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    维西地区中三叠统上兰组物源分析及构造背景判断

    王启宇 牟传龙 贺娟 闫国川 凌亚军 孙小勇

    王启宇, 牟传龙, 贺娟, 闫国川, 凌亚军, 孙小勇, 2018. 维西地区中三叠统上兰组物源分析及构造背景判断. 地球科学, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307
    引用本文: 王启宇, 牟传龙, 贺娟, 闫国川, 凌亚军, 孙小勇, 2018. 维西地区中三叠统上兰组物源分析及构造背景判断. 地球科学, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307
    Wang Qiyu, Mou Chuanlong, He Juan, Yan Guochuan, Ling Yajun, Sun Xiaoyong, 2018. Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area. Earth Science, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307
    Citation: Wang Qiyu, Mou Chuanlong, He Juan, Yan Guochuan, Ling Yajun, Sun Xiaoyong, 2018. Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area. Earth Science, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307

    维西地区中三叠统上兰组物源分析及构造背景判断

    doi: 10.3799/dqkx.2018.307
    基金项目: 

    中国地质调查局项目 DD20160016

    详细信息
      作者简介:

      王启宇(1983-), 男, 工程师, 在职博士, 主要从事沉积盆地分析研究

      通讯作者:

      牟传龙

    • 中图分类号: P597

    Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area

    • 摘要: 前人对于金沙江构造带内三叠纪碎屑岩形成和演化的研究甚少,影响了对金沙江洋盆演化历史的整体认识.维西地区上兰组为砂板岩夹灰岩沉积,与原岩图解结果一致.变质砂岩碎屑锆石U-Pb年龄分布于426~603 Ma、713~980 Ma、1 000~1 600 Ma和1 600~2 500 Ma四个年龄段,年龄信息主要记录了来自扬子陆块及其周缘老基底、同泛非期及加里东期的物质来源;∑REE含量略高于上地壳值且具明显的轻重稀土分异特征,(La/Yb)N=5.23~12.33,具有轻微的δEu异常.碎屑组分特征及判别图解显示其物源主要来自于碰撞造山带及少量火山弧造山带,源岩性质属于再循环的古老沉积物及长英质火山岩类,构造环境为大陆岛弧及活动大陆边缘.以上研究表明上兰组形成于碰撞挤压坳陷构造背景,结合区域构造演化综合判断其为一种弧后前陆盆地构造环境.

       

    • 图  1  滇西维西地区地质简图

      Ⅰ.雀儿山-稻城火山岩浆弧;Ⅱ.甘孜-理塘结合带;Ⅲ.中咱-香格里拉地块;Ⅳ.金沙江-哀牢山结合带;Ⅴ.江达-维西火山岩浆弧;Ⅵ.昌都-兰坪-普洱地块;Ⅶ.保山-镇康地块;Ⅷ.类乌齐-左贡变质地块;Ⅸ.冈底斯-腾冲火山岩浆弧;Ⅹ.印度陆块;Ⅺ.察隅-盈江火山岩浆弧;Ⅻ.开心岭-竹卡火山岩浆弧

      Fig.  1.  The geological sketch in Weixi area of western Yunnan

      图  2  上兰组岩石学显微镜下特征

      a.变长石石英砂岩,粒状变晶结构(+20x);b.绢云变质砂岩,变余细粒砂状结构(+20x);c.绢云变质粉细砂岩,变余细粒砂状结构(+20x);d.绢云变质长石石英砂岩,变余砂状结构(+20x);e.变质细粒岩屑砂岩,变余细粒砂状结构(+20x);f.绢云变质砂岩,变余砂状结构(+20x);g.千枚状绢云石英千枚岩,鳞片粒状变晶结构(+20x);h.千枚状绢云砂质板岩,变余细粒砂状结构(+20x);i.砂质绢云板岩(+20x).图例见表 1

      Fig.  2.  The characteristics of petrographic microscope of Shanglan Formation

      图  3  维西地区上兰组变碎屑岩原岩类型分类图解

      底图据Allègre and Minster(1978)Herron(1988)

      Fig.  3.  Classification on clastic sedimentary rocks of Shanglan Formation

      图  4  维西地区上兰组碎屑锆石CL图像

      Fig.  4.  Cathodoluminescence (CL) images of detrital zircons from sandstones of Shanglan Formation in Weixi area

      图  5  维西地区上兰组碎屑锆石U-Pb年龄谐和图(a、b)及直方分布图(c、d)

      Fig.  5.  Concordia diagrams (a, b) and histograms (c, d) of detrital zircons from sandstones of Shanglan Formation in Weixi area

      图  6  上兰组变砂岩源区构造背景图解

      底图据Dickinson(1979)

      Fig.  6.  Discrimination diagrams for tectonic setting for variable sandstones of Shanglan Formation

      图  7  上兰组化学风化和分选作用分析图解

      图a据Nesbitt and Young (1982);图b据Taylor and McLennan (1985);图c据Camiré et al. (1993);图d据McLennan (1993)

      Fig.  7.  Analysis diagrams of chemical weathering and sorting of Shanglan Formation

      图  8  上兰组碎屑岩源区判别图解

      Floyd and Leveridge(1987)Roser and Korsch(1988)

      Fig.  8.  Discrimination diagrams for the provenance of clastic sedimentary rocks of Shanglan Formation

      图  9  上兰组变碎屑岩主量元素构造环境判别图

      Bhatia(1985).A.大洋岛弧;B.大陆岛弧;C.活动大陆边缘;D.被动大陆边缘

      Fig.  9.  Major elements discrimination diagrams for clastic sedimentary rocks of Shanglan Formation

      图  10  上兰组变碎屑岩微量元素构造环境判别图

      Bhatia(1985).A.大洋岛弧;B.大陆岛弧;C.活动大陆边缘;D.被动大陆边缘

      Fig.  10.  Trace elements discrimination diagrams for clastic sedimentary rocks of Shanglan Formation

      表  1  上兰组16件变砂岩的碎屑成分(%)

      Table  1.   The detrital component statistics (%) of 16 variable sandstone of Shanglan Formation

      样品号 Q F L Qm F Lt Qm P K Lm Lv Ls Lvf Lvmi Lvl C/Q P/F Lv/Lt
      PM06′-1-b2 52 40 8 50 40 10 62.5 7.5 30 5 1 94 6 2 92 0.04 0.19 0.10
      PM06′-4-b1 63.7 8 28.3 60 8 32 68 7.4 24.6 5 10 85 22 30 48 0.06 0.93 0.31
      PM06′-5-b1 68 20 12 55 20 25 69 6.2 24.8 10 15 75 38 20 42 0.19 0.31 0.60
      PM06′-7-b1 42 35 23 30 35 35 49 30.2 20.8 10 20 70 40 10 50 0.29 0.86 0.57
      PM06′-7-b2 58 28 14 50 28 22 66 6.8 27.2 8 20 72 41 6 53 0.14 0.24 0.91
      PM06′-15-b1 57 18 25 52 18 30 65 16.5 18.5 8 15 77 10 10 80 0.09 0.92 0.50
      PM06′-17-b1 70 25 5 65 25 10 75 20 5 2 8 90 5 5 90 0.07 0.80 0.80
      PM06′-17-b2 91 5.7 3.3 88 5.7 6.3 94 4.8 1.2 5 2 93 10 10 80 0.03 0.84 0.32
      PM06′-19-b1 82 5 13 78 5 17 90 4 6 5 10 85 20 5 75 0.05 0.80 0.59
      PM06′-20-b1 72.5 2 25.5 68 2 30 92 1.5 6.5 10 21 69 20 30 50 0.06 0.75 0.70
      PM06′-20-b2 69 3 28 65 3 32 90 1.2 8.8 5 5 90 70 5 25 0.06 0.40 0.16
      PM06′-22-b1 71 6 23 65 6 29 88 3.1 8.9 3 7 90 96 2 2 0.08 0.52 0.24
      PM06′-24-b1 68 20 12 60 20 20 76 15.8 8.2 2 10 88 20 15 65 0.12 0.79 0.50
      PM06′-25-b1 65 26 9 60 26 14 70 21 9 3 5 92 30 5 65 0.08 0.81 0.36
      PM06′-27-b1 65 24 11 60 24 16 71 18 11 5 8 87 12 10 78 0.08 0.75 0.50
      PM06′-28-b1 62 24 14 56 24 20 69 20 11 5 10 85 50 12 38 0.10 0.83 0.50
      注:C/Q、P/F和Lv/Lt为比值.Q.单晶石英+多晶石英;Qm.单晶石英;F.长石;L.岩屑(不含多晶石英);Lt.岩屑(含多晶石英);P.斜长石;K.钾长石;Lm.变质岩屑;Lv.火山岩屑;Ls.沉积岩屑;Lvf.具霏细结构的火山岩屑;Lvmi.具微晶结构火山岩屑;Lvl.具板状结构的火山岩屑;C.多晶石英.
      下载: 导出CSV

