滇西昌宁-孟连带南段组碎屑锆石U-Pb年龄及其对沉积时代和构造环境的制约

黄晓明, 牟传龙, 罗亮, 丛峰, 董会. 2023. 滇西昌宁-孟连带南段组碎屑锆石U-Pb年龄及其对沉积时代和构造环境的制约. 地质通报, 42(7): 1069-1081. doi: 10.12097/j.issn.1671-2552.2023.07.002
引用本文: 黄晓明, 牟传龙, 罗亮, 丛峰, 董会. 2023. 滇西昌宁-孟连带南段组碎屑锆石U-Pb年龄及其对沉积时代和构造环境的制约. 地质通报, 42(7): 1069-1081. doi: 10.12097/j.issn.1671-2552.2023.07.002
HUANG Xiaoming, MOU Chuanlong, LUO Liang, CONG Feng, DONG Hui. 2023. U-Pb geochronology of the detrital zircons from the southern segment of the Changning-Menglian suture zone in western Yunnan: Constraints on sedimentary age and tectonic environment. Geological Bulletin of China, 42(7): 1069-1081. doi: 10.12097/j.issn.1671-2552.2023.07.002
Citation: HUANG Xiaoming, MOU Chuanlong, LUO Liang, CONG Feng, DONG Hui. 2023. U-Pb geochronology of the detrital zircons from the southern segment of the Changning-Menglian suture zone in western Yunnan: Constraints on sedimentary age and tectonic environment. Geological Bulletin of China, 42(7): 1069-1081. doi: 10.12097/j.issn.1671-2552.2023.07.002

滇西昌宁-孟连带南段组碎屑锆石U-Pb年龄及其对沉积时代和构造环境的制约

  • 基金项目:
    中国地质调查局项目《云南省1:5万岩帅、大芒岭、上允3幅区域地质调查》(编号: DD20221635, DD20190053)、《四川盆地地质结构与深层油气综合调查》(编号: DD20211210)
详细信息
    作者简介: 黄晓明(1990-), 男, 硕士, 地质学专业。E-mail: 623078672@qq.com
    通讯作者: 牟传龙(1965-), 男, 博士生导师, 从事沉积地质与油气地质研究。E-mail: cdmchuanlong@163.com
  • 中图分类号: P54;P597+.3

U-Pb geochronology of the detrital zircons from the southern segment of the Changning-Menglian suture zone in western Yunnan: Constraints on sedimentary age and tectonic environment

More Information
  • 为制约滇西昌宁-孟连带南段组的沉积时代和构造环境, 阐明临沧地块演化特征, 对南段组碎屑锆石进行U-Pb年代学研究。研究显示, 南段组具统计意义的最年轻组碎屑锆石年龄为512 Ma、509.6 Ma, 物源具泛非期(680~530 Ma)、晚格林威尔期(980~900 Ma)、早格林威尔期(1300~1100 Ma)3期年龄组段特点。结果表明, 南段组中下部最大沉积下限为寒武纪, 中上部上限为石炭纪。物源来自东冈瓦纳超大陆内部至少3条造山带, 主要为南极Pinjarra造山带、西澳Albany-Fraser造山带、东澳Paterson-Peterman造山带, 具亲冈瓦纳大陆性质。在古生代冈瓦纳大陆重建中, 南段组古地理位置位于澳大利亚地块北缘, 是一个从西澳大利亚地块往东澳大利亚地块, 往北往东迁移, 从被动大陆边缘到活动大陆边缘转换的演化过程。早期沉积环境为滨浅海或三角洲, 后期为弧前增生楔沉积环境。

  • 加载中
  • 图 1  研究区区域构造略图(a、b,据张开均等,2009潘桂棠等,2016Zhang et al., 2012) 及南段组地质简图(c)

    Figure 1. 

    图 2  临沧地块岩性柱状图

    Figure 2. 

    图 3  岩帅镇南段组实测剖面

    Figure 3. 

    图 4  南段组野外(a、b)及镜下(c、d)照片

    Figure 4. 

    图 5  南段组碎屑锆石阴极发光图像

    Figure 5. 

    图 6  南段组锆石类型判别图解(a、b)、构造背景图解(c、d)和稀土元素配分曲线图(e、f) (据Grimes et al., 2007Yang et al., 2012)

    Figure 6. 

    图 7  南段组碎屑锆石U-Pb年龄谐和图(a、c)和相对频率分布图(b、d)

    Figure 7. 

    图 8  南段组与其他相关碎屑锆石U-Pb年龄频谱对比图(据赵林涛等,2019周美玲等,2020)

    Figure 8. 

    图 9  南段组古地理位置和演化图(据聂小妹,2016修改)

    Figure 9. 

