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    东昆仑祁漫塔格地区乌兰乌珠尔早古生代花岗岩锆石U-Pb年代学、地球化学及其地质意义

    韩志辉 孙丰月 田楠 高宏昶 李良 赵拓飞

    韩志辉, 孙丰月, 田楠, 高宏昶, 李良, 赵拓飞, 2021. 东昆仑祁漫塔格地区乌兰乌珠尔早古生代花岗岩锆石U-Pb年代学、地球化学及其地质意义. 地球科学, 46(1): 13-30. doi: 10.3799/dqkx.2020.067
    引用本文: 韩志辉, 孙丰月, 田楠, 高宏昶, 李良, 赵拓飞, 2021. 东昆仑祁漫塔格地区乌兰乌珠尔早古生代花岗岩锆石U-Pb年代学、地球化学及其地质意义. 地球科学, 46(1): 13-30. doi: 10.3799/dqkx.2020.067
    Han Zhihui, Sun Fengyue, Tian Nan, Gao Hongchang, Li Liang, Zhao Tuofei, 2021. Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China. Earth Science, 46(1): 13-30. doi: 10.3799/dqkx.2020.067
    Citation: Han Zhihui, Sun Fengyue, Tian Nan, Gao Hongchang, Li Liang, Zhao Tuofei, 2021. Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China. Earth Science, 46(1): 13-30. doi: 10.3799/dqkx.2020.067

    东昆仑祁漫塔格地区乌兰乌珠尔早古生代花岗岩锆石U-Pb年代学、地球化学及其地质意义

    doi: 10.3799/dqkx.2020.067
    基金项目: 

    国家自然科学基金项目 41402060

    详细信息
      作者简介:

      韩志辉(1995-), 男, 硕士研究生, 主要从事矿床学研究.ORCID:0000-0001-5796-5549.E-mail:1301055924@qq.com

      通讯作者:

      孙丰月, ORCID:0000-0001-9408-7298.E-mail:sunfeng0669@sina.com

    • 中图分类号: P581

    Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China

    • 摘要: 为确定东昆仑祁漫塔格乌兰乌珠尔地区片麻状黑云母花岗岩和二长花岗岩的形成时代、岩石成因、源区性质和构造背景,对该岩石样品进行了锆石U-Pb年代学、地球化学和锆石Hf同位素研究.结果显示:片麻状黑云母花岗岩加权平均年龄为457.5±2.3 Ma,铝饱和指数A/CNK介于0.98~1.02,属准铝质岩石,Na2O/K2O比值为0.440~0.625,属于高钾钙碱性系列.二长花岗岩加权平均年龄为422.5±1.6 Ma,铝饱和指数A/CNK介于1.03~1.05,属弱过铝质岩石.二者均具有高硅(SiO2介于68.93%~74.72%)、高碱(全碱ALK介于6.83%~9.40%)、低磷(P2O5小于0.12%)等特征.富集轻稀土元素,亏损重稀土元素,δEu值为0.29~0.70,显示Eu中度负异常.富集Rb、K等大离子亲石元素,亏损Nb、Ta、P、Ti等高场强元素,属于I型花岗岩.二长花岗岩样品的εHf(t)值为-2.2~+1.4,二阶段模式年龄为1 320~1 546 Ma.结合岩石成岩年龄、地球化学特征及区域构造演化认为片麻状黑云母花岗岩(457.5±2.3 Ma)为下地壳部分熔融产物,形成于原特提斯洋向北俯冲导致的局部拉张环境.二长花岗岩(422.5±1.6 Ma)岩浆来源于中元古代新增生的下部地壳熔融产物,形成于碰撞拼贴后的伸展构造环境.