      表  2  维西地区上兰组主量(%)、微量(10-6)和稀土元素(10-6)分析结果

      Table  2.   Major elements (%), trace elements (10-6) and rare earth elements (10-6) results from clastic sedimentary rocks of Shanglan Formation in Weixi area

      样品号 PM06′-1-H2 PM06′-2-H1 PM06′-4-H1 PM06′-4-H2 PM06′-5-H1 PM06′-7-H1 PM06′-8-H1 PM06′-9-H1 PM06′-10-H1 PM06′-12-H2 PM06′-15-H1 PM06′-20-H1 PM06′-26-H2 PM06′-28-H1 PM06′-29-H1 PM06′-30-H2
      SiO2 57.21 64.14 56.18 90.66 70.14 64.09 64.53 68.45 65.92 53.38 60.34 66.53 67.54 68.99 69.33 45.24
      TiO2 0.88 0.68 0.86 0.23 0.57 0.71 0.72 0.62 0.65 1.43 0.69 0.65 0.76 0.68 0.64 2.19
      Al2O3 20.21 16.44 20.95 2.86 14.48 16.95 17.09 14.76 15.93 14.31 18.09 14.70 13.59 14.79 14.89 16.75
      Fe2O3T 5.82 5.76 5.95 0.92 4.57 5.51 5.52 5.47 5.60 10.86 7.29 5.29 3.97 5.02 5.54 8.58
      MnO 0.04 0.03 0.03 0.08 0.02 0.03 0.04 0.03 0.04 0.20 0.04 0.09 0.05 0.10 0.03 0.15
      MgO 2.81 2.70 2.53 0.70 1.96 2.53 2.77 2.01 2.22 3.87 2.35 2.02 1.14 1.93 0.65 4.68
      CaO 0.57 0.70 0.67 2.63 0.26 0.27 0.24 0.30 0.40 8.01 0.37 2.36 2.15 0.60 0.22 9.59
      Na2O 0.86 0.50 0.24 0.11 0.33 0.56 0.48 1.47 0.48 2.69 0.29 1.89 1.93 1.44 0.08 3.69
      K2O 7.52 5.49 8.29 0.14 3.88 5.04 4.98 3.10 4.84 1.03 5.93 2.86 4.58 3.22 3.64 0.98
      P2O5 0.13 0.14 0.14 0.12 0.13 0.16 0.14 0.15 0.13 0.24 0.12 0.12 0.17 0.12 0.14 0.54
      LOI 3.15 2.77 3.38 0.76 3.00 3.16 3.10 2.93 2.94 3.12 3.46 2.72 3.30 3.08 3.97 7.26
      Total 99.19 99.33 99.22 99.20 99.34 99.00 99.60 99.30 99.12 99.13 98.96 99.22 99.17 99.96 99.11 99.64
      Sc 15.9 13.5 17.7 2.3 10.6 14.8 14.6 13.2 15.7 33.9 16.6 15.8 11.9 16.1 14.2 31.7
      Cr 95.4 77.1 113.0 13.4 58.3 86.9 84.4 68.9 76.8 32.5 69.7 48.4 31.9 54.8 78.8 151.3
      Co 10.6 11.5 10.9 2.2 7.9 11.7 11.0 11.9 13.0 28.2 12.6 13.4 10.0 9.9 12.3 27.1
      Ni 31.3 33.2 40.5 5.4 27.4 39.1 35.4 32.9 45.4 6.4 45.6 30.3 16.3 29.1 32.4 77.7
      Ga 28.2 23.7 29.8 3.16 19.3 25.6 24.5 19.8 23.2 18.9 24.6 17.6 18.7 19.6 20.8 16.9
      Rb 309 219 336 6 154 202 182 141 214 38 275 93 212 103 181 34
      Sr 77.0 57.4 85.9 162 21.9 47.3 27.8 58.4 61.2 244 57.7 116 61.4 31.2 47.7 402.8
      Y 23.1 28.0 27.1 32.8 19.4 15.7 17.5 17.2 31.1 26.8 30.5 25.9 43.3 27.9 32.1 39.3
      Zr 317 206 212 663 204 270 240 164 133 122 168 158 274 163 158 241
      Nb 20.3 16.5 20.9 4.98 12.4 18.0 17.4 14.1 14.5 9.19 15.6 10.9 14.4 10.4 14.9 73.6
      Cs 5.21 5.64 13.20 0.34 2.44 3.22 3.78 3.98 6.03 1.69 8.92 8.61 5.47 5.32 7.70 3.53
      Ba 1026 655 1092 27 432 763 655 476 862 325 835 751 673 386 567 276
      La 53.3 45.9 56.7 20.6 27.4 18.6 26.5 24.7 41.9 19.6 51.3 24.1 48.5 29.4 39.8 39.2
      Ce 93.0 87.5 87.0 29.2 46.5 36.4 68.0 57.1 85.6 40.2 90.3 50.9 94.8 60.9 77.0 74.0
      Pr 12.0 10.1 11.8 4.73 5.92 4.26 6.25 5.70 8.99 4.69 11.3 5.81 10.8 7.14 8.87 8.82
      Nd 41.1 36.4 41.6 18.8 21.8 15.6 22.4 20.5 33.0 18.7 41.2 22.5 40.6 27.3 32.2 34.7
      Sm 6.66 6.69 6.99 4.74 4.07 2.98 4.23 3.92 6.31 4.24 7.88 4.70 8.45 5.82 6.14 7.07
      Eu 1.33 1.14 1.29 0.98 0.73 0.55 0.65 0.64 1.04 1.28 1.49 1.01 1.39 1.17 1.24 2.08
      Gd 4.50 5.19 5.33 4.43 3.13 2.42 3.12 3.07 5.10 4.26 6.32 4.12 7.63 4.98 5.32 6.80
      Tb 0.75 0.85 0.82 0.78 0.55 0.45 0.54 0.52 0.85 0.72 0.95 0.70 1.23 0.82 0.91 1.14
      Dy 4.24 4.80 4.70 4.80 3.26 2.92 3.22 3.14 5.12 4.49 5.53 4.36 7.37 4.96 5.44 7.04
      Ho 0.81 0.93 0.90 0.96 0.66 0.59 0.66 0.63 1.01 0.90 1.07 0.89 1.46 0.98 1.07 1.41
      Er 2.46 2.77 2.67 2.81 2.00 1.83 2.03 1.97 3.07 2.70 3.17 2.85 4.24 2.94 3.20 4.16
      Tm 0.38 0.39 0.38 0.41 0.30 0.30 0.32 0.30 0.45 0.40 0.44 0.44 0.61 0.45 0.46 0.59
      Yb 2.54 2.58 2.51 2.72 2.08 1.95 2.13 2.05 2.94 2.68 2.98 3.05 3.97 2.93 3.07 3.90
      Lu 0.40 0.37 0.40 0.40 0.31 0.32 0.34 0.33 0.44 0.41 0.44 0.47 0.58 0.46 0.44 0.58
      Hf 8.46 5.46 5.70 16.4 5.38 7.02 6.24 4.44 3.61 3.19 4.77 4.43 7.34 4.53 4.46 5.45
      Ta 1.57 1.25 1.54 0.39 0.91 1.31 1.24 1.08 1.13 0.63 1.22 0.85 1.18 0.79 1.17 4.03
      Pb 31.6 10.6 21.0 100 11.9 8.06 7.09 9.03 11.0 7.17 30.1 12.6 16.5 3.26 5.41 3.40
      Th 25.2 18.7 24.4 9.91 14.4 20.6 21.3 17.7 18.0 6.38 20.1 10.8 25.4 10.6 18.2 5.99
      U 3.57 3.27 3.96 2.31 2.40 2.96 3.00 2.80 4.10 1.62 4.19 2.49 4.91 2.28 3.17 1.10
      下载: 导出CSV