    表 1  南段组碎屑锆石U-Th-Pb定年结果

    Table 1.  U-Th-Pb dating results of detrital zircon from Nanduan Formation

    测点号 Th/U 同位素比值 年龄/Ma 谐和度
    207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U
    PM103-3-1变质岩屑石英砂岩
    1 0.51 0.0593 0.0011 0.7654 0.0155 0.0931 0.0007 588.9 10.2 577.1 8.9 573.9 4.1 99%
    2 2.78 0.0813 0.0031 2.2170 0.0852 0.1978 0.0022 1227.8 74.1 1186.4 26.9 1163.6 12.0 98%
    3 1.52 0.0779 0.0016 2.0876 0.0442 0.1940 0.0015 1146.3 42.1 1144.7 14.6 1143.1 8.2 99%
    4 0.89 0.0753 0.0012 1.7343 0.0263 0.1668 0.0010 1075.9 25.5 1021.4 9.8 994.6 5.6 97%
    5 1.96 0.0626 0.0022 0.8139 0.0288 0.0945 0.0008 694.5 75.9 604.6 16.1 582.2 4.8 96%
    6 0.69 0.0782 0.0012 2.1211 0.0330 0.1964 0.0013 1153.7 30.7 1155.7 10.8 1156.0 6.8 99%
    7 0.78 0.1961 0.0026 14.5988 0.1973 0.5394 0.0035 2794.1 21.9 2789.5 13.0 2781.0 14.6 99%
    8 0.19 0.0596 0.0022 0.7029 0.0257 0.0856 0.0009 588.6 80.4 540.5 15.3 529.4 5.2 97%
    9 0.86 0.0903 0.0019 3.0534 0.0649 0.2452 0.0021 1431.5 39.5 1421.1 16.3 1413.8 10.8 99%
    10 0.31 0.0573 0.0016 0.7483 0.0199 0.0949 0.0008 501.9 59.3 567.2 11.6 584.4 4.6 97%
    11 0.88 0.0783 0.0013 2.1530 0.0377 0.1991 0.0012 1153.7 33.3 1166.0 12.2 1170.5 6.6 99%
    12 1.64 0.0591 0.0016 0.6858 0.0186 0.0841 0.0007 568.6 52.8 530.3 11.2 520.3 4.2 98%
    13 1.00 0.0662 0.0022 1.3593 0.0459 0.1492 0.0015 813.0 69.6 871.6 19.8 896.7 8.6 97%
    14 0.46 0.0634 0.0013 0.9860 0.0207 0.1126 0.0010 720.4 44.4 696.7 10.6 687.7 5.7 98%
    15 0.25 0.0640 0.0012 1.0064 0.0195 0.1138 0.0009 742.6 39.7 707.1 9.9 694.5 5.5 98%
    16 1.22 0.0742 0.0031 1.5613 0.0621 0.1542 0.0019 1055.6 84.7 955.0 24.6 924.3 10.7 96%
    17 0.44 0.0699 0.0016 1.3373 0.0284 0.1386 0.0011 924.1 45.2 862.1 12.4 836.7 6.1 97%
    18 1.30 0.0680 0.0019 1.3647 0.0396 0.1450 0.0014 869.4 59.3 873.9 17.0 873.1 7.8 99%
    19 2.49 0.0574 0.0012 0.6859 0.0149 0.0865 0.0007 509.3 46.3 530.3 9.0 534.6 4.3 99%
    20 0.91 0.0694 0.0019 1.2859 0.0352 0.1338 0.0010 922.2 54.8 839.5 15.7 809.4 5.7 96%
    21 0.61 0.0558 0.0010 0.6272 0.0110 0.0813 0.0006 442.6 8.3 494.4 6.9 504.1 3.4 98%
    22 1.67 0.0616 0.0020 0.8547 0.0267 0.1005 0.0010 661.1 68.5 627.2 14.6 617.3 6.1 98%
    23 0.68 0.1056 0.0015 4.2387 0.0633 0.2927 0.0057 1725.6 26.5 1681.5 12.3 1654.9 28.3 98%
    24 0.92 0.0603 0.0016 0.9923 0.0254 0.1194 0.0011 613.0 52.8 699.9 12.9 727.0 6.3 96%
    25 0.54 0.0756 0.0013 1.8553 0.0299 0.1777 0.0012 1083.3 33.3 1065.3 10.7 1054.6 6.8 98%
    26 0.82 0.0583 0.0011 0.6782 0.0125 0.0841 0.0006 542.6 40.7 525.7 7.6 520.5 3.6 99%
    27 0.70 0.0777 0.0013 1.6557 0.0310 0.1539 0.0017 1140.4 32.6 991.7 11.9 922.9 9.7 92%
    28 1.13 0.0852 0.0013 2.4636 0.0394 0.2090 0.0015 1320.4 25.0 1261.4 11.6 1223.6 7.9 96%
    29 0.76 0.0806 0.0013 2.3000 0.0370 0.2066 0.0015 1210.8 26.9 1212.3 11.4 1210.4 7.8 99%
    30 1.47 0.0603 0.0018 0.7539 0.0217 0.0907 0.0008 616.7 63.0 570.5 12.6 559.7 4.9 98%
    31 0.75 0.0796 0.0012 2.1580 0.0339 0.1961 0.0014 1187.0 25.0 1167.6 10.9 1154.1 7.4 98%
    32 0.51 0.0637 0.0015 0.9658 0.0225 0.1101 0.0010 731.5 51.8 686.3 11.6 673.1 5.5 98%
    33 0.63 0.0828 0.0015 2.3029 0.0416 0.2014 0.0016 1264.8 34.7 1213.2 12.8 1182.8 8.6 97%
    34 1.73 0.0606 0.0014 0.8016 0.0182 0.0958 0.0008 633.4 50.0 597.7 10.3 589.8 4.5 98%
    35 0.33 0.0706 0.0012 1.5283 0.0267 0.1565 0.0010 946.3 39.8 941.8 10.7 937.5 5.6 99%
    36 0.85 0.0594 0.0012 0.7416 0.0158 0.0903 0.0006 581.2 13.9 563.3 9.2 557.3 3.8 98%
    37 0.63 0.0742 0.0014 1.8205 0.0345 0.1774 0.0013 1047.8 38.9 1052.9 12.4 1052.5 7.2 99%
    38 1.85 0.0724 0.0022 1.4793 0.0463 0.1481 0.0015 998.2 29.5 922.0 19.0 890.4 8.6 96%
    39 0.84 0.0692 0.0013 1.4375 0.0272 0.1502 0.0012 905.6 39.7 904.7 11.3 901.9 6.8 99%
    40 2.62 0.0557 0.0019 0.6332 0.0211 0.0825 0.0008 442.6 77.8 498.1 13.1 511.2 4.9 97%
    41 0.88 0.0778 0.0019 2.1660 0.0549 0.2010 0.0021 1142.6 48.1 1170.2 17.6 1180.6 11.1 99%
    42 0.70 0.0767 0.0013 2.0746 0.0352 0.1952 0.0014 1122.2 33.3 1140.4 11.6 1149.5 7.5 99%
    43 0.61 0.0679 0.0020 1.2444 0.0363 0.1329 0.0011 864.8 -136.1 820.9 16.5 804.1 6.5 97%
    44 0.92 0.0945 0.0024 3.2804 0.0807 0.2519 0.0023 1520.4 48.5 1476.4 19.2 1448.2 12.1 98%
    45 1.17 0.0578 0.0015 0.7368 0.0189 0.0924 0.0008 524.1 62.0 560.5 11.1 569.8 4.8 98%
    46 0.59 0.0734 0.0012 1.8640 0.0314 0.1835 0.0013 1025.0 34.1 1068.4 11.2 1085.9 7.0 98%
    47 2.34 0.0778 0.0026 2.0800 0.0732 0.1927 0.0022 1142.6 66.7 1142.3 24.1 1136.2 11.8 99%
    48 1.87 0.0624 0.0020 0.8138 0.0259 0.0945 0.0009 687.1 68.5 604.6 14.5 582.2 5.1 96%
    49 0.29 0.2297 0.0029 16.8191 0.2163 0.5291 0.0036 3050.3 19.3 2924.6 12.5 2737.5 15.3 93%
    50 0.88 0.0581 0.0015 0.7516 0.0200 0.0938 0.0009 531.5 57.4 569.2 11.6 578.1 5.1 98%
    51 1.39 0.1312 0.0021 6.9215 0.1175 0.3813 0.0030 2114.5 27.9 2101.4 15.1 2082.3 14.1 99%