       

    • 图  1  乌兰乌珠尔地区地质简图

      图a中:KBF.东昆北断裂; KZF.东昆中断裂; KBF.东昆南断裂; ANMQNF.阿尼玛卿南缘段裂; 图b中:1.第四系;2.金水口群片麻岩;3.黑云母钾长花岗岩;4.中细粒二长花岗岩;5斑状中细粒二长花岗岩;6.片麻状黑云母花岗岩;7.闪长岩脉;8.辉绿岩脉;9.断层;10.采样位置;图a研究区位置图据李世金等(2012)

      Fig.  1.  Sketch geologica map of Wulanwuzhuer

      图  2  乌兰乌珠尔花岗岩显微照片

      Al.碱性长石;Bt.黑云母;Pl.斜长石;Qtz.石英

      Fig.  2.  The micrographs from Wulanwuzhuer granites

      图  3  乌兰乌珠尔花岗岩锆石CL图像

      Fig.  3.  Cathodoluminescence images of analyzed zircons of the Wulanwuzhuer granites

      图  4  乌兰乌珠尔花岗岩U-Pb年龄谐和图

      Fig.  4.  U-Pb concordia diagram for wulanwuzhuer granites

      图  5  乌兰乌珠尔花岗岩TAS、A/CNK-A/NK、SiO2-K2O图解

      a.据Middlemost(1994);b.据Maniar and Piccoli(1989);c.据Peccerillo and Taylor(1976)

      Fig.  5.  Total alkali versus SiO2、A/CNK-A/NK diagrams and SiO2 versus K2O for the wulanwuzhuer granites

      图  6  乌兰乌珠尔花岗岩稀土元素配分模式和微量元素蛛网图

      a.球粒陨石值据Boynton(1984);b.原始地幔值据Sun and McDonough(1989)

      Fig.  6.  Chondrite-normalized REE patterns and primitive mantle-normalized trace element patterns for the Wulanwuzhuer granites

      图  7  乌兰乌珠尔二长花岗岩锆石的εHf(t)-t图解

      Yang et al.(2006)

      Fig.  7.  εHf(t) versus t diagram of the wulanwuzhuer monzonitic granites

      图  8  乌兰乌珠尔花岗岩成因类型判别图解

      a, b, c据Whalen et al.(1987);d, e, f据Chappell(1999)

      Fig.  8.  Diagrammatic analysis of genetic types of wulanwuzhuer granites

      图  9  乌兰乌珠尔花岗岩构造环境判别图解

      Batchelor and Bowden(1985)

      Fig.  9.  Tectonic setng discrimination diagrams of the Wulanwuzhuer granites

      图  10  东昆仑地区奥陶纪-晚志留世地球动力学演化示意

      李良(2018)

      Fig.  10.  Schematic diagram of Ordovician-Late Silurian geodynamic evolution in East Kunlun area

      表  1  乌兰乌珠尔花岗岩锆石LA-ICP-MS U-Pb同位素分析结果

      Table  1.   Zircon LA-ICP-MS U-Pb isotope analysis results of Wulanwuzhuer granites