      表  3  维西地区上兰组变细砂岩碎屑锆石的U-Pb同位素数据

      Table  3.   U-Pb isotopic data for detrital zircon from clastic sedimentary rocks of Shanglan Formation in Weixi area

      样品 元素含量(10-6) 同位素比值 年龄(Ma) 谐和度(%)
      Pb Th U 207Pb/206Pb 1 σ 207Pb/235U 1 σ 206Pb/238U 1 σ 207Pb/206Pb 1 σ 207Pb/235U 1 σ 206Pb/238U 1 σ
      1 1 874 742 2.53 0.066 4 0.001 6 1.446 1 0.034 9 0.157 2 0.001 3 820 51.8 908 14.5 941 7.4 96
      2 11 319 3 022 3.75 0.058 1 0.001 3 0.736 1 0.016 3 0.091 3 0.000 7 600 50.0 560 9.6 563 4.0 99
      3 1 861 1 688 1.10 0.159 8 0.002 7 10.141 8 0.165 9 0.457 7 0.003 4 2 453 29.2 2 448 15.2 2 429 15.3 99
      4 774 1 347 0.57 0.071 9 0.001 6 1.696 0 0.034 8 0.170 5 0.001 4 983 44.4 1 007 13.1 1 015 7.8 99
      5 845 730 1.16 0.159 1 0.003 0 10.349 9 0.199 5 0.469 3 0.004 6 2 446 31.5 2 467 17.9 2 480 20.4 99
      6 718 948 0.76 0.078 5 0.001 9 2.270 0 0.054 1 0.208 7 0.001 9 1 161 48.2 1 203 16.8 1 222 10.0 98
      7 164 299 0.55 0.074 5 0.002 7 1.936 5 0.070 2 0.188 0 0.002 1 1 055 69.4 1 094 24.3 1 111 11.2 98
      8 761 664 1.15 0.090 0 0.002 2 3.208 9 0.075 4 0.257 2 0.002 3 1 428 41.7 1 459 18.2 1 475 11.7 98
      9 287 165 1.74 0.160 6 0.004 3 10.571 4 0.267 3 0.476 6 0.005 2 2 462 45.4 2 486 23.5 2 512 22.9 98
      10 8 430 1 266 6.66 0.059 8 0.001 8 0.813 4 0.024 5 0.098 0 0.000 8 594 66.7 604 13.7 603 4.9 99
      11 719 926 0.78 0.103 9 0.002 2 4.428 7 0.097 7 0.307 0 0.002 8 1 695 72.4 1 718 18.3 1 726 13.8 99
      12 250 345 0.73 0.118 2 0.002 8 6.546 3 0.151 1 0.399 5 0.003 4 1 931 42.4 2 052 20.4 2 167 15.5 94
      13 697 326 2.14 0.058 5 0.002 6 0.718 2 0.033 0 0.088 8 0.001 0 546 93.5 550 19.5 549 6.2 99
      14 343 199 1.72 0.063 8 0.002 5 1.557 7 0.058 3 0.178 4 0.002 7 744 83.3 954 23.1 1 058 15.0 89
      15 525 776 0.68 0.053 7 0.001 7 0.573 6 0.017 7 0.077 5 0.000 8 367 75.0 460 11.4 481 4.7 95
      16 580 268 2.16 0.072 7 0.002 9 1.706 7 0.062 8 0.171 4 0.002 2 1 006 82.6 1 011 23.6 1 020 11.9 99
      17 697 533 1.31 0.149 3 0.003 0 9.220 3 0.179 2 0.445 3 0.003 6 2 338 33.2 2 360 17.9 2 374 16.2 99
      18 1 134 1 059 1.07 0.064 7 0.001 7 1.262 7 0.033 6 0.140 8 0.001 3 765 55.6 829 15.1 849 7.5 97
      19 1 243 1 341 0.93 0.072 7 0.001 7 1.727 5 0.040 1 0.171 3 0.001 7 1 006 46.6 1 019 14.9 1 019 9.4 99
      20 848 572 1.48 0.076 3 0.002 1 1.960 2 0.052 0 0.185 8 0.002 2 1 106 58.3 1 102 17.8 1 099 11.9 99
      21 597 241 2.47 0.064 6 0.002 6 1.208 2 0.047 3 0.136 4 0.001 8 761 85.9 804 21.8 824 10.4 97
      22 781 2 140 0.36 0.376 1 0.006 1 45.402 6 0.843 9 0.867 2 0.008 0 3 816 24.6 3 896 18.7 4 025 27.6 96
      23 345 348 0.99 0.484 0 0.008 2 70.329 4 1.165 9 1.047 3 0.008 2 4 193 25.2 4 333 16.9 4 619 26.1 93
      24 433 1 306 0.33 0.056 6 0.001 7 0.586 4 0.017 5 0.074 7 0.000 8 476 66.7 469 11.2 465 4.9 99
      25 849 2 777 0.31 0.150 0 0.002 8 6.838 1 0.125 8 0.328 1 0.002 7 2 347 31.5 2 091 16.4 1 829 13.3 86
      26 494 506 0.98 0.068 9 0.002 3 1.274 4 0.041 5 0.133 7 0.001 5 894 63.9 834 18.5 809 8.3 96
      27 1 145 1 351 0.85 0.057 0 0.001 8 0.601 7 0.019 2 0.076 1 0.000 9 500 73.1 478 12.1 473 5.4 98
      28 886 2 390 0.37 0.061 9 0.001 5 1.152 9 0.027 9 0.134 5 0.001 5 733 51.8 779 13.2 813 8.6 95
      29 369 1 068 0.35 0.078 5 0.001 9 2.074 5 0.047 7 0.190 5 0.001 7 1 159 41.7 1 140 15.8 1 124 9.1 98
      30 4 395 3 328 1.32 0.072 4 0.001 4 1.721 8 0.034 3 0.171 2 0.001 4 996 40.0 1 017 12.8 1 019 7.6 99
      31 1 440 647 2.23 0.073 1 0.001 9 1.765 4 0.045 9 0.174 5 0.001 7 1 017 86.1 1 033 16.9 1 037 9.6 99
      32 539 512 1.05 0.068 6 0.002 1 1.475 9 0.045 0 0.155 5 0.001 6 887 64.8 921 18.5 932 9.1 98
      33 1 394 2 337 0.60 0.073 9 0.001 6 1.967 8 0.041 3 0.191 9 0.001 5 1 039 44.4 1 105 14.2 1 132 8.2 97
      34 1 943 652 2.98 0.064 7 0.002 1 1.221 4 0.041 1 0.136 1 0.001 4 765 68.5 810 18.8 823 8.0 98
      35 1 599 1 580 1.01 0.059 9 0.001 6 0.754 2 0.019 7 0.090 9 0.000 9 611 57.4 571 11.4 561 5.5 98
      36 996 294 3.39 0.067 9 0.003 5 0.815 2 0.041 6 0.087 4 0.001 2 865 107 605 23.3 540 6.9 88
      37 1 112 1 157 0.96 0.161 2 0.003 6 10.418 0 0.233 4 0.466 5 0.004 4 2 468 36.9 2 473 20.8 2 468 19.4 99
      38 534 996 0.54 0.192 6 0.004 0 14.448 2 0.301 7 0.541 9 0.004 9 2 765 33.6 2 780 19.9 2 791 20.6 99
      39 976 761 1.28 0.074 0 0.002 0 1.734 7 0.046 9 0.169 9 0.001 5 1 043 55.6 1 022 17.4 1 012 8.4 99
      40 1 131 905 1.25 0.071 5 0.001 8 1.821 0 0.044 6 0.185 6 0.002 0 972 56.5 1 053 16.1 1 098 10.9 95
      41 312 679 0.46 0.079 7 0.002 1 2.192 9 0.057 3 0.199 5 0.001 8 1 191 52.9 1 179 18.2 1 173 9.8 99
      42 1 409 2 034 0.69 0.055 8 0.001 4 0.536 5 0.013 2 0.069 8 0.000 6 443 53.7 436 8.7 435 3.8 99
      43 686 526 1.30 0.168 2 0.003 4 10.954 5 0.223 5 0.472 4 0.004 2 2 540 33.3 2 519 19.1 2 494 18.3 98
      44 251 701 0.36 0.094 8 0.002 2 3.485 1 0.089 6 0.266 1 0.002 6 1 524 43.4 1 524 20.3 1 521 13.1 99
      45 841 1 116 0.75 0.102 4 0.002 4 3.910 0 0.096 3 0.276 8 0.002 6 1 669 48.3 1 616 19.9 1 575 13.1 97
      46 684 1 159 0.59 0.064 1 0.001 9 1.052 3 0.030 8 0.119 3 0.001 2 746 61.1 730 15.3 727 7.1 99
      47 1 068 1 477 0.72 0.077 9 0.001 9 1.991 6 0.049 1 0.185 8 0.001 8 1 143 48.9 1 113 16.7 1 098 9.6 98
      48 1 164 1 478 0.79 0.181 9 0.003 4 11.185 0 0.215 4 0.445 3 0.003 4 2 670 31.6 2 539 18.0 2 374 15.4 93
      49 2 599 1 683 1.54 0.058 3 0.001 5 0.721 2 0.019 9 0.089 6 0.001 0 539 57.4 551 11.8 553 5.8 99
      50 988 1 501 0.66 0.365 1 0.006 1 39.841 9 0.693 7 0.788 3 0.006 0 3 771 26.3 3 767 17.4 3 747 21.6 99
      51 394 386 1.02 0.075 3 0.002 6 1.888 2 0.061 6 0.182 2 0.001 8 1 077 70.4 1 077 21.7 1 079 9.7 99
      52 1 511 1 745 0.87 0.059 2 0.001 9 0.595 6 0.018 6 0.072 7 0.000 6 572 66.7 474 11.9 452 3.7 95
      53 346 1 319 0.26 0.071 3 0.001 6 1.632 1 0.037 4 0.165 1 0.001 4 966 47.4 983 14.4 985 7.6 99