    52 0.69 0.0695 0.0010 1.2726 0.0213 0.1323 0.0011 922.2 31.5 833.5 9.5 801.2 6.3 96%
    53 1.10 0.0793 0.0013 2.2516 0.0376 0.2059 0.0018 1188.9 33.3 1197.3 11.8 1206.7 9.6 99%
    54 0.63 0.0792 0.0174 1.1081 0.2478 0.1007 0.0009 1176.9 413.9 757.3 119.4 618.2 5.0 79%
    55 0.74 0.0625 0.0012 0.9079 0.0185 0.1052 0.0010 694.5 47.2 655.9 9.8 644.6 5.6 98%
    56 1.57 0.1474 0.0023 8.6420 0.1382 0.4249 0.0032 2316.7 27.2 2301.0 14.6 2282.8 14.6 99%
    57 1.39 0.0581 0.0014 0.7029 0.0178 0.0876 0.0008 600.0 53.7 540.5 10.6 541.1 4.8 99%
    58 1.12 0.0719 0.0022 1.4165 0.0425 0.1431 0.0014 983.3 61.6 895.9 17.9 862.1 8.2 96%
    59 0.93 0.0673 0.0034 1.0268 0.0510 0.1117 0.0015 855.6 102.8 717.3 25.6 682.5 8.5 95%
    60 0.65 0.0788 0.0013 2.1596 0.0345 0.1985 0.0014 1168.5 27.6 1168.1 11.1 1167.4 7.4 99%
    61 1.56 0.0779 0.0022 2.0841 0.0596 0.1943 0.0020 1146.3 89.8 1143.6 19.6 1144.9 10.7 99%
    62 0.79 0.0777 0.0015 2.1423 0.0416 0.1998 0.0018 1138.9 37.0 1162.6 13.5 1174.0 9.6 99%
    63 1.08 0.0663 0.0018 1.3365 0.0345 0.1465 0.0013 814.5 51.7 861.7 15.0 881.0 7.2 97%
    64 1.01 0.2733 0.0042 24.3614 0.3677 0.6440 0.0047 3325.0 24.5 3283.0 14.9 3204.6 18.4 97%
    65 0.13 0.0594 0.0013 0.8437 0.0187 0.1027 0.0010 588.9 48.1 621.2 10.3 630.4 5.6 98%
    66 0.69 0.0775 0.0015 2.1110 0.0404 0.1970 0.0014 1144.5 38.9 1152.4 13.2 1159.3 7.7 99%
    67 1.48 0.0672 0.0015 1.1955 0.0258 0.1291 0.0010 842.6 52.8 798.5 12.0 782.7 5.6 97%
    68 1.91 0.0868 0.0028 2.7844 0.0924 0.2329 0.0027 1366.7 64.0 1351.4 24.8 1349.4 14.3 99%
    69 0.33 0.0559 0.0011 0.7408 0.0147 0.0960 0.0007 450.0 13.9 562.9 8.6 590.7 4.2 95%
    70 0.89 0.0766 0.0014 1.9247 0.0345 0.1822 0.0014 1109.3 37.0 1089.7 12.0 1079.1 7.7 99%
    71 1.09 0.0601 0.0023 0.7986 0.0302 0.0970 0.0011 609.3 88.0 596.1 17.0 596.8 6.3 99%
    72 0.76 0.1563 0.0022 9.4065 0.1598 0.4352 0.0043 2416.7 24.4 2378.5 15.7 2329.1 19.3 97%
    73 1.43 0.0796 0.0027 1.7644 0.0596 0.1604 0.0017 1188.0 66.7 1032.5 21.9 959.2 9.6 92%
    74 0.80 0.0824 0.0017 2.2625 0.0458 0.1989 0.0015 1253.7 40.7 1200.7 14.3 1169.6 8.3 97%
    75 1.23 0.0835 0.0015 2.4112 0.0446 0.2084 0.0015 1281.2 30.6 1245.9 13.3 1220.4 7.9 97%
    76 1.17 0.0812 0.0012 2.2311 0.0338 0.1987 0.0013 1225.6 29.9 1190.9 10.7 1168.3 7.3 98%
    77 0.84 0.0670 0.0015 1.2193 0.0278 0.1316 0.0011 838.9 46.3 809.5 12.8 797.0 6.2 98%
    78 0.87 0.0767 0.0014 1.8068 0.0350 0.1702 0.0012 1122.2 37.0 1047.9 12.7 1013.3 6.7 96%
    79 0.70 0.2223 0.0035 17.2880 0.2872 0.5620 0.0046 2997.8 30.7 2951.0 16.1 2874.7 19.0 97%
    80 1.01 0.0794 0.0023 2.0692 0.0568 0.1893 0.0018 1183.3 56.9 1138.7 18.8 1117.4 9.7 98%
    81 1.15 0.0576 0.0022 0.7029 0.0271 0.0886 0.0010 516.7 85.2 540.5 16.2 547.5 5.8 98%
    82 1.55 0.0825 0.0028 2.1660 0.0719 0.1911 0.0021 1257.4 65.0 1170.2 23.1 1127.2 11.4 96%
    83 2.25 0.0793 0.0021 2.1464 0.0584 0.1963 0.0018 1188.9 52.9 1163.9 18.8 1155.1 9.9 99%
    84 0.93 0.0581 0.0020 0.7696 0.0273 0.0962 0.0010 531.5 75.9 579.5 15.6 592.3 5.7 97%
    85 0.88 0.0773 0.0015 2.1206 0.0395 0.1987 0.0014 1127.8 32.4 1155.5 12.9 1168.4 7.8 98%
    86 3.07 0.0629 0.0022 0.8234 0.0301 0.0943 0.0010 705.6 74.1 610.0 16.7 581.2 5.9 95%
    87 1.48 0.0784 0.0016 2.1952 0.0432 0.2031 0.0016 1166.7 40.7 1179.5 13.7 1192.0 8.3 98%
    88 1.85 0.0752 0.0021 1.9180 0.0512 0.1852 0.0017 1075.9 54.2 1087.4 17.8 1095.4 9.2 99%
    89 0.88 0.0568 0.0013 0.7243 0.0167 0.0924 0.0007 483.4 84.2 553.2 9.8 569.7 4.3 97%
    90 0.12 0.0593 0.0016 0.7576 0.0206 0.0927 0.0008 576.0 59.2 572.6 11.9 571.2 4.6 99%
    91 0.81 0.0782 0.0015 2.1632 0.0402 0.2004 0.0014 1153.7 38.4 1169.3 12.9 1177.3 7.7 99%
    92 0.87 0.0767 0.0018 2.0550 0.0452 0.1944 0.0016 1114.5 13.9 1134.0 15.0 1145.2 8.4 99%
    93 1.14 0.0565 0.0016 0.7013 0.0202 0.0901 0.0009 472.3 97.2 539.6 12.0 556.1 5.4 96%
    94 0.41 0.0738 0.0012 1.9194 0.0317 0.1878 0.0012 1036.7 63.9 1087.8 11.1 1109.5 6.7 98%
    95 0.76 0.0776 0.0014 2.1456 0.0389 0.1998 0.0014 1138.9 35.2 1163.6 12.6 1174.3 7.5 99%
    96 1.16 0.0777 0.0019 2.1620 0.0510 0.2014 0.0016 1138.9 43.5 1168.9 16.4 1182.7 8.7 98%
    97 0.87 0.0768 0.0013 2.0532 0.0357 0.1934 0.0014 1116.7 34.1 1133.4 11.9 1139.6 7.6 99%
    98 1.90 0.0662 0.0023 0.7210 0.0240 0.0795 0.0007 813.0 73.3 551.3 14.1 493.2 4.4 88%
    99 1.00 0.1066 0.0018 4.7062 0.0816 0.3195 0.0025 1742.6 31.5 1768.3 14.6 1787.2 12.0 98%
    100 1.12 0.0735 0.0017 1.9780 0.0437 0.1951 0.0016 1027.8 44.9 1108.0 14.9 1148.8 8.9 96%
    101 1.19 0.0782 0.0015 2.1731 0.0426 0.2013 0.0016 1153.7 34.3 1172.5 13.7 1182.4 8.4 99%
    102 0.57 0.0712 0.0017 1.3796 0.0337 0.1402 0.0011 964.8 44.3 880.3 14.4 845.8 6.4 96%
    103 0.63 0.0594 0.0011 0.7654 0.0143 0.0933 0.0007 583.4 38.9 577.1 8.3 575.0 4.1 99%