      测点号 同位素比值 含量(10-6) 232Th/238U 同位素年龄(Ma)
      207Pb/ 206Pb 207Pb/ 235U 206Pb/ 238U 208Pb/ 232Th Th U 207Pb/ 206Pb 207Pb/ 235U 206Pb/ 238U
      WLWZE-N1(黑云母花岗岩)
      WLWZE-N1-01 0.056 5 0.000 6 0.572 0 0.007 6 0.073 3 0.000 6 0.022 1 0.000 5 691 1 657 0.42 472.1 24 459.3 5 456.0 4
      WLWZE-N1-02 0.057 5 0.000 9 0.570 8 0.007 8 0.071 8 0.001 0 0.022 2 0.000 9 704 2 083 0.34 510.9 35 458.6 5 446.9 6
      WLWZE-N1-03 0.055 7 0.00 04 0.565 7 0.007 0 0.073 5 0.000 7 0.022 8 0.000 4 355 1 869 0.19 440.7 17 455.2 5 457.1 4
      WLWZE-N1-04 0.056 1 0.000 5 0.573 0 0.005 1 0.074 0 0.000 6 0.022 9 0.000 6 497 1 758 0.28 456.4 19 459.9 3 460.1 4
      WLWZE-N1-05 0.056 3 0.000 7 0.574 1 0.006 4 0.073 9 0.000 6 0.022 6 0.000 7 462 1 093 0.42 465.2 26 460.6 4 459.3 4
      WLWZE-N1-06 0.056 1 0.000 5 0.568 7 0.004 7 0.073 5 0.000 6 0.022 9 0.000 7 548 1 422 0.39 456.0 21 457.2 3 457.0 3
      WLWZE-N1-07 0.056 3 0.001 2 0.573 4 0.014 4 0.073 7 0.001 0 0.0235 0.000 8 187 442 0.42 465.2 48 460.2 9 458.3 6
      WLWZE-N1-08 0.057 7 0.001 0 0.571 7 0.010 7 0.071 8 0.000 7 0.022 2 0.000 7 114 267 0.43 519.7 38 459.1 7 447.1 4
      WLWZE-N1-09 0.055 4 0.000 6 0.554 6 0.006 9 0.072 6 0.000 7 0.022 4 0.000 5 176 866 0.20 427.7 24 448.0 5 452.0 4
      WLWZE-N1-10 0.056 0 0.000 8 0.577 5 0.007 6 0.074 8 0.000 5 0.022 9 0.000 6 292 986 0.30 451.0 31 462.8 5 464.8 3
      WLWZE-N1-11 0.056 1 0.001 0 0.567 7 0.010 1 0.073 6 0.000 6 0.022 8 0.000 7 96 201 0.48 455.5 40 456.5 7 457.6 4
      WLWZE-N1-12 0.055 9 0.000 9 0.569 7 0.009 4 0.073 7 0.000 8 0.022 2 0.000 7 464 1 135 0.41 446.4 37 457.8 6 458.5 5
      WLWZE-N1-13 0.056 1 0.000 4 0.568 8 0.004 9 0.073 3 0.000 5 0.022 1 0.000 3 742 1 565 0.47 457.6 17 457.2 3 456.3 3
      WLWZE-N1-14 0.055 7 0.000 7 0.564 7 0.008 8 0.073 6 0.000 9 0.022 3 0.000 5 212 400 0.53 440.6 28 454.6 6 457.9 5
      WLWZE-N1-15 0.061 3 0.000 8 0.637 2 0.010 5 0.075 2 0.000 6 0.030 7 0.000 9 381 2 489 0.15 649.6 27 500.6 7 467.6 4
      WLWZE-N1-16 0.056 3 0.000 7 0.565 4 0.009 3 0.072 5 0.000 7 0.022 2 0.000 4 337 698 0.48 465.4 29 455.0 6 451.3 5
      WLWZE-N1-17 0.055 9 0.000 5 0.568 8 0.007 5 0.073 5 0.000 6 0.023 1 0.000 3 413 1 060 0.39 449.7 21 457.2 5 457.4 4
      WLWZE-N1-18 0.062 4 0.000 6 0.636 3 0.008 9 0.073 8 0.000 6 0.025 4 0.000 2 784 2 593 0.30 686.5 20 500.0 6 459.1 4
      WLWZE-N1-19 0.056 0 0.000 4 0.573 2 0.005 3 0.074 1 0.000 4 0.022 5 0.000 2 613 1 294 0.47 450.8 16 460.1 3 460.9 2
      WLWZE-N1-20 0.064 7 0.000 8 0.607 8 0.010 2 0.068 0 0.000 5 0.027 0 0.000 4 473 1 316 0.36 764.6 27 482.2 6 424.1 3
      WLWZE-N1-21 0.056 7 0.000 6 0.560 9 0.008 4 0.071 6 0.000 5 0.022 6 0.000 3 400 994 0.40 480.1 23 452.1 5 445.6 3
      WLWZE-N1-22 0.055 7 0.001 2 0.569 1 0.014 5 0.074 0 0.000 8 0.022 7 0.000 5 186 363 0.51 441.0 47 457.5 9 460.0 5
      WLWZE-N1-23 0.055 5 0.001 0 0.569 3 0.016 3 0.073 9 0.001 1 0.022 1 0.000 6 427 1 152 0.37 432.8 41 457.5 11 459.6 7
      WLWZE-N1-24 0.057 2 0.000 9 0.569 2 0.010 9 0.072 0 0.000 6 0.022 0 0.000 5 257 508 0.51 500.8 34 457.5 7 448.1 4