      54 893 609 1.47 0.065 1 0.002 3 1.134 9 0.039 3 0.126 3 0.001 4 776 75.1 770 18.7 767 8.0 99
      55 1 379 793 1.74 0.074 7 0.002 1 1.751 9 0.046 9 0.169 4 0.001 8 1 061 56.6 1 028 17.3 1 009 9.8 98
      56 3 325 3 520 0.94 0.089 8 0.002 0 1.521 9 0.035 1 0.121 9 0.001 0 1 421 43.7 939 14.1 741 5.9 76
      57 604 1 016 0.59 0.209 7 0.004 1 15.359 8 0.293 3 0.527 7 0.004 0 2 903 31.8 2 838 18.3 2 732 16.8 96
      58 871 656 1.33 0.102 2 0.002 7 3.868 0 0.101 4 0.273 2 0.003 0 1 665 54.5 1 607 21.2 1 557 15.0 96
      59 1 004 954 1.05 0.081 3 0.002 1 2.142 8 0.053 8 0.190 5 0.001 9 1 228 49.7 1 163 17.4 1 124 10.3 96
      60 841 984 0.85 0.061 1 0.002 1 0.625 6 0.020 9 0.074 2 0.000 8 643 76.8 493 13.0 461 4.7 93
      61 1 482 1 151 1.29 0.112 4 0.002 7 4.603 2 0.109 3 0.295 4 0.002 7 1 839 43.982 5 1 750 19.8 1 668 13.3 95
      62 495 532 0.93 0.079 1 0.002 6 1.673 7 0.053 7 0.153 6 0.001 7 1 174 66.202 5 999 20.4 921 9.6 91
      63 1 178 736 1.60 0.117 4 0.003 2 5.014 1 0.136 8 0.308 0 0.002 8 1 918 16.2 1 822 23.1 1 731 13.6 94
      64 374 456 0.82 0.058 1 0.002 7 0.584 3 0.026 8 0.073 3 0.001 0 532 99.1 467 17.2 456 5.8 97
      65 905 792 1.14 0.176 4 0.004 4 11.074 8 0.278 4 0.452 6 0.004 1 2 620 41.8 2 529 23.5 2 407 18.4 95
      66 444 543 0.82 0.100 1 0.002 7 3.306 6 0.090 5 0.237 8 0.002 2 1 628 49.8 1 483 21.4 1 375 11.3 92
      67 2 768 1 066 2.60 0.177 8 0.003 8 11.858 6 0.257 1 0.480 4 0.003 9 2 632 34.7 2 593 20.4 2 529 17.1 97
      68 1 102 145 7.63 0.182 9 0.004 9 12.274 3 0.341 4 0.485 0 0.006 2 2 679 44.4 2 626 26.2 2 549 27.1 97
      69 476 567 0.84 0.088 1 0.003 0 2.148 1 0.085 0 0.173 8 0.002 3 1 385 66.7 1 164 27.4 1 033 12.6 88
      70 1 554 1 339 1.16 0.100 8 0.002 0 3.646 8 0.072 2 0.260 3 0.002 0 1 640 36.3 1 560 15.8 1 492 10.4 95
      71 2 588 1 278 2.03 0.063 9 0.002 1 0.774 0 0.024 6 0.087 4 0.000 8 739 36.1 5 82 14.1 540 4.6 92
      72 940 980 0.96 0.095 0 0.002 0 3.325 8 0.067 8 0.252 3 0.002 0 1 528 40.3 1 487 15.9 1 450 10.6 97
      73 816 25 32.24 0.190 2 0.025 2 2.763 5 0.244 5 0.125 5 0.005 1 2 744 220 1 346 66.0 762 29.0 44
      74 1 353 1 177 1.15 0.060 0 0.001 7 0.974 6 0.028 3 0.117 0 0.001 0 606 61.1 691 14.6 713 5.8 96
      75 674 701 0.96 0.085 3 0.003 1 2.413 2 0.094 7 0.203 5 0.001 8 1 322 70.4 1 247 28.2 1 194 9.9 95
      76 3 919 1 303 3.01 0.072 1 0.001 5 1.694 1 0.036 1 0.169 6 0.001 7 991 43.1 1 006 13.6 1 010 9.5 99
      77 428 516 0.83 0.108 9 0.002 4 4.885 6 0.106 8 0.323 9 0.003 2 1 781 39.0 1 800 18.5 1 809 15.5 99
      78 1 750 907 1.93 0.058 8 0.002 0 0.758 3 0.025 7 0.093 3 0.001 0 567 75.9 573 14.9 575 5.8 99
      79 866 479 1.81 0.078 5 0.002 3 2.173 9 0.064 3 0.200 2 0.002 3 1 158 59.3 1 173 20.6 1 177 12.3 99
      80 1 661 1 110 1.50 0.080 3 0.001 8 2.221 6 0.050 7 0.199 7 0.001 9 1 203 40.6 1 188 16.0 1 174 10.1 98
      81 878 917 0.96 0.165 2 0.003 4 11.986 4 0.235 9 0.523 0 0.004 5 2 510 34.3 2 603 18.5 2 712 19.1 95
      82 2 377 1 128 2.11 0.164 4 0.003 2 10.836 7 0.206 8 0.475 2 0.003 9 2 502 65.9 2 509 17.8 2 506 16.9 99
      83 532 1 344 0.40 0.068 9 0.001 6 1.615 9 0.036 6 0.169 2 0.001 4 898 48.2 976 14.2 1 008 7.7 96
      84 268 241 1.11 0.268 1 0.004 9 24.731 0 0.453 6 0.666 1 0.006 2 3 295 29.0 3 298 18.0 3 291 24.0 99
      85 1 008 1 665 0.61 0.107 2 0.001 9 4.988 6 0.111 3 0.334 6 0.004 0 1 754 31.9 1 817 18.9 1 861 19.5 97
      86 788 1 046 0.75 0.069 7 0.001 8 1.773 7 0.044 6 0.183 9 0.001 4 920 52.6 1 036 16.4 1 088 7.8 95
      87 847 1 030 0.82 0.076 3 0.001 7 1.877 5 0.042 3 0.177 7 0.001 5 1 102 44.4 1 073 15.0 1 055 8.4 98
      88 405 1 513 0.27 0.058 3 0.001 6 0.565 4 0.015 0 0.070 3 0.000 7 539 59.3 455 9.7 438 3.9 96
      89 783 1 064 0.74 0.072 1 0.001 7 1.790 5 0.042 5 0.179 5 0.001 5 991 48.2 1 042 15.5 1 064 8.1 97
      90 171 552 0.31 0.071 7 0.002 2 1.803 3 0.055 4 0.182 3 0.001 9 977 58.3 1 047 20.1 1 079 10.2 96
      91 502 1 208 0.42 0.159 0 0.003 0 9.002 0 0.176 2 0.408 9 0.003 6 2 456 31.8 2 338 18.0 2 210 16.4 94
      92 1 331 761 1.75 0.072 1 0.001 9 1.701 4 0.044 9 0.170 9 0.001 7 989 55.1 1 009 16.9 1 017 9.3 99
      93 689 880 0.78 0.085 1 0.001 8 2.624 2 0.058 1 0.222 3 0.002 0 1 320 42.4 1 307 16.3 1 294 10.6 98
      94 648 1 180 0.55 0.054 9 0.001 8 0.541 5 0.016 7 0.071 4 0.000 7 409 67.6 439 11.0 445 4.2 98
      95 2 472 2 599 0.95 0.075 9 0.001 4 1.926 3 0.036 8 0.182 6 0.001 7 1 094 36.0 1 090 12.8 1 081 9.1 99
      96 1 135 698 1.63 0.075 0 0.002 6 1.849 8 0.059 3 0.178 9 0.001 8 1 133 73.1 1 063 21.2 1 061 9.8 99
      97 3 296 1 754 1.88 0.100 6 0.002 0 4.307 7 0.084 0 0.307 7 0.002 1 1 635 37.0 1 695 16.1 1 730 10.4 97
      98 1 076 1 841 0.58 0.075 7 0.001 8 1.892 7 0.044 1 0.179 4 0.001 5 1 088 52.3 1 079 15.5 1 064 8.4 98
      99 419 1 253 0.33 0.081 6 0.002 3 2.074 4 0.056 0 0.182 6 0.001 6 1 235 49.8 1 140 18.5 1 081 8.5 94
      100 396 103 3.85 0.082 2 0.004 8 1.934 6 0.105 6 0.173 8 0.003 0 1 251 114 1 093 36.6 1 033 16.2 94
      101 305 760 0.40 0.059 3 0.002 3 0.563 1 0.021 5 0.068 3 0.000 7 576 80.5 454 14.0 426 4.4 93
      102 1 103 1 876 0.59 0.072 2 0.001 7 1.445 0 0.033 5 0.143 7 0.001 4 992 46.3 908 13.9 866 7.9 95
      103 968 322 3.00 0.072 8 0.003 0 1.583 5 0.065 9 0.156 7 0.001 9 1 009 89.8 964 25.9 938 10.6 97
      104 830 876 0.95 0.107 9 0.002 2 4.582 5 0.091 9 0.305 5 0.002 5 1 765 41.7 1 746 16.7 1 718 12.5 98
      105 379 648 0.58 0.163 3 0.003 1 10.382 8 0.193 6 0.457 2 0.003 6 2 490 31.8 2 470 17.4 2 427 16.0 98
      106 501 129 3.88 0.077 7 0.004 7 0.958 1 0.051 5 0.093 4 0.001 9 1 139 120 682 26.7 576 11.1 83
      107 489 473 1.03 0.058 5 0.003 1 0.561 0 0.029 0 0.069 7 0.000 9 546 115 452 18.8 435 5.4 96
      108 804 466 1.73 0.161 9 0.003 6 10.156 1 0.224 1 0.452 1 0.004 1 2 476 37 2 449 20.5 2 405 18.4 98
      下载: 导出CSV

