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东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代:来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

王彦斌 王浩 任留东 焦永艳 仝来喜 WILLIAMSIan S

王彦斌, 王浩, 任留东, 等, 2021. 东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代:来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束. 地质力学学报, 27 (5): 768-782. DOI: 10.12090/j.issn.1006-6616.2021.27.05.063
引用本文: 王彦斌, 王浩, 任留东, 等, 2021. 东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代:来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束. 地质力学学报, 27 (5): 768-782. DOI: 10.12090/j.issn.1006-6616.2021.27.05.063
WANG Yanbin, WANG Hao, REN Liudong, et al., 2021. Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica. Journal of Geomechanics, 27 (5): 768-782. DOI: 10.12090/j.issn.1006-6616.2021.27.05.063
Citation: WANG Yanbin, WANG Hao, REN Liudong, et al., 2021. Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica. Journal of Geomechanics, 27 (5): 768-782. DOI: 10.12090/j.issn.1006-6616.2021.27.05.063

东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代:来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

doi: 10.12090/j.issn.1006-6616.2021.27.05.063
基金项目: 

国家自然科学基金项目 40773042

国家自然科学基金项目 41073014

国家自然科学基金项目 41373052

国家自然科学基金项目 41773049

国家海洋局极地考察办公室对外合作项目 CHINARE-IC201707

详细信息
    作者简介:

    王彦斌(1966-), 男, 博士, 研究员, 从事同位素地质年代学和地球化学研究工作。E-mail: wangyanbin@bjshrimp.cn

  • 中图分类号: P597.3

Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica

Funds: 

the National Natural Science Foundation of China 40773042

the National Natural Science Foundation of China 41073014

the National Natural Science Foundation of China 41373052

the National Natural Science Foundation of China 41773049

the Polar Office of the State Oceanic Bureau of China CHINARE-IC201707

  • 摘要: 东南极Windmill群岛变质杂岩经历的变质和岩浆事件与西澳大利亚Albany-Fraser造山带在时间上相对应,并可能与罗迪尼亚超大陆的拼合有关。Windmill群岛Bailey半岛的镁铁质片麻岩(角闪石-单斜辉石-斜方辉石-黑云母-斜长石-石英-磁铁矿-锆石)被认为具有较早的形成年龄,其中还出露属于正片麻岩的淡色片麻岩(斜长石-钾长石-石英-黑云母-锆石)。对这两种片麻岩中的锆石分别进行了SHRIMP U-Pb年龄测定,首次获得该区镁铁质片麻岩锆石核部207Pb/206Pb加权平均年龄1403±28 Ma,该年龄记录了本区中元古代早期岩浆事件,这是Windmill群岛地区记录的最早一期岩浆事件,可能受到了东部莫森大陆(Mawson Continent)构造岩浆活动的影响。铁镁质片麻岩锆石增生边的年龄为1318±34 Ma,则记录了早期构造热事件。淡色片麻岩中锆石核部年龄为1257±51 Ma,与Bailey半岛的片麻状含石榴子石花岗岩侵位年龄一致,共同记录了该区的一期岩浆活动。淡色片麻岩中锆石增生边的年龄为1197±26 Ma,记录了晚期的变质事件。这些新的年龄数据强烈支持1375~1151 Ma期间东南极Windmill群岛与西澳大利亚Albany-Fraser造山带相连接的构造模型,同时也为罗迪尼亚超大陆拼合过程提供了重要的年代学约束。

     

  • 图  1  Windmill群岛地质简图(据Zhang et al., 2012修改)

    a、b-Windmill群岛在南极的位置;c-Windmill群岛北部地质简图

    Figure  1.  Sketch geological map of the Windmill Islands (modified after Zhang et al., 2012)

    (a and b) Location of the Windmill Islands in Antarctica; (c)Sketch geological map of the northern part of the Windmill Islands

    图  2  Bailey半岛地质简图(据Paul et al., 1995修改)

    Figure  2.  Geological map of the Bailey Peninsula (modified after Paul et al., 1995)

    图  3  Bailey半岛镁铁质片麻岩和淡色片麻岩显微镜下照片

    Hbl-角闪石;Opx-斜方辉石;Cpx-单斜辉石;Bt-黑云母;Pl-斜长石;Qtz-石英;Mag-磁铁矿; Kfs-钾长石
    a-镁铁质片麻岩(C0121-1),单偏光;b-镁铁质片麻岩(C0121-1),正交偏光;c-淡色片麻岩(C0121-2),单偏光;d-淡色片麻岩(C0121-2),正交偏光

    Figure  3.  Micrographs showing petrographic features of the mafic gneiss and leucogneiss in the Bailey Peninsula, Windmill Islands