      WLWZE-N4(二长花岗岩)
      WLWZE-N4-01 0.055 6 0.000 5 0.518 6 0.005 9 0.067 4 0.000 5 0.021 6 0.001 1 576 1 503 0.38 436.2 18 424.2 4 420.4 3
      WLWZE-N4-02 0.055 5 0.000 5 0.514 7 0.005 7 0.067 1 0.000 6 0.023 7 0.001 1 700 2 164 0.32 431.0 19 421.6 4 418.7 4
      WLWZE-N4-03 0.055 0 0.000 5 0.518 6 0.005 0 0.068 2 0.000 4 0.021 4 0.000 4 1 040 2 077 0.50 411.5 19 424.2 3 425.5 2
      WLWZE-N4-04 0.054 8 0.000 5 0.515 0 0.005 2 0.068 0 0.000 5 0.021 1 0.000 5 493 1 398 0.35 403.8 19 421.8 4 424.0 3
      WLWZE-N4-05 0.060 4 0.000 4 0.525 8 0.004 7 0.063 1 0.000 5 0.022 8 0.000 5 431 1 595 0.27 616.9 16 429.0 3 394.3 3
      WLWZE-N4-06 0.055 3 0.000 7 0.521 5 0.008 2 0.068 2 0.000 9 0.021 3 0.000 7 347 2 186 0.16 424.3 29 426.1 6 425.2 5
      WLWZE-N4-07 0.057 7 0.000 4 0.522 3 0.004 2 0.065 6 0.000 5 0.021 2 0.000 3 519 1 916 0.27 518.5 14 426.7 3 409.4 3
      WLWZE-N4-08 0.056 3 0.001 0 0.523 5 0.010 1 0.067 2 0.000 9 0.021 2 0.000 8 461 1 943 0.24 464.1 38 427.5 7 419.0 5
      WLWZE-N4-09 0.062 5 0.000 4 0.564 9 0.005 3 0.065 4 0.000 4 0.024 2 0.000 4 188 445 0.42 690.2 15 454.7 4 408.3 2
      WLWZE-N4-10 0.057 5 0.000 3 0.521 3 0.004 6 0.065 6 0.000 4 0.017 6 0.000 2 531 1 292 0.41 510.7 11 426.0 3 409.6 3
      WLWZE-N4-11 0.055 4 0.000 4 0.516 2 0.004 5 0.067 4 0.000 5 0.022 4 0.000 6 163 5 602 0.03 429.0 18 422.6 3 420.6 3
      WLWZE-N4-12 0.055 8 0.000 5 0.517 7 0.005 7 0.067 2 0.000 5 0.019 4 0.000 4 124 4 587 0.03 445.8 19 423.6 4 419.1 3
      WLWZE-N4-13 0.055 1 0.000 4 0.517 1 0.005 4 0.067 9 0.000 5 0.020 4 0.000 2 755 2 817 0.27 416.6 16 423.2 4 423.7 3
      WLWZE-N4-14 0.057 0 0.000 5 0.534 1 0.006 4 0.067 9 0.000 5 0.020 3 0.000 2 531 1 589 0.33 490.7 20 434.5 4 423.2 3
      WLWZE-N4-15 0.056 6 0.000 3 0.508 4 0.003 7 0.065 0 0.000 4 0.021 6 0.000 2 509 1 947 0.26 477.3 10 417.4 3 406.1 2
      WLWZE-N4-16 0.055 4 0.000 6 0.522 8 0.006 7 0.068 2 0.000 7 0.021 2 0.000 6 198 6 531 0.03 429.9 24 427.0 5 425.5 4
      WLWZE-N4-17 0.057 2 0.000 6 0.531 6 0.006 6 0.067 3 0.000 6 0.022 9 0.000 7 394 1 127 0.35 498.6 22 432.8 4 419.6 4
      WLWZE-N4-18 0.054 9 0.000 5 0.513.0 0.005 7 0.067 7 0.000 5 0.021 0 0.000 4 360 1 714 0.21 408.2 22 420.4 4 422.0 3
      WLWZE-N4-19 0.055 5 0.000 6 0.517 1 0.006 3 0.067 6 0.000 5 0.021 0 0.000 3 1 395 5 238 0.27 430.8 24 423.2 4 421.7 3
      WLWZE-N4-20 0.055 5 0.000 4 0.539 9 0.004 5 0.070 4 0.000 4 0.021 3 0.000 2 458 1 936 0.24 433.1 15 438.4 3 438.7 3
      WLWZE-N4-21 0.055 0 0.000 3 0.517 1 0.004 8 0.067 9 0.000 5 0.020 8 0.000 5 1 224 2 964 0.41 413.9 14 423.2 3 423.7 3
      WLWZE-N4-22 0.056 0 0.000 4 0.523 3 0.004 6 0.067 7 0.000 5 0.019 6 0.000 2 862 3 030 0.28 450.6 14 427.4 3 422.5 3
      WLWZE-N4-23 0.056 0 0.000 3 0.523 1 0.004 6 0.067 6 0.000 5 0.027 4 0.001 2 1 397 4 420 0.32 453.1 14 427.2 3 421.9 3
      WLWZE-N4-24 0.055 5 0.000 6 0.518 8 0.006 3 0.067 7 0.000 6 0.021 4 0.000 7 236 1 839 0.13 431.1 23 424.4 4 422.5 4
      下载: 导出CSV