    104 0.94 0.0770 0.0022 2.0791 0.0584 0.1956 0.0019 1121.9 56.0 1141.9 19.3 1151.8 10.1 99%
    PM103-24-1变质岩屑石英砂岩
    1 0.52 0.0701 0.0016 1.6165 0.0386 0.1669 0.0015 931.5 52.8 976.6 15.0 995.2 8.5 98%
    2 1.00 0.0654 0.0023 1.2079 0.0415 0.1346 0.0015 787.0 73.3 804.2 19.1 814.3 8.7 98%
    3 0.43 0.0901 0.0013 2.9780 0.0479 0.2387 0.0017 1428.7 23.1 1402.0 12.3 1379.8 8.9 98%
    4 1.42 0.0774 0.0018 1.9581 0.0455 0.1835 0.0016 1131.5 46.3 1101.2 15.6 1086.1 8.5 98%
    5 0.49 0.3034 0.0039 28.6725 0.3701 0.6830 0.0039 3488.0 20.8 3442.4 12.9 3355.9 14.9 97%
    6 1.94 0.0609 0.0022 0.7885 0.0289 0.0941 0.0010 635.2 77.8 590.3 16.4 580.0 6.2 98%
    7 0.72 0.0583 0.0016 0.6940 0.0188 0.0863 0.0007 542.6 65.7 535.2 11.3 533.8 4.4 99%
    8 1.40 0.0612 0.0022 0.9295 0.0320 0.1109 0.0011 655.6 77.8 667.4 16.8 678.0 6.6 98%
    9 0.82 0.0597 0.0016 0.7578 0.0201 0.0918 0.0008 594.5 25.0 572.7 11.6 566.1 4.6 98%
    10 1.33 0.0560 0.0024 0.6471 0.0271 0.0846 0.0012 450.0 96.3 506.7 16.7 523.4 7.0 96%
    11 1.04 0.0725 0.0020 1.5767 0.0442 0.1575 0.0015 1011.1 56.6 961.1 17.4 942.7 8.1 98%
    12 2.22 0.0615 0.0028 0.6968 0.0314 0.0825 0.0012 657.4 91.7 536.9 18.8 511.1 6.9 95%
    13 1.09 0.1572 0.0021 9.6217 0.1382 0.4429 0.0031 2425.6 23.6 2399.2 13.3 2363.4 14.0 98%
    14 0.46 0.1607 0.0021 10.1723 0.1395 0.4580 0.0026 2464.8 23.3 2450.6 12.8 2430.8 11.5 99%
    15 0.61 0.0621 0.0019 0.7873 0.0244 0.0920 0.0008 679.6 65.9 589.7 13.9 567.6 5.0 96%
    16 0.65 0.0735 0.0016 1.7430 0.0387 0.1717 0.0013 1027.8 43.4 1024.6 14.3 1021.6 7.2 99%
    17 2.14 0.0572 0.0018 0.6366 0.0196 0.0813 0.0008 498.2 68.5 500.2 12.2 503.9 4.9 99%
    18 0.41 0.0653 0.0012 0.9383 0.0185 0.1040 0.0007 783.3 45.4 672.0 9.7 637.7 4.2 94%
    19 0.51 0.0569 0.0020 0.7464 0.0268 0.0956 0.0010 487.1 79.6 566.1 15.6 588.7 5.9 96%
    20 0.98 0.1049 0.0014 4.4041 0.0618 0.3037 0.0018 1722.2 25.8 1713.1 11.7 1709.6 9.0 99%
    21 1.32 0.1156 0.0016 5.3437 0.0718 0.3346 0.0023 1900.0 24.4 1875.9 11.6 1860.7 11.2 99%
    22 0.80 0.0808 0.0014 2.2684 0.0404 0.2029 0.0013 1217.0 34.1 1202.5 12.6 1190.7 7.0 99%
    23 0.30 0.0733 0.0013 1.6602 0.0276 0.1638 0.0012 1033.3 35.2 993.4 10.6 978.1 6.5 98%
    24 0.98 0.0738 0.0016 1.6178 0.0357 0.1587 0.0015 1035.2 44.4 977.1 13.8 949.6 8.3 97%
    25 0.38 0.0695 0.0014 0.9435 0.0220 0.0975 0.0008 916.7 47.2 674.7 11.5 599.8 4.7 88%
    26 0.18 0.0623 0.0016 0.9586 0.0240 0.1115 0.0009 683.3 58.3 682.6 12.5 681.2 5.3 99%
    27 1.31 0.0817 0.0017 2.3068 0.0469 0.2046 0.0016 1238.9 39.7 1214.4 14.4 1199.7 8.8 98%
    28 0.40 0.0613 0.0017 0.8431 0.0234 0.0995 0.0009 650.0 59.3 620.8 12.9 611.7 5.2 98%
    29 0.48 0.0848 0.0016 2.4290 0.0479 0.2069 0.0017 1322.2 36.0 1251.2 14.2 1212.5 9.2 96%
    30 1.38 0.0639 0.0021 0.7674 0.0261 0.0867 0.0009 738.9 36.1 578.3 15.0 536.1 5.3 92%
    31 1.43 0.0563 0.0012 0.6510 0.0138 0.0838 0.0006 464.9 52.8 509.1 8.5 518.6 3.8 98%
    32 0.67 0.0773 0.0021 2.1130 0.0557 0.1985 0.0019 1131.5 53.7 1153.0 18.2 1167.0 10.4 98%
    33 0.35 0.0571 0.0013 0.6400 0.0149 0.0811 0.0007 498.2 45.4 502.3 9.2 503.0 4.3 99%
    34 0.47 0.0916 0.0017 3.1822 0.0594 0.2513 0.0020 1461.1 34.7 1452.8 14.4 1445.0 10.2 99%
    35 1.01 0.0715 0.0012 1.5794 0.0263 0.1599 0.0010 972.2 34.4 962.1 10.4 956.2 5.8 99%
    36 0.39 0.0662 0.0016 1.1797 0.0285 0.1290 0.0012 813.0 48.1 791.2 13.3 782.0 6.8 98%
    37 1.15 0.0806 0.0014 2.2331 0.0414 0.2006 0.0015 1210.8 39.8 1191.5 13.0 1178.4 8.3 98%
    38 0.61 0.0583 0.0011 0.6684 0.0130 0.0828 0.0006 542.6 40.7 519.7 7.9 513.0 3.6 98%
    39 0.49 0.0903 0.0015 3.2054 0.0548 0.2571 0.0020 1431.5 32.9 1458.5 13.3 1474.9 10.2 98%
    40 0.65 0.0731 0.0012 1.7296 0.0296 0.1711 0.0011 1016.7 33.3 1019.6 11.0 1018.2 6.3 99%
    41 0.72 0.1635 0.0025 10.5306 0.1562 0.4651 0.0032 2492.3 25.9 2482.6 13.9 2462.0 14.0 99%
    42 0.40 0.0828 0.0026 2.4895 0.0774 0.2178 0.0025 1265.1 59.4 1269.0 22.5 1270.2 13.3 99%
    43 0.93 0.0779 0.0014 2.1602 0.0396 0.2005 0.0015 1144.1 37.0 1168.3 12.7 1178.3 7.8 99%
    44 0.41 0.1796 0.0022 12.1245 0.1510 0.4877 0.0033 2649.1 20.4 2614.1 11.8 2560.6 14.4 97%
    45 1.11 0.0871 0.0014 2.7814 0.0493 0.2308 0.0020 1362.0 31.5 1350.5 13.3 1338.6 10.7 99%
    46 1.53 0.0805 0.0014 2.2687 0.0389 0.2040 0.0016 1209.3 33.8 1202.6 12.1 1196.5 8.7 99%
    47 0.53 0.0771 0.0013 2.0674 0.0361 0.1939 0.0015 1124.1 39.8 1138.1 12.0 1142.5 8.3 99%
    48 0.72 0.1069 0.0018 4.6740 0.0804 0.3160 0.0022 1746.6 37.2 1762.6 14.4 1770.1 11.0 99%
    49 0.49 0.0704 0.0015 1.4978 0.0316 0.1538 0.0013 942.6 42.6 929.5 12.9 922.4 7.3 99%
    50 0.85 0.0798 0.0018 2.1731 0.0491 0.1970 0.0015 1194.4 45.8 1172.5 15.7 1159.4 8.2 98%
    51 0.59 0.2140 0.0027 17.0406 0.2152 0.5752 0.0036 2936.1 20.1 2937.1 12.3 2929.1 14.9 99%
    52 1.41 0.0766 0.0015 2.1213 0.0398 0.2014 0.0026 1110.8 38.9 1155.8 13.0 1182.8 13.8 97%