      表  4  上兰组碎屑岩与不同构造背景砂岩的稀土元素特征值比较

      Table  4.   Comparison of the detrital rocks of Shanglan Formation with the rare earth element characteristics of sandstones under various tectonic settings

      构造背景 源区类型 La(10-6) Ce(10-6) ∑REE La/Yb (La/Yb)N ∑LREE/∑HREE δEu
      大洋岛弧 未切割的岩浆弧 8±1.7 19±3.7 58±10 4.2±1.3 2.8±0.9 3.8±0.9 1.04±0.11
      大陆岛弧 切割的岩浆弧 27±4.5 59±8.2 146±20 11±3.6 7.5±2.5 7.7±1.7 0.79±0.13
      安第斯型大陆边缘 上隆的基底 37 78 186 12.5 8.5 9.1 0.60
      被动大陆边缘 克拉通内部高地 39 85 210 15.9 10.8 8.5 0.56
      本次研究 35.08 67.58 164.14 12.77 9.16 8.45 0.65
      注:据Bhatia(1985)修改.
      下载: 导出CSV

      表  5  上兰组碎屑岩与不同构造背景砂岩的微量元素特征值比较

      Table  5.   Comparison of the detrital rocks of Shanglan Formation with the trace element characteristics of sandstones under various tectonic settings