    (a)Plane-polarized light image of mafic gneiss; (b)Cross-polarized light image of mafic gneiss; (c)Plane-polarized light image of leucogneiss; (d)Cross-polarized light image of leucogneiss
    Hbl-hornblende; Opx-orthopyroxene; Cpx-clinopyroxene; Bt-biotite; Pl-plagioclase; Qtz-quartz; Mag-magnetite; Kfs-K-feldspar

    图  4  Bailey半岛镁铁质片麻岩和淡色片麻岩样品锆石透射光和阴极发光图像

    a-镁铁质片麻岩(C0121-1);b-淡色片麻岩样品(C0121-2)

    Figure  4.  Characteristic images of the analyzed zircons from the mafic gneiss and leucogneiss in the Bailey Peninsula

    (a) The mafic gneiss sample (C0121-1); (b) The leucogneiss sample (C0121-2)

    图  5  Bailey半岛镁铁质片麻岩样品锆石U-Pb谐和图

    Figure  5.  U-Pb concordia diagram of zircons from the mafic gneiss in the Bailey Peninsula

    图  6  Bailey半岛淡色片麻岩样品锆石U-Pb谐和图

    Figure  6.  U-Pb concordia diagram of the zircons from the leucogneiss in the Bailey Peninsula

    图  7  南极洲和澳大利亚的冈瓦纳大陆构造图(据Liu et al., 2018修改)

    AFO-Albany-Fraser造山带;BH-Bunger丘陵;CCr-Curnamona克拉通;M-F-C-Madura-Forrest-Coompana省;MR-Miller Range;NC-Nornalup杂岩; TA-Terre Adélie克拉通; WAC-西澳克拉通;WI-Windmill群岛; WL-威尔克斯地

    Figure  7.  Tectonic map of Antarctica and Australia in a Gondwana configuration(modified after Liu et al., 2018)

    AFO-Albany-Fraser Orogen; BH-Bunger Hills; CCr-Curnamona Craton; M-F-C-Madura-Forrest-Coompana Provinces; MR-Miller Range; NC-Nornalup Complex; TA-Terre Adélie Craton; WAC-West Australian Craton; WI-Windmill Islands; WL-Wilkes Land

    表  1  Bailey半岛镁铁质片麻岩和淡色片麻岩中锆石SHRIMP U-Pb同位素数据

    Table  1.   SHRIMP U-Pb isotopic analytical data of the mafic gneiss and leucogneiss from the Bailey Peninsula, Windmill Islands