    53 1.16 0.0766 0.0015 2.0926 0.0437 0.1972 0.0016 1122.2 39.7 1146.4 14.4 1160.5 8.6 98%
    54 1.23 0.0778 0.0022 2.1097 0.0581 0.1968 0.0020 1142.6 54.5 1152.0 19.0 1157.9 10.6 99%
    55 1.00 0.0702 0.0012 1.5253 0.0252 0.1572 0.0012 1000.0 33.3 940.6 10.1 941.1 6.6 99%
    56 0.70 0.0738 0.0056 0.8869 0.0604 0.0875 0.0008 1035.2 155.6 644.7 32.5 540.9 4.6 82%
    57 0.77 0.0805 0.0019 2.2665 0.0556 0.2034 0.0018 1209.3 47.4 1201.9 17.3 1193.4 9.6 99%
    58 0.42 0.0696 0.0012 1.4561 0.0252 0.1511 0.0010 916.7 34.1 912.4 10.4 907.3 5.8 99%
    59 0.35 0.0803 0.0013 2.3382 0.0428 0.2103 0.0018 1205.6 32.2 1224.0 13.0 1230.3 9.9 99%
    60 0.88 0.0770 0.0015 1.9770 0.0395 0.1857 0.0013 1120.4 37.8 1107.7 13.5 1097.8 7.2 99%
    61 0.13 0.0773 0.0012 2.0022 0.0305 0.1875 0.0013 1128.7 30.1 1116.3 10.4 1107.7 7.0 99%
    62 0.86 0.0791 0.0015 2.1913 0.0426 0.2001 0.0014 1175.9 37.0 1178.3 13.6 1175.9 7.7 99%
    63 1.24 0.0773 0.0017 2.2031 0.0497 0.2066 0.0019 1131.5 44.4 1182.0 15.8 1210.8 10.4 97%
    64 0.76 0.0878 0.0014 2.7846 0.0466 0.2292 0.0015 1388.9 30.7 1351.4 12.5 1330.3 8.1 98%
    65 0.99 0.0620 0.0017 0.7953 0.0202 0.0932 0.0008 675.9 57.4 594.2 11.4 574.7 4.9 96%
    66 0.29 0.0621 0.0014 0.8625 0.0199 0.1006 0.0008 679.6 50.0 631.5 10.9 618.0 4.7 97%
    67 0.70 0.1061 0.0015 4.5039 0.0696 0.3070 0.0020 1800.0 27.0 1731.7 12.9 1725.9 10.0 99%
    68 0.72 0.1058 0.0016 4.5361 0.0738 0.3104 0.0024 1728.7 32.4 1737.6 13.6 1742.8 11.7 99%
    69 0.61 0.1891 0.0024 13.3110 0.1752 0.5095 0.0034 2734.9 20.7 2702.0 12.6 2654.3 14.6 98%
    70 0.79 0.0594 0.0014 0.7976 0.0191 0.0973 0.0007 588.9 51.8 595.5 10.8 598.8 4.4 99%
    71 0.63 0.0721 0.0013 1.6284 0.0309 0.1635 0.0012 990.7 38.1 981.2 12.0 976.0 6.6 99%
    72 0.93 0.0748 0.0015 1.8633 0.0375 0.1809 0.0015 1062.7 42.6 1068.1 13.3 1072.1 8.2 99%
    73 1.38 0.0592 0.0017 0.7692 0.0213 0.0946 0.0010 572.3 63.0 579.3 12.2 582.6 5.7 99%
    74 1.22 0.2448 0.0032 20.7897 0.2894 0.6145 0.0042 3151.6 21.0 3128.8 13.7 3088.2 16.8 98%
    75 0.91 0.1639 0.0021 10.6402 0.1426 0.4699 0.0031 2498.2 21.1 2492.2 12.6 2483.3 13.8 99%
    76 0.48 0.1063 0.0013 4.4756 0.0585 0.3046 0.0019 1738.9 23.6 1726.5 10.9 1713.9 9.3 99%
    77 1.19 0.0734 0.0012 1.6567 0.0298 0.1632 0.0012 1027.8 34.7 992.1 11.4 974.3 6.8 98%
    78 1.49 0.1018 0.0039 2.9249 0.1327 0.2043 0.0019 1657.7 71.4 1388.4 34.3 1198.4 10.4 85%
    79 0.48 0.0709 0.0013 1.5366 0.0270 0.1570 0.0012 955.2 36.3 945.2 10.8 940.3 6.9 99%
    80 0.29 0.0726 0.0013 1.6384 0.0293 0.1631 0.0012 1005.6 35.2 985.1 11.3 974.2 6.7 98%
    81 0.99 0.0825 0.0017 2.3293 0.0462 0.2048 0.0017 1257.4 39.4 1221.3 14.1 1200.8 9.4 98%
    82 0.96 0.1007 0.0019 3.9489 0.0731 0.2843 0.0022 1636.7 -163.9 1623.8 15.0 1613.0 11.1 99%
    83 1.05 0.0601 0.0015 0.7452 0.0180 0.0900 0.0007 605.6 51.8 565.4 10.5 555.6 4.1 98%
    84 2.23 0.0598 0.0018 0.7110 0.0194 0.1138 0.0281 594.5 63.7 545.3 11.5 694.9 162.7 74%
    85 0.77 0.0594 0.0022 0.8915 0.0323 0.1094 0.0013 588.9 79.6 647.2 17.3 669.3 7.4 96%
    86 0.56 0.0696 0.0022 1.0696 0.0674 0.1039 0.0032 916.7 65.6 738.5 33.1 637.2 18.9 85%
    87 0.78 0.0587 0.0018 0.6651 0.0211 0.0825 0.0008 553.7 66.7 517.7 12.9 510.8 4.9 98%
    88 1.25 0.0818 0.0018 2.3094 0.0527 0.2047 0.0017 1240.4 42.6 1215.2 16.2 1200.7 9.4 98%
    89 0.62 0.0772 0.0015 2.1323 0.0424 0.2007 0.0016 1127.8 39.4 1159.3 13.8 1178.8 8.5 98%
    90 0.40 0.0737 0.0033 1.6407 0.0698 0.1641 0.0022 1032.4 90.3 986.0 26.8 979.5 12.3 99%
    91 3.22 0.0779 0.0040 0.8864 0.0511 0.0816 0.0010 1146.3 102.6 644.4 27.5 505.4 6.0 75%
    92 0.75 0.0737 0.0013 1.7081 0.0296 0.1683 0.0012 1033.0 67.6 1011.6 11.1 1003.0 6.6 99%
    93 0.94 0.0562 0.0025 0.6587 0.0280 0.0870 0.0012 461.2 100.0 513.8 17.2 537.7 7.0 95%
    94 0.48 0.1547 0.0018 9.4980 0.1182 0.4444 0.0029 2398.5 19.4 2387.4 11.5 2370.5 12.8 99%
    95 1.25 0.0568 0.0014 0.7428 0.0185 0.0947 0.0008 483.4 84.2 564.0 10.8 583.2 4.9 96%
    96 0.46 0.1065 0.0017 4.6188 0.0793 0.3143 0.0025 1739.8 30.1 1752.7 14.4 1761.9 12.3 99%
    97 0.20 0.0579 0.0010 0.7353 0.0133 0.0920 0.0007 524.1 38.9 559.7 7.8 567.4 4.1 98%
    98 2.08 0.1729 0.0025 11.8799 0.1857 0.4976 0.0042 2587.0 24.4 2595.0 14.7 2603.4 18.3 99%
    99 0.70 0.0573 0.0014 0.6438 0.0166 0.0813 0.0007 501.9 55.6 504.7 10.3 503.7 3.9 99%
    100 0.59 0.0575 0.0014 0.7310 0.0181 0.0922 0.0008 522.3 55.6 557.1 10.6 568.3 4.6 98%
    101 0.89 0.1416 0.0022 8.1929 0.1262 0.4186 0.0032 2247.2 26.5 2252.6 14.0 2254.2 14.5 99%
    102 1.78 0.0770 0.0014 2.1429 0.0367 0.2016 0.0016 1121.3 39.8 1162.8 11.9 1183.7 8.4 98%
    103 0.79 0.0610 0.0017 0.8919 0.0245 0.1062 0.0010 638.9 61.1 647.4 13.1 650.5 6.0 99%
    104 1.28 0.0769 0.0026 0.9166 0.0343 0.0853 0.0007 1118.2 67.4 660.6 18.2 527.9 4.2 77%
    下载: 导出CSV
  • [1]