      构造背景 大洋岛弧 大陆岛弧 活动大陆边缘 被动大陆边缘 本次研究
      Th(10-6) 2.27±0.7 11.11±1.1 18.8±3.0 16.7±3.5 16.73
      U(10-6) 1.09±0.21 2.53±0.24 3.90±0.5 3.2±0.8 3.008
      Hf(10-6) 2.1±0.6 6.3±2.0 6.8 10.1 6.056
      Rb/Sr 0.05±0.05 0.65±0.33 0.89±0.24 1.19±0.4 0.763
      Th/U 2.1±0.78 4.6±0.45 4.8±0.38 5.6±0.7 5.05
      La/Y 0.48±0.12 1.02±0.07 1.33±0.09 1.31±0.26 1.332
      La/Sc 0.55±0.22 1.82±0.3 4.55±0.8 6.25±1.35 2.778
      Th/Sc 0.15±0.08 0.85±0.13 2.59±0.5 3.06±0.8 1.363
      注:据Bhatia and Crook(1986)修改.
      下载: 导出CSV
    • Allègre, C.J., Minster, J.F., 1978.Quantitative Models of Trace Element Behavior in Magmatic Processes.Earth and Planetary Science Letters, 38(1):1-25.https://doi.org/10.1016/0012-821x(78)90123-1 doi: 10.1016/0012-821X(78)90123-1
      Barth, T., 1999.Similarities and Differences in Hydrous Pyrolysis of Biomass and Source Rocks.Organic Geochemistry, 30(12):1495-1507.https://doi.org/10.1016/s0146-6380(99)00121-7 doi: 10.1016/S0146-6380(99)00121-7
      Bhatia, M.R., 1985.Composition and Classification of Paleozoic Flysch Mudrocks of Eastern Australia:Implications in Provenance and Tectonic Setting Interpretation.Sedimentary Geology, 41(2-4):249-268.https://doi.org/10.1016/0037-0738(84)90065-4 http://cn.bing.com/academic/profile?id=7a125321b32d3e52dd5b2612bea3c974&encoded=0&v=paper_preview&mkt=zh-cn
      Bhatia, M.R., Crook, K.A.W., 1986.Trace Element Characteristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins.Contributions to Mineralogy and Petrology, 92(2):181-193.https://doi.org/10.1007/bf00375292 doi: 10.1007/BF00375292
      Camiré, G.E., Laflèche, M.R., Ludden, J.N., 1993.Archaean Metasedimentary Rocks from the Northwestern Pontiac Subprovince of the Canadian Shield:Chemical Characterization, Weathering and Modelling of the Source Areas.Precambrian Research, 62(3):285-305.https://doi.org/10.1016/0301-9268(93)90026-x doi: 10.1016/0301-9268(93)90026-X
      Cawood, P.A., Hawkesworth, C.J., Dhuime, B., 2012.Detrital Zircon Record and Tectonic Setting.Geology, 40(10):875-878.https://doi.org/10.1130/g32945.1 doi: 10.1130/G32945.1
      Cawood, P.A., Nemchin, A.A., 2000.Provenance Record of a Rift Basin:U-Pb Ages of Detrital Zircons from the Perth Basin, Western Australia.Sedimentary Geology, 134(3-4):209-234.https://doi.org/10.1016/s0037-0738(00)00044-0 doi: 10.1016/S0037-0738(00)00044-0
      Chen, Y.L., Luo, Z.H., ,Liu, C., et al., 2001.New Recognition of Kangding-Mianning Metamorphic Complexes from Sichuan, Western Yangtze Craton:Evidence from Nd Isotopic Composition.Earth Science, 26(3):279-285 (in Chinese with English abstract).
      Dickinson, W.R., 1982.Compositions of Sandstones in Circum-Pacific Subduction Complexes and Fore-Arc Basins.AAPG Bulletin, 66:121-137.https://doi.org/10.1306/03b59a4e-16d1-11d7-8645000102c1865d http://cn.bing.com/academic/profile?id=f643b6fd08c7c6506c519288fc195e53&encoded=0&v=paper_preview&mkt=zh-cn
      Dickinson, W.R., Harbaugh, D.W., Saller, A.H., et al., 1983.Detrital Modes of Upper Paleozoic Sandstones Derived from Antler Orogen in Nevada; Implications for Nature of Antler Orogeny.American Journal of Science, 283(6):481-509. https://doi.org/10.2475/ajs.283.6.481
      Dickinson, W.R., Suczek, C.A., 1979.Plate Tectonics and Sandstone Compositions.AAPG Bulletin, 63(12):2164-2182.
      Du, L.L., Guo, J.H., Geng, Y.S., et a1., 2013.Age and Tectonic Setting of the Yanbian Group in the Southwestern Yangtze Block:Constraints from Clastic Sedimentary Rocks.Acta Petrologica Sinica, 29(2):641-672 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302021
      Fedo, C.M., Nesbitt, H.W., Young, G.M., 1995.Unraveling the Effects of Potassium Metasomatism in Sedimentary Rocks and Paleosols, with Implications for Paleoweathering Conditions and Provenance.Geology, 23(10):921-924.https://doi.org/10.1130/0091-7613(1995)023<0921:uteopm>2.3.co;2 doi: 10.1130/0091-7613(1995)023<0921:UTEOPM>2.3.CO;2
      Fedo, C.M., Sircombe, K.N., Rainbird, R.H., 2003.Detrital Zircon Analysis of the Sedimentary Record.Reviews in Mineralogy and Geochemistry, 53(1):277-303. https://doi.org/10.2113/0530277
      Floyd, P.A., Leveridge, B.E., 1987.Tectonic Environment of the Devonian Gramscatho Basin, South Cornwall:Framework Mode and Geochemical Evidence from Turbiditic Sandstones.Journal of the Geological Society, 144(4):531-542. https://doi.org/10.1144/gsjgs.144.4.0531
      Gao, R., Xiao, L., He, Q., et al., 2010.Geochronology, Geochemistry and Petrogenesis of Granites in Weixi-Deqin, West Yunnan.Earth Science, 35(2):186-200 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2010.019 http://d.old.wanfangdata.com.cn/Periodical/dqkx201002003
      Geng, Y.S., Yang, C.H., Wang, X.H., et al., 2007.Age of Crystalline Basement in Western Margin of Yangtze Terrane.Geological Journal of China Universities, 13(3):429-441 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200703012
      Greentree, M.R., Li, Z.X., Li, X.H., et al., 2006.Late Mesoproterozoic to Earliest Neoproterozoic Basin Record of the Sibao Orogenesis in Western South China and Relationship to the Assembly of Rodinia.Precambrian Research, 151(1-2):79-100. https://doi.org/10.1016/j.precamres.2006.08.002
      Herron, M.M., 1988.Geochemical Classification of Terrigenous Sands and Shales from Core or Log Data.Journal of Sedimentary Research, 58(5):820-829.https://doi.org/10.1306/212f8e77-2b24-11d7-8648000102c1865d http://d.old.wanfangdata.com.cn/Periodical/njlgdxxb201705016
      Hu, Q.H., Jin, J.C., Zhao, Y., et al., 2014.Geological Characteristics of Triassic Pantiange Volcanic Arc Region in Weixi of Yunnan and Its Significance for Prospecting.Mineral Resources and Geology, 28(5):568-577 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcydz201405008
      Jian, P., Liu, D.Y., Sun, X.M., 2003.SHRIMP Dating of Baimaxueshan and Ludian Granitoid Batholiths, Northwestern Yunnan Province, and Its Geological Implications.Acta Geoscientia Sinica, 24(4):337-342 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200304008
      Lehmann, B., Zhao, X.F., Zhou, M.F., et al., 2013.Mid-Silurian Back-Arc Spreading at the Northeastern Margin of Gondwana:The Dapingzhang Dacite-Hosted Massive Sulfide Deposit, Lancangjiang Zone, Southwestern Yunnan, China.Gondwana Research, 24(2):648-663. https://doi.org/10.1016/j.gr.2012.12.018
