮阳带东段岩石类型丰富,主要包括3类(套)岩石:(1)变质岩,如变质花岗岩(花岗片麻岩)、(石榴)斜长角闪岩、大理岩、云母石英片岩和变质复理石等;(2)岩浆岩,主要为中生代花岗岩、正长岩和火山岩等;(3)盆地沉积岩,主要为中新生代沉积及少量石炭纪沉积.然而,该区一直未发现古生代变质作用的岩石学记录.为此,对北淮阳带东段金寨县铁冲一带与大理岩相共生的石榴斜长角闪岩开展了锆石SHRIMP U-Pb定年和初步的岩石学研究.结果表明,该区石榴斜长角闪岩经历了355±5 Ma变质作用,因而首次发现研究区经历了石炭纪变质作用,为秦岭-桐柏造山带的东延以及大别山碰撞造山带的古生代构造演化过程提供了新的制约.

       

    • 图  1  大别山造山带的地质简图(据Liu et al., 2007修改)

      BZ.北淮阳带;NDZ.北大别杂岩带;CDZ.中大别超高压变质带;SDZ.南大别低温榴辉岩带;SZ.宿松变质带;HMZ.浒湾混杂岩带;HZ.红安低温榴辉岩带;DC.角闪岩相大别杂岩;XMF.晓天-磨子潭断裂;WSF.五河-水吼断裂;HMF.花凉亭-弥陀断裂;TSF.太湖-山龙断裂;TLF.郯庐断裂;SMF.商城-麻城断裂;DWF.大悟断裂

      Fig.  1.  Schematic geological map of the Dabie orogen

      图  2  北淮阳带东段金寨县铁冲地质简图

      Fig.  2.  Schematic geological map of the Tiechong area, Jinzhai in the eastern segment of the Beihuaiyang zone

      图  3  北淮阳带东段金寨县李桥与大理岩相伴生的石榴斜长角闪岩野外照片

      Fig.  3.  A field photograph showing garnet amphibolite coexisting with marble in the eastern segment of the Beihuaiyang zone at Liqiao, Jinzhai

      图  4  北淮阳带东段石榴斜长角闪岩的显微照片

      Grt.石榴子石; Pl.斜长石; Cpx.单斜辉石; Hbl.角闪石; Ttn.榍石; Cc.方解石

      Fig.  4.  Photomicrographs of garnet amphibolite from the eastern Beihuaiyang zone

      图  5  代表性锆石的阴极发光图像

      Fig.  5.  Cathodoluminescene (CL) images of representative zircons

      图  6  锆石U-Pb谐和图

      Fig.  6.  U-Pb concordia diagram of zircon

      表  1  北淮阳带东段石榴斜长角闪岩的锆石SHRIMP U-Pb数据(a)

      Table  1.   SHRIMP zircon U-Pb data for garnet amphibolite from the eastern Beihuaiyang zone

      分析点号 206Pbc (%) U 10-6 Th 10-6 232Th /238U 206Pb* 10-6 207Pb* /206Pb*(±%) 207Pb* /235U(±%) 206Pb* /238U(±%) 206Pb/238U年龄(Ma)
      1705TC9_1.1 4.17 6.3 1.30 0.21 0.31 0.051 6 16.0 0.397 17.0 0.055 9 3.3 350±13
      1705TC9_2.1 7.57 5.3 0.12 0.02 0.27 0.062 0 34.0 0.470 34.0 0.055 2 2.5 347±10
      1705TC9_3.1 8.93 3.6 0.11 0.03 0.19 0.041 0 41.0 0.320 41.0 0.057 2 3.0 359±19
      1705TC9_4.1 4.19 6.3 1.40 0.24 0.32 0.073 5 12.0 0.581 12.0 0.057 3 2.2 359±10
      1705TC9_5.1 8.93 4.7 0.77 0.17 0.25 0.084 0 23.0 0.660 23.0 0.056 6 2.6 355±12
      1705TC9_6.1 2.50 8.9 2.00 0.23 0.45 0.059 6 10.0 0.467 10.0 0.056 9 1.9 356±7
      1705TC9_7.1 3.83 15.0 2.30 0.16 0.77 0.062 3 11.0 0.485 12.0 0.056 4 1.5 354±6
      1705TC9_8.1 2.06 15.0 4.60 0.31 0.76 0.044 9 7.6 0.347 7.8 0.056 1 1.5 352±6
      1705TC9_9.1 9.13 4.2 0.61 0.15 0.22 0.067 0 21.0 0.520 21.0 0.056 3 2.9 353±13
      1705TC9_10.1 4.29 5.8 0.74 0.13 0.30 0.040 3 17.0 0.321 17.0 0.057 7 2.4 362±10
      1705TC9_11.1 5.34 4.2 0.72 0.18 0.22 0.069 0 19.0 0.540 19.0 0.057 0 2.9 358±12
      1705TC9_12.1 3.20 6.0 1.00 0.17 0.30 0.058 0 19.0 0.457 19.0 0.057 0 2.3 357±9
      1705TC9_13.1 2.24 11.0 2.40 0.22 0.55 0.068 5 15.0 0.541 15.0 0.057 3 1.9 359±8
      1705TC9_14.1 7.63 10.0 2.00 0.21 0.53 0.060 0 28.0 0.480 28.0 0.058 2 2.2 365±12
      1705TC9_15.1 10.08 6.0 1.00 0.17 0.32 0.068 0 26.0 0.520 26.0 0.055 2 2.5 346±15
      1705TC9_16.1 24.60 4.5 0.82 0.19 0.29 0.080 0 51.0 0.640 51.0 0.057 7 3.9 361±27
      注:(a)误差为1σ,Pbc和Pb*分别表示普通铅和放射性成因铅;用208Pb进行普通铅扣除.
      下载: 导出CSV
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