    Anderson T. Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation[J]. Chemical Geology, 2005, 216(3/4): 249-270.

    [2]

    Cawood P A, Nemchin A A. Provenance record of a rift basin: U/Pb ages of detrital zircons from the Perth Basin, Western Australia[J]. Sedimentary Geology, 2000, 134: 209-234. doi: 10.1016/S0037-0738(00)00044-0

    [3]

    Cawood P A, Johnson M R W, Nemchin A A. Early Paleozoic orogenesis along the Indian margin of Gondwana: Tectonic response to Gondwana assembly[J]. Earth and Planetary Science Letters, 2007, 255(1/2): 70-84.

    [4]

    Cawood P A, Hawkesworth C J, Dhuime B. Detrital zircon record and tectonic setting[J]. Geology, 2012, 40(10): 875-878. doi: 10.1130/G32945.1

    [5]

    Clark D J, Hensen B J, Kinny P D. Geochronological constraints for a two-stage history of the Albany-Fraser Orogen, Western Australia[J]. Precambrain Research, 2000, 102(3/4): 155-183.

    [6]

    Chen W T, Zhou M F, Zhao X F. Late Paleoproterozoic sedimentary and mafic rocks in the Hekou area, SW China: Implication for the reconstruction of the Yangtze Block in Columbia[J]. Precambrian Research, 2013, 231: 61-77. doi: 10.1016/j.precamres.2013.03.011

    [7]

    Downes P J, Dunkley D J, Fletcher I R, et al. Zirconolite, zircon and monazite-(Ce)U-Th-Pb age constraints on the emplacement, deformation and alteration history of the Cummins Range carbonatite complex, Halls Creek Orogen, Kimberley region, Western Australia[J]. Mineralogy and Petrology, 2016, 110(2/3): 199-222.

    [8]

    Dong C Y, Li C, Wan Y S, et al. Detrital zircon age model of Ordovician Wenquan quartzite south of Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet: Constraint on tectonic affinity and source regions[J]. Science China (Earth Sciences), 2011, 54(7): 1034-1042. doi: 10.1007/s11430-010-4166-x

    [9]

    Feng Q L. Stratigraphy of volcanic rocks in the Changning-Menglian belt in southwestern Yunnan, China[J]. Journal of Asian Earth Sciences, 2002, 20(6): 657-664. doi: 10.1016/S1367-9120(02)00006-8

    [10]

    Fedo C M, Sircombe K N, Rainbird R H. Detrital zircon analysis of the sedimentary record[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1): 277-303. doi: 10.2113/0530277

    [11]

    Fontaine H. Permian of Southeast Asia: an overview[J]. Journal of Asian Earth Sciences, 2002, 20(6): 567-588. doi: 10.1016/S1367-9120(01)00076-1

    [12]

    Gehrels G, Kapp P, DeCelles P, et al. Detrital zircon geochronology of pre-Tertiary strata in the Tibetan-Himalayan or ogen[J]. Tectonics, 2011, 30(5): TC5016.

    [13]

    Guo L, Zhang H F, Harris N, et al. Late Devonian-Early Carboniferous magmatism in the Lhasa terrane and its tectonic implications: Evidences from detrital zircons in the Nyingchi Complex[J]. Lithos, 2016, 245: 47-59. doi: 10.1016/j.lithos.2015.06.018

    [14]

    Grimes C B, John B E, Kelemen P B, et al. Trace element chemistry of zircons from oceanic crust: A method for distinguishing detrital zircon provenance[J]. Geology, 2007, 35(7): 643-646. doi: 10.1130/G23603A.1

    [15]

    Hughes N C, Myrow P M, McKenzie N R, et al. Age and implications of the phosphatic Birmania Formation, Rajasthan, India[J]. Precambrian Research, 2015, 267: 164-173. doi: 10.1016/j.precamres.2015.06.012

    [16]

    Jian P, Liu D, Kröner A, et al. Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (Ⅰ): Geochemistry of ophiolites, arc/back-arc assemblages and within-plate igneous rocks[J]. Lithos, 2009a, 113: 748-766. doi: 10.1016/j.lithos.2009.04.004

    [17]

    Jian P, Liu D, Kröner A, et al. Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (Ⅱ): Insights from zircon ages of ophiolites, arc/back-arc assemblages and within-plate igneous rocks and generation of the Emeishan CFB province[J]. Lithos, 2009b, 113: 767-784. doi: 10.1016/j.lithos.2009.04.006

    [18]

    Jin X C, Wang Y Z, Xie G L. Devonian to Triassic Successions of the Changning-Menglian Belt, Western Yunnan, China[J]. Acta Geologica Sinica, 2003, 77(4): 440-456. doi: 10.3321/j.issn:1000-9515.2003.04.004

    [19]

    Ksienzyk A K, Jacobs J, Boger S D, et al. U-Pb ages of metamorphic monazite and detrital zircon from the Northampton Complex: evidence of two orogenic cycles in Western Australia[J]. Precambrian Research, 2012, 198: 37-50.

    [20]

    Li C, Zhai Q G, Dong Y S, et al. High-Pressure Eclogite-Blueschist Metamorphic Belt and Closure of Paleo-Tethys Ocean in Central Qiangtang, Qinghai-Tibet Plateau[J]. Journal of Earth Science, 2009, 20(2): 209-218. doi: 10.1007/s12583-009-0021-4

    [21]

    Leier A L, Kapp P, Gehrels G E, et al. Detrital zircon geochronology of Carboniferous-Cretaceousstrata in the Lhasa terrane, southern Tibet[J]. Basin Research, 2007, 19(3): 361-378. doi: 10.1111/j.1365-2117.2007.00330.x

    [22]

    Liu X M, Gao S, Diwu C R, et al. Precambrian crustal growth of Yangtze Craton as revealed by detrital zircon studies[J]. American Journal of Science, 2008, 308(4): 421-468. doi: 10.2475/04.2008.02

    [23]

    Metcalfe I. Gondwanaland dispersion, Asian accretion and evolution of eastern Tethys[J]. Journal of the Geological Society of Australia, 1996, 43: 605-623.