    点号 206Pbc/% 含量/×10-6 232Th/238U 年龄/Ma 同位素比值
    U Th 206Pb* 207Pb/206Pb ±1σ 206Pb/238U ±1σ 不和谐度 207Pb*/206Pb* ±/% 207Pb*/235U ±/% 206Pb*/238U ±/% 误差
    C0121-1镁铁质片麻岩
    1.1c 0.07 117 60 25.7 0.53 1406 35 1462 12 -4 0.0891 1.8 3.126 2.0 0.2545 0.91 0.4
    2.1r 0.07 218 7 43.7 0.03 1322 27 1352 8 -2 0.0853 1.4 2.745 1.5 0.2334 0.7 0.4
    3.1c 2.5 26 11 6.02 0.42 1224 200 1490 28 -22 0.0811 10.0 2.91 11.0 0.2601 2.1 0.2
    4.1c 0.15 79 42 17.1 0.54 1439 44 1441 15 0 0.0906 2.3 3.13 2.6 0.2505 1.1 0.4
    5.1r 0.04 1910 0 362 0.00 1328 9.1 1284 3 3 0.08556 0.47 2.599 0.55 0.22032 0.29 0.5
    5.2r 1.35 127 1 27 0.01 1392 71 1406 12 -1 0.0884 3.7 2.97 3.8 0.2437 0.99 0.3
    6.1c 0.29 118 47 24.8 0.41 1359 42 1406 12 -3 0.0869 2.2 2.922 2.4 0.2438 0.97 0.4
    7.1c 0.27 92 30 20.1 0.34 1399 48 1458 14 -4 0.0888 2.5 3.107 2.7 0.2539 1.1 0.4
    8.1c 0.0 70 38 15.8 0.56 1451 43 1497 23 -3 0.0912 2.3 3.288 2.9 0.2614 1.8 0.6
    9.1c 0.1 108 39 23 0.37 1361 39 1431 13 -5 0.087 2.0 2.982 2.3 0.2486 1.0 0.5
    10.1c 0.92 66 23 14.9 0.36 1500 77 1503 20 0 0.0936 4.1 3.39 4.3 0.2626 1.5 0.3
    10.2r 0.08 200 5 40.9 0.03 1321 47 1375 10 -4 0.0853 2.4 2.795 2.6 0.2378 0.77 0.3
    11.1c 0.34 80 24 17.3 0.31 1433 67 1440 15 0 0.0904 3.5 3.12 3.7 0.2503 1.2 0.3
    12.1c 0.57 39 11 8.74 0.28 1389 69 1473 22 -6 0.0883 3.6 3.13 3.9 0.2567 1.7 0.4
    13.1r 0.0 202 5 41.8 0.02 1324 27 1389 9 -5 0.0854 1.4 2.832 1.6 0.2405 0.73 0.5
    14.1r 0.0 388 25 70.9 0.07 1205 22 1242 6 -3 0.08032 1.1 2.353 1.2 0.2125 0.55 0.4
    15.1c 1.19 54 25 11.6 0.48 1343 130 1423 20 -6 0.0862 6.7 2.94 6.9 0.247 1.5 0.2
    16.1c 0.29 108 32 22 0.31 1387 39 1374 18 1 0.0882 2.0 2.888 2.5 0.2375 1.5 0.6
    17.1r 0.0 387 22 68.9 0.06 1239 22 1215 6 2 0.08173 1.1 2.338 1.3 0.2074 0.56 0.4
    C0121-2淡色片麻岩
    1.1r 0.02 1698 33 314 0.02 1196 11 1256 15 -5 0.07996 0.54 2.373 1.4 0.2152 1.3 0.9
    2.1c 0.2 92 170 17.1 1.91 1191 50 1264 19 -6 0.0798 2.6 2.382 3.1 0.2166 1.7 0.6
    3.1c 0.48 55 112 10.8 2.09 1335 62 1315 23 2 0.0859 3.2 2.68 3.7 0.2262 2.0 0.5
    4.1r 0.02 2484 127 418 0.05 1229 11 1152 13 6 0.08132 0.56 2.195 1.4 0.1957 1.3 0.9
    5.1c 0.82 106 125 18.2 1.22 1292 80 1166 19 10 0.084 4.1 2.29 4.5 0.1982 1.8 0.4
    6.1r 0.04 3400 194 577 0.06 1247 10 1161 14 7 0.08207 0.53 2.233 1.4 0.1973 1.3 0.9
    7.1c 0.69 153 411 26.7 2.78 1395 78 1186 18 15 0.0886 4.1 2.47 4.4 0.2021 1.7 0.4
    8.1r 0.02 3436 233 576 0.07 1181 11 1149 13 3 0.07936 0.54 2.135 1.4 0.1951 1.3 0.9
    9.1c 0.34 129 217 22.6 1.73 1240 45 1189 18 4 0.0818 2.3 2.285 2.8 0.2026 1.6 0.6
    10.1c 0.28 150 183 26.7 1.26 1229 51 1213 27 1 0.0813 2.6 2.321 3.6 0.207 2.5 0.7
    11.1r 0.09 2648 110 455 0.04 1277 11 1173 14 8 0.08331 0.56 2.293 1.4 0.1996 1.3 0.9
    12.1c 0.51 506 305 87.7 0.62 1226 34 1179 15 4 0.0812 1.7 2.246 2.2 0.2006 1.4 0.6
    13.1c 1.33 328 288 61.1 0.9 1337 59 1248 17 7 0.0859 3.1 2.53 3.4 0.2135 1.5 0.4
    13.2r 0.08 2336 76 384 0.03 1180 14 1127 13 5 0.07932 0.7 2.089 1.5 0.191 1.3 0.9
    14.1r 0.35 2191 73 366 0.03 1192 16 1142 14 4 0.07979 0.81 2.133 1.5 0.1939 1.3 0.8
    注:误差为1s;Pbc和Pb*分别表示普通铅和放射成因铅;标准校正值的误差为1.03%;普通铅校正应用204Pb实测值;c: 锆石核(core);r: 锆石增生边(rim)
    下载: 导出CSV

    表  2  东南极Windmill群岛地质演化的锆石和独居石U-Pb年龄和石榴子石-全岩Sm-Nd同位素年龄记录

    Table  2.   Summary of litho-tectonic and metamorphic evolution as determined by U-Pb SHRIMP zircon and monazite analyses and Grt-WR Sm-Nd data