      Liu, B.B., Peng, T.P., Fan, W.M., et al., 2017.Geochronology of Detrital Zircon from the Upper Silurian-Lower Devonian Sedimentary Rocks at Both Sides of the Ailaoshan Tectonic Zone:Provenance and Geological Significance.Geotectonica et Metallogenia, 41(4):734-752 (in Chinese with English abstract).
      Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004
      Lu, S.N, 1996.Position and Role of Precambrian Geology in Earth Sciences.Geological Review, 42(4):311-316 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000002758
      Ludwig, K.R., 2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley.
      Mao, X.C., Wang, L.Q., Li, B., et al., 2012.Discovery of the Late Silurian Volcanic Rocks in the Dazhonghe Area, Yunxian-Jinggu Volcanic Arc Belt, Western Yunnan, China and Its Geological Significance.Acta Petrologica Sinica, 28(5):1517-1528 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201205014
      McLennan, S.M., Hemming, S., McDaniel, D.K., et al., 1993.Geochemical Approaches to Sedimentation, Provenance, and Tectonics.Special Paper of the Geological Society of America, 284:21-40.https://doi.org/10.1130/spe284-p21 doi: 10.1130/SPE284
      McLennan, S.M., Hemming, S.R., Taylor, S.R., et al., 1995.Early Proterozoic Crustal Evolution:Geochemical and Nd-Pb Isotopic Evidence from Metasedimentary Rocks, Southwestern North America.Geochimica et Cosmochimica Acta, 59(6):1153-1177.https://doi.org/10.1016/0016-7037(95)00032-u doi: 10.1016/0016-7037(95)00032-U
      Mo, X.X., Lu, F.X., Shen, S.Y., 1993.Volcanism and Mineralization in Sanjiang Tethys.Geological Publishing House, Beijing (in Chinese).
      Morton, A.C., Claoué-Long, J.C., Berge, C., 1996.SHRIMP Constraints on Sediment Provenance and Transport History in the Mesozoic Statfjord Formation, North Sea.Journal of the Geological Society, 153(6):915-929. https://doi.org/10.1144/gsjgs.153.6.0915
      Mou, C.L, Wang, L.Q., 2000.The Evolution of the Volcano-Sedimentary Basin during the Late Triassic in Deqia, Yunnan.Journal of Mineralogy and Petrology, 20(3):23-28 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200003005
      Mou, C.L, Yu, Q., 2002.The Age of Volcanic Rock of the Pantiange Formation in the Lanping Basin, Yunnan Province.Journal of Stratigraphy, 26(4):289-292 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200204009
      Nesbitt, H.W., Young, G.M., 1982.Early Proterozoic Climates and Plate Motions Inferred from Major Element Chemistry of Lutites.Nature, 299(5885):715-717. https://doi.org/10.1038/299715a0
      Qiu, Y.M., Gao, S., McNaughton, N.J., et al., 2000.First Evidence of >3.2 Ga Continental Crust in the Yangtze Craton of South China and Its Implications for Archean Crustal Evolution and Phanerozoic Tectonics.Geology, 28(1):11-14.https://doi.org/10.1130/0091-7613(2000)028<0011:feogcc>2.3.co;2 http://cdmd.cnki.com.cn/Article/CDMD-10213-1014081416.htm
      Rainbird, R.H., Hearnan, L.M., Young, G., 1992.Sampling Laurentia:Detrital Zircon Geochronology Offers Evidence for an Extensive Neoproterozoic River System Originating from the Grenville Orogen.Geology, 20(4):351-354.https://doi.org/10.1130/0091-7613(1992)020<0351:sldzgo>2.3.co;2 doi: 10.1130/0091-7613(1992)020<0351:SLDZGO>2.3.CO;2
      Roser, B.P., Korsch, R.J., 1988.Provenance Signatures of Sandstone-Mudstone Suites Determined Using Discriminant Function Analysis of Major-Element Data.Chemical Geology, 67(1-2):119-139. https://doi.org/10.1016/0009-2541(88)90010-1
      Ru, S.S., Li, F., Wu, J., et al., 2012.Geochemistry and Chronology of Granodiorite Porphyry in the Dapingzhang Cu Polymetallic Deposit.Acta Petrologica et Mineralogica, 31(4):531-540 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201204006
      Sun, Z.M., Yin, F.G., Guan, J.L., et al., 2009.SHRIMP U-Pb Dating and Its Stratigraphic Significance of Tuff Zircons from Heishan Formation of Kunyang Group, Dongchuan Area, Yunnan Province, China.Geological Bulletin of China, 28(7):896-900 (in Chinese with English abstract).
      Taylor, S.R., McLennan, S.M., 1985.The Continental Crust:Its Composition and Evolution.Blackwell, Oxford.
      Taylor, S.R., McLennan, S.M., 1995.The Geochemical Evolution of the Continental Crust.Reviews of Geophysics, 33(2):241-262.https://doi.org/10.1029/95rg00262 doi: 10.1029/95RG00262
      Wang, B.D., Wang, L.Q., Qiangba, Z.X., et al., 2011.Early Triassic Collision of Northern Lancangjiang Suture:Geochronological, Geochemical and Hf Isotope Evidences from the Granitic Gneiss in Leiwuqi Area, East Tibet.Acta Petrologica Sinica, 27(9):2752-2762 (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201109023
      Wang, B.D., Wang, L.Q., Chen, J.L., et al., 2014.Triassic Three-Stage Collision in the Paleo-Tethys:Constraints from Magmatism in the Jiangda-Deqen-Weixi Continental Margin Arc, SW China.Gondwana Research, 26(2):475-491. https://doi.org/10.1016/j.gr.2013.07.023
      Wang, D.B., Tang, Y., Liao, S.Y., et al., 2013.Zircon U-Pb Dating and Its Geological Implications of the Metamorphic Rock Series in Ailaoshan Ranges, Western Yunnan.Acta Petrologica Sinica, 29(4):1261-1278 (in Chinese with English abstract). https://www.researchgate.net/publication/286015761_Zircon_U-Pb_dating_and_its_geological_implications_of_the_metamorphic_rock_series_in_Ailao_Shan_Ranges_western_Yunnan
      Wang, L.Q., Li, D.M., Guan, S.P., et al., 2001.The Evolution of the Luchun-Hongponiuchang Superimposed Rifting Basin, Deqin County, Yunnan Province.Journal of Mineralogy and Petrology, 21(3):81-89 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200103013
      Wang, L.Q., Li, D.M., Guan, S.P., et al., 2002a.The Rb-Sr Age Determinations of the "Bimodal" Volcanic Rocks in the Luchun-Hongponiuchang Superimposed Rift Basin, Deqen, Yunnan.Sedimentary Geology and Tethyan Geology, 22(1):65-71 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl200201012
      Wang, L.Q., Hou, Z.Q., Mo, X.X., et al., 2002b.The Post-Collisional Crustal Extension Setting:An Important Mineralizing Environment of Volcanic Massive Sulfide Deposits in Jinsha Orogenic Belt.Acta Geologica Sinica, 76(4):541-556 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=1eec64f5e2e06b216d1d8c48e5dc8b16&encoded=0&v=paper_preview&mkt=zh-cn
      Wang, L.Q., Pan, G.T., Li, D.M., et al., 1999.The Spatio-Temporal Framework and Geological Evolution of the Jinshajiang Arc-Basin Systems.Acta Geologica Sinica, 73(3):206-218 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900084696