    [24]

    Metcalfe I. Permian tectonic framework and palaeogeography of SE Asia[J]. Journal of Asian Earth Sciences, 2002, 20: 551-566. doi: 10.1016/S1367-9120(02)00022-6

    [25]

    Metcalfe I. Palaeozoic and Mesozoic tectonic evolution and palaeogeography of East Asian crustal fragments: The Korean Peninsula in context[J]. Gondwana Research, 2006, 9: 24-46. doi: 10.1016/j.gr.2005.04.002

    [26]

    Metcalfe I. Gondwana dispersion and Asian accretion: Tectonic and palaeogeographic evolution of eastern Tethys[J]. Journal of Asian Earth Sciences, 2013, 66: 1-33. doi: 10.1016/j.jseaes.2012.12.020

    [27]

    Meert J G. A synopsis of events related to the assembly of eastern Gondwana[J]. Tectonophysics, 2003, 362(1/4): 1-40.

    [28]

    Malone S J, Meert J G, Banerjee D M, et al. Paleomagnetism and detrital zircon geochronology of the Upper Vindhyan sequence, Son Valley and Rajasthan, India: a ca. 1000 Ma closure age for the Purana Basins[J]. Precambrian Research, 2008, 164: 137-159. doi: 10.1016/j.precamres.2008.04.004

    [29]

    McDonough W F, Sun S S. The composition of the Earth[J]. Chemical Geology, 1995, 120(3/4): 223-253.

    [30]

    Stampfli G M, Borel G D. A plate tectonic model for the Paleozoic and Mesozoic of the Tethyan domain constrained by dynamic plate boundaries and restored synthetic oceanic isochrones[C]//1st International Symposium of the Faculty of Mines on Earth Science and Engineering, Istanbul Technical University, 2002: 77.

    [31]

    Stampfli G M, Borel G D. The transmed transects in space and time: constrained on the Paleozoic evolution of Mediterranean domain[C]//Cavazza W, Roure F, Spakman W, et al. The Transmed Atlas (the Mediterranean Region from Crust to Mantle). Springer-Verlag Berlin Heidelberg, 2004: 53-90.

    [32]

    Turner C C, Meert J G, Pandit M K, et al. A detrital zircon U-Pb and Hf isotopic transect across the Son Valley sector of the Vindhyan Basin, India: Implications for basin evolution and paleogeography[J]. Gondwana Research, 2014, 26(1): 348-364. doi: 10.1016/j.gr.2013.07.009

    [33]

    Wang L J, Yu J H, Griffin W L, et al. Early crustal evolution in the western Yangtze Block: Evidence from U-Pb and Lu-Hf isotopes on detrital zircons from sedimentary rocks[J]. Precambrian Research, 2012, 222/223: 368-385. doi: 10.1016/j.precamres.2011.08.001

    [34]

    Wang L J, Griffin W L, Yu J H, et al. U-Pb and Lu-Hf isotopes in detrital zircon from Neoproterozoic sedimentary rocks in the northern Yangtze Block: Implications for Precambrian crustal evolution[J]. Gondwana Research, 2013, 23(4): 1261-1272. doi: 10.1016/j.gr.2012.04.013

    [35]

    Veevers J J, Saeed A, Belousova E A, et al. U-Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton[J]. Earth Science Reviews, 2005, 68(3): 245-279.

    [36]

    Voice P J, Kowalewski M, Eriksson K A. Quantifying the timing and rate of crustal evolution: Global compilation of radiometrically dated detrital zircon grains[J]. The Journal of Geology, 2011, 119(2): 109-126. doi: 10.1086/658295

    [37]

    Yin C Q, Lin S F, Davis D W, et al. Tectonic evolution of the southeastern margin of the Yangtze Block: Constraints from SHRIMP U-Pb and LA-ICP-MS Hf isotopic studies of zircon from the eastern Jiangnan Orogenic Belt and implications for the tectonic interpretation of South China[J]. Precambrian Research, 2013, 236: 145-156. doi: 10.1016/j.precamres.2013.07.022

    [38]

    Yang J H, Cawood P A, Du Y S, et al. Large Igneous Province and magmatic arc sourced Permian-Triassic volcanogenic sediments in China[J]. Sedimentary Geology, 2012, 261/262: 120-131. doi: 10.1016/j.sedgeo.2012.03.018

    [39]

    Zhao T Y, Feng Q L, Metcalfe I, et al. Detrital zircon U-Pb-Hf isotopes and provenance of Late Neoproterozoic and Early Paleozoic sediments of the Simao and Baoshan blocks, SWChina: Implications for Proto-Tethys and Paleo-Tethys evolution and Gondwana reconstruction[J]. Gondwana Research, 2017, 51: 193-208. doi: 10.1016/j.gr.2017.07.012

    [40]

    Zhu D C, Zhao Z D, Niu Y, et al. Lhasa terrane in southern Tibet came from Australia[J]. Geology, 2011, 39: 727-730.

    [41]

    Zhang K J, Zhang Y X, Tang X C, et al. Late Mesozoic tectonic evolution and growth of the Tibetan plateau prior to the Indo-Asian collision[J]. Earth-Science Reviews, 2012, 114: 236-249. doi: 10.1016/j.earscirev.2012.06.001

    [42]

    Zhang K J, Cai J X, Zhang Y X, et al. Eclogites from central Qiangtang, northern Tibet (China) and tectonic implications[J]. Earth and Planetary Science Letters, 2006, 245(3/4): 722-729.

    [43]

    曾文涛, 刘桂春, 冯庆来, 等. 临沧地体亲缘性及南段组物源——来自泥盆纪—石炭纪南段组碎屑锆石U-Pb年龄的证据[J]. 地质通报, 2017, 36(7): 1175-1187. doi: 10.3969/j.issn.1671-2552.2017.07.008 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20170708&flag=1

    [44]

    成都地质调查中心. 1: 5万大芒光房幅、双江县幅、文东幅区域地质矿产调查报告[R]. 2019.

    [45]

    崔春龙, 曾允孚, 黄志勋, 等. 滇西昌宁-孟连带南段组沉积环境及沉积机理[J]. 西南工学院学报, 1998, 13(1): 33-38. https://www.cnki.com.cn/Article/CJFDTOTAL-XNGX801.006.htm

    [46]

    邓军, 王庆飞, 李龚健. 复合造山和复合成矿系统: 三江特提斯例析[J]. 岩石学报, 2016, 32(8): 2225-2247. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201608001.htm

    [47]

    邓军, 王长明, 李文昌, 等. 三江特提斯复合造山与成矿作用研究态势及启示[J]. 地学前缘, 2014, 21(1): 52-64. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201401008.htm

    [48]

    邓军, 杨立强, 王长明. 三江特提斯复合造山与成矿作用研究进展[J]. 岩石学报, 2011, 27(9): 2501-2509. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201109002.htm

    [49]

    段向东. 滇西南耿马地区昌宁-孟连带盆地演化研究[D]. 中国地质大学(武汉) 博士学位论文, 2013.