    地质事件 样品地点及形式 年龄/Ma 分析方法 参考文献
    Balaena岛辉长岩侵位 519 斜长石K-Ar Webb et al., 1963
    晚期粗玄岩墙侵位
    细晶岩墙侵位 Robinson脊 1138±9 锆石SHRIMP U-Pb Post,2000
    变形作用(D4) 北东-南西向左旋剪切和脆性断裂
    橄榄石辉长岩墙侵位
    变形作用(D3) 早期构造单元的南北向褶皱
    变形作用(D2) 紧闭到等斜F2褶皱
    Ardery紫苏花岗岩侵位 Bosner岛 1163±7 锆石SHRIMP U-Pb Post,2000
    Robinson脊 1178±7, 1178±6 锆石LA-ICPMS U-Pb Morrissey et al., 2017b
    Robinson脊 1196±8, 1205±13 锆石LA-ICPMS U-Pb Zhang et al., 2012
    Ford岛花岗岩侵位 Ford岛 1173±9 锆石SHRIMP U-Pb Post,2000
    黑云母花岗岩侵入变沉积岩 Mitchell半岛 1235±7 锆石LA-ICPMS U-Pb Morrissey et al., 2017b
    麻粒岩相和部分熔融和变形作用(M2/D2) Mitchell半岛混合岩淡色体 1137±3 Sm-Nd(Grt-WR) Post, 2000
    Herring岛麻粒岩变质事件 1142±7 独居石SHRIMP U-Pb Post, 2000
    Bailey半岛正片麻岩 1156±17 Sm-Nd(Grt-WR) Post, 2000
    Clark半岛正片麻岩 1169±7 独居石HRIMP U-Pb Post, 2000
    Herring岛麻粒岩锆石变质增长边 1171±9 锆石SHRIMP U-Pb Post, 2000
    Bailey半岛含正片麻岩 1171±13 独居石SHRIMP U-Pb Post, 2000
    Clark半岛石榴黑云片麻岩淡色体 1171±6 独居石SHRIMP U-Pb Post, 2000
    Cameron岛、Herring岛、Mitchell半岛和Robinson脊变沉积岩锆石变质边 ca.1325~1170 锆石LA-ICPMS U-Pb Morrissey et al., 2017b
    Mitchell半岛、Herring岛变泥质岩 1177±4, 1200~1170,1185±8 独居石LA-ICPMS U-Pb Morrissey et al., 2007a
    Bailey半岛正片麻岩同变质至变形后D2a锆石变质增生 1214±10 锆石SHRIMP U-Pb Post, 2000
    Bailey半岛淡色片麻岩锆石变质增生边 1197±26 锆石SHRIMP U-Pb 文中
    麻粒岩相重结晶 ca.1210~1180 锆石和独居石SHRIMP U-Pb,Sm-Nd(Grt-WR) Post et al., 1997
    花岗质岩石的侵位 Bailey含石榴子石花岗片麻岩侵位和片麻状含石榴子石花岗岩 1242±13, 1247±13, 1258±12 锆石LA-ICPMS U-Pb Zhang et al., 2012
    Bailey半岛淡色片麻岩原岩侵位 1257±51 锆石SHRIMP U-Pb 文中
    Clark半岛正片麻岩 1315±6 锆石SHRIMP U-Pb Post, 2000
    Clark半岛正片麻岩 1323±7 锆石LA-ICPMS U-Pb Morrissey et al., 2017b
    高角闪岩-麻粒岩相变质作用和变形作用(M1/D1) 角闪岩相重结晶 ca.1400~1300 锆石SHRIMP U-Pb Post et al., 1997
    Mitchell半岛变泥质岩 1305±7 独居石LA-ICPMS U-Pb Morrissey et al., 2007a
    Bailey半岛镁铁质片麻岩变质 1318±34 锆石SHRIMP U-Pb 文中
    Clark半岛石榴黑云片麻岩淡色体 1342±21 锆石SHRIMP U-Pb Post, 2000
    变沉积岩原岩沉积时代 Cameron岛、Herring岛、Mitchell半岛和Robinson脊变沉积岩 ca.1350~1315 锆石LA-ICPMS U-Pb Morrissey et al., 2017b
    Herring岛石榴堇青黑云片麻岩 ca.1400~1350 锆石SHRIMP U-Pb Post, 2000
    Chappel岛 1450±80 锆石SHRIMP U-Pb Williams et al., 1983
    ca.2500~1700 锆石SHRIMP U-Pb Post et al., 1997
    花岗岩的侵位 Bailey半岛石榴花岗片麻岩、片麻状石榴花岗岩(继承锆石) 1372±13 锆石LA-ICPMS U-Pb Zhang et al., 2012
    镁铁质岩石的侵位 Bailey半岛 1403±28 锆石SHRIMP U-Pb 文中
    下载: 导出CSV
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  • 收稿日期:  2021-06-28
  • 修回日期:  2021-08-23
  • 预出版日期:  2021-12-31
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