      Wang, L.Q., Pan, G.T., Li, D.M., et al., 2000.The Evolution and Mineralization of the Jomda-Weixi Continental Marginal Volcanic Arc, Southwestern China.Sedimentary Geology and Tethyan Geology, 20(2):1-17 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl200002001
      Xie, J., Zhu, B.Q., Chang, X.Y., 2005.Geochemical Characteristics of Basic-intermediate Volcanic Rocks from Jinshajiang Belt in Northwestern Yunnan, China.Bulletin of Mineralogy Petrology and Geochemistry, 24(4):299-308 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb200504004
      Xu X.S., O'Reilly, S.Y., Griffin, W.L., et al., 2005.Relict Proterozoic Basement in the Nanling Mountains (SE China) and Its Tectonothermal Overprinting.Tectonics, 24(2):TC2003.https://doi.org/10.1029/2004tc001652 doi: 10.1029-2004TC001652/
      Xu, X.S., O'Reilly, S.Y., Griffin, W.L., et al., 2007.The Crust of Cathaysia:Age, Assembly and Reworking of Two Terranes.Precambrian Research, 158(1-2):51-78. https://doi.org/10.1016/j.precamres.2007.04.010
      Yan, D.P., Zhou, M.F., Wang, C.Y., et al., 2006.Structural and Geochronological Constraints on the Tectonic Evolution of the Dulong-Song Chay Tectonic Dome in Yunnan Province, SW China.Journal of Asian Earth Sciences, 28(4-6):332-353. https://doi.org/10.1016/j.jseaes.2005.10.011
      Yao, H.Z., Xu, A.W., Tang, C.Y., et al., 2006.Geological Characteristics of the Early-Middle Triassic Volcano-Sedimentary Basin in the Eastern Tibet.Geology and Mineral Resources of South China, 22(3):41-47 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hndzykc200603007
      Yu, J.H., O'Reilly, S.Y., Wang, L.J., et al., 2008.Where Was South China in the Rodinia Supercontinent? Evidence From U-Pb Geochronology and Hf Isotopes of Detrital Zircons.Precambrian Research, 164(1-2):1-15. https://doi.org/10.1016/j.precamres.2008.03.002
      Zhang, C.H., Gao, L.Z., Shi, X.Y., et al., 2014.SHRIMP Age of the Volcanic Rock from the Fanjingshan Group and Its Chronostratigraphic Significances.Earth Science Frontiers, 21(2):139-143 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201402011
      Zhang, Q., Zhou, D.J., Zhao, D.S., et al., 1996.Wilson Cycle of the Paleo-Tethyan Orogenic Belt in Western Yunnan:Record of Magmatism and Discussion on Mantle Processes.Acta Petrologica Sinica, 12(1):17-28 (in Chinese with English abstract).
      Zhou, X.Y., Yu, J.H., Wang, L.J., et al., 2015.Compositions and Formation of the Basement Metamorphic Rocks in Yunkai Terrane, Western Guangdong Province, South China.Acta Petrologica Sinica, 31(3):855-882 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201503018
      Zhu, R.X., Li, X.H., Hou, X.G., et al., 2009.SIMS U-Pb Zircon Age of a Tuff Layer in the Meishucun Section, Yunnan, Southwest China:Constraint on the Age of the Precambrian-Cambrian Boundary.Science China Earth Sciences, 52(9):1385-1392. https://doi.org/10.1007/s11430-009-0152-6
      Zi, J.W., Cawood, P.A., Fan, W.M., et al., 2012.Triassic Collision in the Paleo-Tethys Ocean Constrained by Volcanic Activity in SW China.Lithos, 144-145:145-160. https://doi.org/10.1016/j.lithos.2012.04.020
      陈岳龙, 罗照华, 刘翠, 2001.对扬子克拉通西缘四川康定-冕宁变质基底的新认识——来自Nd同位素的证据.地球科学, 26(3):279-285. https://doi.org/10.3321/j.issn:1000-2383.2001.03.010
      杜利林, 郭敬辉, 耿元生, 等, 2013.扬子西南缘盐边群时代及构造环境:来自碎屑沉积岩的约束.岩石学报, 29(2):641-672. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302021
      胡清华, 金建才, 赵勇, 等, 2014.云南维西三叠纪攀天阁火山弧区域地质特征及找矿意义.矿产与地质, 28(5):568-577. doi: 10.3969/j.issn.1001-5663.2014.05.008
      耿元生, 杨崇辉, 王新社, 等, 2007.扬子地台西缘结晶基底的时代.高校地质学报, 13(3):429-441. doi: 10.3969/j.issn.1006-7493.2007.03.012
      简平, 刘敦一, 孙晓猛, 2003.滇西北白马雪山和鲁甸花岗岩基SHRIMP U-Pb年龄及其地质意义.地球学报, 24(4):337-342. doi: 10.3321/j.issn:1006-3021.2003.04.008
      高睿, 肖龙, 何琦, 等.2010.滇西维西-德钦一带花岗岩年代学、地球化学和岩石成因.地球科学, 35(2):186-200.https://doi.org/10.3799/dqkx.2010.019 http://earth-science.net/WebPage/Article.aspx?id=1943
      刘兵兵, 彭头平, 范蔚茗, 等, 2017.哀牢山构造带两侧上志留统-下泥盆统碎屑锆石年代学:物源及其构造意义.大地构造与成矿学, 41(4):734-752. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx201704010
      陆松年, 1996.前寒武纪地质学在当代地球科学中的地位与作用.地质论评, 42(4):311-316. doi: 10.3321/j.issn:0371-5736.1996.04.006
      毛晓长, 王立全, 李冰, 等, 2012.云县-景谷火山弧带大中河晚志留世火山岩的发现及其地质意义.岩石学报, 28(5):1517-1528. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201205014
      莫宣学, 路风香, 沈上越, 1993.三江特提斯火山作用与成矿.北京:地质出版社, 178-235.
      牟传龙, 王立全, 2000.云南德钦及邻区晚三叠世火山沉积盆地演化.矿物岩石, 20(3):23-28. doi: 10.3969/j.issn.1001-6872.2000.03.005
      牟传龙, 余谦, 2002.云南兰坪盆地攀天阁组火山岩的Rb-Sr年龄.地层学杂志, 26(4):289-292. doi: 10.3969/j.issn.0253-4959.2002.04.009
      汝珊珊, 李峰, 吴静, 等, 2012.云南大平掌铜多金属矿区花岗闪长斑岩地球化学特征及年代学研究.岩石矿物学杂志, 31(4):531-540. doi: 10.3969/j.issn.1000-6524.2012.04.006
      孙志明, 尹福光, 关俊雷等, 2009.云南东川地区昆阳群黑山组凝灰岩锆石SHRIMP U-Pb年龄及其地层学意义.地质通报, 28(7):896-900. doi: 10.3969/j.issn.1671-2552.2009.07.009
      王保弟, 王立全, 强巴扎西, 等, 2011.早三叠世北澜沧江结合带碰撞作用:类乌齐花岗质片麻岩年代学、地球化学及Hf同位素证据.岩石学报, 27(9):2752-2762. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201109023
      王冬兵, 唐渊, 廖世勇, 等, 2013. 滇西哀牢山变质岩系锆石U-Pb定年及其地质意义. 岩石学报, 29(4): 1261-1278.
      王立全, 潘桂棠, 李定谋, 等, 1999.金沙江弧-盆系时空结构及地史演化.地质学报, 73(3):206-218. doi: 10.3321/j.issn:0001-5717.1999.03.002
      王立全, 潘桂棠, 李定谋, 等, 2000.江达-维西陆缘火山弧的形成演化及成矿作用.沉积与特提斯地质, 20(2):1-17 doi: 10.3969/j.issn.1009-3850.2000.02.001
      王立全, 李定谋, 管士平, 等, 2001.云南德钦鲁春-红坡牛场上叠裂谷盆地演化.矿物岩石, 21(3):81-89. doi: 10.3969/j.issn.1001-6872.2001.03.013
      王立全, 李定谋, 管士平, 等, 2002a.云南德钦鲁春-红坡牛场上叠裂谷盆地"双峰式"火山岩的Rb-Sr年龄值.沉积与特提斯地质, 22(1):65-71. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl200201012
      王立全, 侯增谦, 莫宣学, 等, 2002b.金沙江造山带碰撞后地壳伸展背景——火山成因块状硫化物矿床的重要成矿环境.地质学报, 76(4):541-556. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200204011
      谢静, 朱炳泉, 常向阳, 2005.滇西北金沙江带中基性火山岩的地球化学特征.矿物岩石地球化学通报, 24(4):299-308. doi: 10.3969/j.issn.1007-2802.2005.04.004
      姚华舟, 徐安武, 汤朝阳, 等, 2006.西藏东部早-中三叠世火山——沉积盆地地质特征.华南地质与矿产, 22(3):41-47. doi: 10.3969/j.issn.1007-3701.2006.03.007
      张传恒, 高林志, 武振杰, 等, 2014.梵净山火山岩锆石SHRIMP年龄及其年代地层学意义.地学前缘, 21(2):139-143. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201402011
      张旗, 周德进, 赵大升, 等, 1996.滇西古特提斯造山带的威尔逊旋回:岩浆活动记录和深部过程讨论.岩石学报, 12(1):17-28. doi: 10.3321/j.issn:1000-0569.1996.01.002
      周雪瑶, 于津海, 王丽娟, 等, 2015.粤西云开地区基底变质岩的组成和形成.岩石学报, 31(3):855-882. http://d.old.wanfangdata.com.cn/Conference/8248277
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