    [50]

    方宗杰, 周志澄, 林敏基. 关于滇西地质的若干新认识[J]. 科学通报, 1990, 5: 363-365. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199005013.htm

    [51]

    方宗杰, 周志澄, 林敏基. 从地层学的角度探讨昌宁-孟连缝合带的若干问题[J]. 地层学杂志, 1992, 16(4): 292-303. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ199204008.htm

    [52]

    冯庆来, 刘本培, 叶玫, 等. 滇西南南段组和拉巴群地质时代及构造背景[J]. 地层学杂志, 1996, 20(3): 183-189. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ199603003.htm

    [53]

    耿元生, 旷红伟, 杜利林, 等. 从哥伦比亚超大陆裂解事件论古/中元古代的界限[J]. 岩石学报, 2019, 35(8): 2299-2324. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201908002.htm

    [54]

    龚一鸣, 杜远生, 冯庆来, 等. 造山带沉积地质与圈层耦合[M]. 武汉: 中国地质大学出版社, 1996: 1-16.

    [55]

    贾进华. 滇西南昌宁-孟连带南段群沉积特征及其构造古地理意义——兼论临沧地体的性质[J]. 岩相古地理, 1994, 14(4): 42-48. https://www.cnki.com.cn/Article/CJFDTOTAL-YXGD199404004.htm

    [56]

    金小赤, 王义昭, 谢广连. 滇西昌宁-孟连带的地层格架[J]. 地质通报, 2002, 21(6): 315-321. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20020681&flag=1

    [57]

    李三忠, 赵国春, 孙敏. 华北克拉通早元古代拼合与Columbia超大陆形成研究进展[J]. 科学通报, 2016, 61(9): 919-925. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201609004.htm

    [58]

    李维科, 王晓林, 刘兵, 等. 滇西保山地块南部公养河群研究新进展[J]. 地质通报, 2018, 37(11): 1970-1979. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20181102&flag=1

    [59]

    李兴振, 潘桂棠, 罗建宁. 论三江地区冈瓦纳和劳亚大陆的分界[J]. 青藏高原地质文集, 1990, (20): 217-233. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199012001022.htm

    [60]

    李永森, 陈炳蔚. 怒江、澜沧江、金沙江地区构造与成矿作用[J]. 矿床地质, 1991, 10(4): 289-299. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ199104000.htm

    [61]

    刘本培, 冯庆来, 方念乔, 等. 滇西南昌宁-孟连带和澜沧江带古特提斯多岛洋构造演化[J]. 地球科学——中国地质大学学报, 1993, 18(5): 529-539. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199305000.htm

    [62]

    毛晓长. 保山-镇康地块及邻区早古生代地质特征及特提斯构造演化[D]. 中国地质大学(北京) 博士学位论文, 2016.

    [63]

    聂小妹. 滇西南及泰国北部古生代早中期特提斯演化研究[D]. 中国地质大学(武汉) 博士学位论文, 2016.

    [64]

    潘桂棠, 陆松年, 肖庆辉, 等. 中国大地构造阶段划分和演化[J]. 地学前缘, 2016, 23(6): 1-23. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201606006.htm

    [65]

    彭虎, 李才, 解超明, 等. 藏北羌塘中部日湾茶卡组物源——LA-ICP-MS锆石U-Pb年龄及稀土元素特征[J]. 地质通报, 2014, 33(11): 1715-1727. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20141108&flag=1

    [66]

    彭智敏, 王保弟, 胡金锋, 等. 云南滇西地区早古生代增生杂岩的厘定及其洋壳俯冲消减作用——基于1: 5万文东幅地质调查的新认识[J]. 中国地质, 2022, 49(5): 1656-1672. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202205019.htm

    [67]

    彭智敏, 王国之, 王保弟, 等. 云南邦丙澜沧岩群中发现蓝闪石榴辉岩[J]. 成都理工大学学报(自然科学版), 2019, 46(5): 639-640. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201905014.htm

    [68]

    宋培平, 丁林, 李震宇, 等. 北羌塘地块的"前世今生"[C]//2018年中国地球科学联合学术年会. 中国北京, 2018: 1.

    [69]

    王保弟, 王立全, 王冬兵, 等. 三江昌宁-孟连带原-古特提斯构造演化[J]. 地球科学, 2018, 43(8): 2527-2550. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201808001.htm

    [70]

    王舫, 刘福来, 冀磊, 等. 澜沧江杂岩带澜沧群浅变质岩系碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J]. 岩石学报, 2017, 33(9): 2975-2985. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201709020.htm

    [71]

    王慧宁. 昌宁-孟连造山带榴辉岩、蓝片岩和变沉积岩的岩石学、变质演化及其时古特提斯洋-陆俯冲造山的制约[D]. 中国地质科学院博士学位论文, 2020.

    [72]

    王新利, 林丽, 朱利东, 等. 对滇西昌宁-孟连带大地构造背景的认识[J]. 地质找矿论丛, 2007, 22(2): 134-138. https://www.cnki.com.cn/Article/CJFDTOTAL-DZZK200702010.htm

    [73]

    王义昭, 李兴林, 段丽兰, 等. 三江地区南段大地构造与成矿[M]. 北京: 地质出版社, 2000.

    [74]

    吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 16: 1589-1604. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416001.htm

    [75]

    邢晓婉, 张玉芝. 滇西西盟帕可组沉积时代厘定及构造意义: 锆石U-Pb年代学及Lu-Hf同位素证据[J]. 矿物岩石地球化学通报, 2016.35(5): 936-948. https://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201605022.htm

    [76]

    杨学俊, 贾小川, 熊昌利, 等. 滇西高黎贡山南段公养河群变质基性火山岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报, 2012, 31(2/3): 264-276. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2012020308&flag=1

    [77]

    于远山, 张斌辉, 陈敏华, 等. 滇西勐海西定地区南段组褶叠层构造及其研究意义[J]. 沉积与特提斯地质, 2020, 42(4): 626-641. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD202204009.htm

    [78]

    云南省地质局. 1: 20万澜沧县幅、勐海县幅区域地质报告[R]. 1982.

    [79]

    云南省地质矿产局. 1: 20万凤庆幅区域地质报告[R]. 1981.

    [80]

    云南省地质矿产局. 1: 20万孟连幅区域地质报告[R]. 1982.

    [81]

    云南省地质矿产局. 1: 20万沧源幅、上班老幅区域地质报告[R]. 1986.

    [82]

    云南省地质矿产局, 云南省区域地质志[M]. 北京: 地质出版社. 1990.

    [83]

    云南省地质矿产局. 云南省岩石地层[M]. 武汉: 中国地质大学出版社, 1996: 1-366.

    [84]

    张开均, 唐显春. 青藏高原腹地榴辉岩研究进展及其地球动力学意义[J]. 科学通报, 2009, 54(13): 1804-1814. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200913003.htm

    [85]

    赵林涛, 李三忠, 吕勇, 等. 滇西允沟岩组碎屑锆石年龄谱对相关地块亲缘性的约束[J]. 岩石学报, 2019, 35(9): 2911-2925. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201909019.htm

    [86]

    郑建彬. 昌宁-孟连带东部晚古生代碎屑岩沉积学与碎屑锆石年代学研究——对滇西古特提斯演化的指示意义[D]. 中国地质科学院博士学位论文, 2019.

    [87]

    钟大赉. 滇川西部古特提斯造山带[M]. 北京: 科学出版社, 1998.

    [88]

    周美玲, 夏小平, 彭头平, 等. 滇西保山地块早古生代碎屑锆石U-Pb-Hf同位素研究及其对冈瓦纳大陆重建的制约[J]. 岩石学报, 2020, 36(2): 469-483. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB202002009.htm

  • 加载中

(9)

(1)

计量
  • 文章访问数:  1436
  • PDF下载数:  84
  • 施引文献:  0
出版历程
收稿日期:  2021-04-12
修回日期:  2021-08-20
刊出日期:  2023-07-15

目录