      表  2  乌兰乌珠尔花岗岩主量元素(%)、稀土元素及微量元素(10-6)分析结果

      Table  2.   Major(%), REE and trace (10-6) element copositions of the Wulanwuzhuer granites

      样号 WLWZE-N1-1 WLWZE-N1-2 WLWZE-N1-3 WLWZE-N1-4 WLWZE-N1-5 WLWZE-N4-1 WLWZE-N4-2 WLWZE-N4-3 WLWZE-N4-4 WLWZE-N4-5
      SiO2 68.93 70.19 70.36 70.13 70.42 74.82 74.29 74.61 74.03 74.92
      TiO2 0.39 0.36 0.37 0.34 0.36 0.14 0.17 0.15 0.14 0.11
      Al2O3 14.19 13.62 13.21 13.76 13.09 12.66 12.46 12.71 13.03 12.83
      TFe2O3 3.81 3.66 3.83 3.62 3.74 1.45 1.85 1.76 1.86 1.34
      MnO 0.13 0.12 0.12 0.10 0.12 0.06 0.07 0.09 0.07 0.06
      MgO 1.26 1.20 1.28 1.14 1.17 0.24 0.23 0.20 0.25 0.21
      CaO 2.82 2.53 2.51 2.35 2.21 1.14 0.45 1.02 1.02 1.03
      Na2O 2.77 2.64 2.48 2.64 2.27 2.41 1.86 2.38 2.59 2.41
      K2O 4.42 4.48 4.36 4.54 5.16 5.79 7.54 5.90 5.82 6.01
      P2O5 0.12 0.12 0.12 0.11 0.11 0.04 0.10 0.04 0.05 0.04
      LOI 0.77 0.80 0.84 0.79 0.94 0.57 0.31 0.45 0.46 0.43
      Total 99.60 99.71 99.47 99.51 99.57 99.31 99.32 99.32 99.32 99.39
      ALK 7.19 7.12 6.83 7.18 7.42 8.19 9.40 8.29 8.41 8.42
      Na2O/K2O 0.63 0.59 0.57 0.58 0.44 0.42 0.25 0.40 0.44 0.40
      Mg# 24.67 20.00 18.27 20.80 23.43 39.54 39.32 39.77 38.33 38.15
      La 48.6 26.9 49.3 59.8 38.1 59.1 17.7 51.7 51.4 37.6
      Ce 93.8 54.0 95.9 110 69.7 113 33.2 98.3 115 73.1
      Pr 11.5 6.82 11.7 11.9 7.80 12.5 3.82 10.9 13.4 9.14
      Nd 40.6 23.8 41.6 45.5 30.6 48.3 15.0 41.7 47.9 33.8
      Sm 7.62 5.58 7.85 8.35 6.38 8.72 3.06 7.55 7.98 6.16
      Eu 0.987 1.02 1.05 1.22 1.23 0.784 0.698 0.845 0.835 0.603
      Gd 7.11 5.46 7.35 8.48 6.61 7.63 2.93 6.82 7.34 5.03
      Tb 1.11 0.930 1.20 1.03 0.896 0.675 0.363 0.634 0.818 0.566
      Dy 5.84 5.51 6.19 5.55 5.18 2.39 1.95 2.47 3.03 2.12
      Ho 1.24 1.13 1.33 1.04 0.988 0.330 0.346 0.368 0.518 0.350
      Er 3.29 3.07 3.55 3.03 2.94 0.86 1.00 1.04 1.47 0.992
      Tm 0.498 0 0.467 0 0.532 0 0.420 0 0.414 0 0.083 9 0.132 0 0.120 0 0.164 0 0.109 0
      Yb 3.14 2.99 3.46 2.67 2.66 0.539 0.879 0.798 1.13 0.826
      Lu 0.470 0.432 0.518 0.370 0.375 0.075 0.121 0.120 0.163 0.117
      Y 29.7 26.5 31.1 28.1 27.6 7.82 9.05 9.26 11.7 7.88
      ΣREE 226 138 232 260 174 263 90.2 233 262 178
      LREE 203 118 207 237 157 242 73.4 211 236 160
      HREE 22.7 20.0 24.1 22.6 20.1 12.6 7.71 12.4 14.6 10.1
      LREE/HREE 8.95 5.91 8.60 10.5 7.66 19.3 9.52 17.1 16.1 15.9
      (La/Yb)N 11.1 6.46 10.2 16.1 10.3 73.8 13.6 43.7 30.8 30.7
      (Gd/Lu)N 1.88 1.57 1.77 2.85 2.19 12.7 3.00 7.09 5.61 5.34
      Rb/Sr 0.853 0.897 1.02 0.887 1.52 2.12 2.26 2.22 2.01 1.85
      Ba/Nb 34.9 38.9 37.6 49.6 45.3 38.3 41.2 36.1 33.1 57.5
      La/Nb 3.01 1.73 3.12 3.92 2.55 7.98 1.96 6.42 6.43 8.61
      Th/La 0.944 1.13 0.982 0.641 0.662 0.563 0.512 0.571 0.771 0.758
      Nb/Ta 14.0 13.0 14.8 14.4 15.7 20.5 22.6 22.9 16.0 16.3
      δEu 0.403 0.558 0.417 0.438 0.574 0.287 0.703 0.353 0.328 0.321
      V 44.9 41.7 45.2 61.2 60.1 13.7 15.5 15.3 5.80 5.48
      Co 6.88 6.32 6.46 7.32 5.83 1.50 1.74 2.25 1.28 1.39
      Ni 7.98 8.29 8.11 7.48 6.43 1.95 1.84 4.06 2.08 3.69
      Cu 6.03 5.95 6.81 4.53 4.39 3.21 6.11 7.04 4.30 3.30
      Zn 194 197 198 181 106 12.4 13.2 11.7 14.1 11.0
      Ga 15.8 13.7 15.0 17.0 16.0 16.3 13.5 17.5 14.9 13.6
      Rb 198 194 217 264 306 204 228 225 195 181
      Sr 232 216 213 299 201 96.0 101 101 97.1 97.6
      Y 29.7 26.5 31.1 28.1 27.6 7.82 9.05 9.26 11.7 7.88
      Zr 76.5 76.0 66.1 72.9 48.1 81.6 74.5 97.4 69.2 81.5
      Nb 16.7 15.5 15.8 15.2 14.9 7.40 9.00 8.06 8.00 4.36
      Cs 13.6 14.0 18.1 16.8 21.9 4.69 3.79 4.96 6.27 4.98
      Ba 564 605 593 756 677 284 371 291 265 251
      Lu 0.470 0.432 0.518 0.370 0.375 0.075 0.121 0.120 0.163 0.117
      Hf 2.52 2.62 2.27 2.32 1.49 2.33 2.09 2.74 2.12 2.55
      Ta 1.15 1.19 1.07 1.06 0.948 0.361 0.398 0.352 0.501 0.267
      Th 45.8 30.3 48.4 38.3 25.2 33.3 9.05 29.5 39.6 28.5
      U 4.03 3.00 4.44 4.19 3.99 2.81 1.61 2.88 3.10 2.50
      下载: 导出CSV

      表  3  乌兰乌珠尔花岗岩锆石Hf同位素分析结果

      Table  3.   Zircon Hf isotopic compositions of Wulanwuzhuer granites

      样品 t(Ma) 176Yb/177Hf 176Lu/177Hf εHf(0) εHf(t) TDM1 TDM2 fLu/Hf
      WLWZE-N4-1 423 0.051 910 0.001 932 0.000 077 -8.82 -0.05 0.70 1 058 1 411 -0.94
      WLWZE-N4-2 423 0.052 300 0.001 988 0.000 079 -9.76 -1.01 0.66 1 098 1 471 -0.94
      WLWZE-N4-3 423 0.026 188 0.000 929 0.000 003 -9.86 -0.81 0.46 1 071 1 459 -0.97
      WLWZE-N4-4 423 0.027 585 0.001 006 0.000 049 -7.64 1.39 0.72 985 1 320 -0.97
      WLWZE-N4-8 423 0.024 066 0.000 874 0.000 017 -11.25 -2.19 0.52 1 125 1 546 -0.97
      WLWZE-N4-11 423 0.041 139 0.001 681 0.000 018 -9.09 -0.25 0.54 1 061 1 423 -0.95
      WLWZE-N4-12 423 0.038 887 0.001 360 0.000 024 -8.44 0.49 0.56 1 026 1 377 -0.96
      WLWZE-N4-13 423 0.033 894 0.001 223 0.000 005 -9.01 -0.04 0.51 1 045 1 410 -0.96
      WLWZE-N4-16 423 0.028 747 0.001 053 0.000 012 -9.76 -0.75 0.51 1 071 1 455 -0.97
      WLWZE-N4-18 423 0.034 242 0.001 215 0.000 015 -10.66 -1.69 0.58 1 111 1 515 -0.96
      WLWZE-N4-23 423 0.040 920 0.001 712 0.000 013 -10.52 -1.70 0.54 1 121 1 515 -0.95
      WLWZE-N4-24 423 0.022 720 0.000 799 0.000 023 -7.96 1.12 0.61 992 1 337 -0.98
      下载: 导出CSV
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