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    南天山英买来花岗岩的地质、地球化学特征及其地质意义

    马乐天 张招崇 董书云 张舒 张东阳 黄河

    马乐天, 张招崇, 董书云, 张舒, 张东阳, 黄河, 2010. 南天山英买来花岗岩的地质、地球化学特征及其地质意义. 地球科学, 35(6): 908-920. doi: 10.3799/dqkx.2010.106
    引用本文: 马乐天, 张招崇, 董书云, 张舒, 张东阳, 黄河, 2010. 南天山英买来花岗岩的地质、地球化学特征及其地质意义. 地球科学, 35(6): 908-920. doi: 10.3799/dqkx.2010.106
    MA Le-tian, ZHANG Zhao-chong, DONG Shu-yun, ZHANG Shu, ZHANG Dong-yang, HUANG He, 2010. Geology and Geochemistry of the Yingmailai Granitic Intrusion in the Southern Tianshan and Its Implications. Earth Science, 35(6): 908-920. doi: 10.3799/dqkx.2010.106
    Citation: MA Le-tian, ZHANG Zhao-chong, DONG Shu-yun, ZHANG Shu, ZHANG Dong-yang, HUANG He, 2010. Geology and Geochemistry of the Yingmailai Granitic Intrusion in the Southern Tianshan and Its Implications. Earth Science, 35(6): 908-920. doi: 10.3799/dqkx.2010.106

    南天山英买来花岗岩的地质、地球化学特征及其地质意义

    doi: 10.3799/dqkx.2010.106
    基金项目: 

    国家科技支撑计划 2007BAB25B05

    "111计划" B07011

    详细信息
      作者简介:

      马乐天(1986-), 女, 学士, 地质学专业E-mail: mlt285772317@126.com

      通讯作者:

      张招崇, E-mail: zczhang@cugb.edu.cn

    • 中图分类号: P596

    Geology and Geochemistry of the Yingmailai Granitic Intrusion in the Southern Tianshan and Its Implications

    • 摘要: 新疆英买来岩体位于南天山中段, 其主体由黑云母钾长花岗岩组成, 局部有二云母钾长花岗岩, 形成于晚二叠世.岩体中有两种少量椭球状的包体, 一是暗色细粒包体, 二是浅色包体.花岗岩和包体的地球化学特征基本相似, 它们在主量元素特征上以高Si、富K、富碱, 贫Mg、Ca为特征, 微量元素特征上表现为富Rb、Ba、Th以及轻重稀土的高度分馏和Nb、Ta、Zr、Hf等的负异常.花岗岩和包体的Harker图解显示出一致的变化趋势, 表明它们是同源岩浆演化的产物.其A/CNK值为0.99~1.08, 显示出准铝-过铝的特点, 而稀土元素配分曲线则显示出强烈富集轻稀土和明显的负Eu异常.结合其高的(87Sr/86Sr)t值(0.71036~0.71585)和负的εNd(t)值(-1.67~-6.45), 推测岩浆起源于壳源含斜长石的角闪石质岩石脱水条件下的部分熔融(深度<50km), 其母岩浆在就位前发生了以黑云母和斜长石为主伴随有磁铁矿等副矿物的分离结晶作用.英买来花岗岩体的岩石类型以及地球化学特征表明其是介于A型和S型之间的一种过渡类型花岗岩类, 其形成时的构造环境为碰撞晚期或接近碰撞结束向后碰撞过渡阶段.

       

    • 图  1  新疆构造单元划分(a)和英买来岩体地质图(b)(据新疆地质矿产局第八地质大队2008年资料修改)

      Ⅲ.塔里木-卡拉库姆板块;Ⅲ1.塔里木微板块;Ⅲ11.东阿莱-哈尔克古生代复合沟弧带;Ⅲ12.艾尔宾晚古生代残斜盆地;Ⅲ13.阔克塔勒晚古生代陆缘盆地;Ⅲ14.虎拉山晚古生代裂陷槽;Ⅲ15.柯坪前陆盆地;Ⅲ16.库鲁克塔格陆缘地块;Ⅲ17.塔里木中央地块;1.第四系覆盖;2.阿克苏群片麻岩、浅粒岩、云母片岩;3.二叠纪中粗粒似斑状钾长花岗岩;4.二叠纪粗粒似斑状钾长花岗岩;5.二叠纪细粒花岗闪长岩;6.青白口纪片麻状粗粒二长花岗岩;7.辉绿岩脉;8.岩相界线;9.逆断层及产状;10.采样点

      Fig.  1.  Tectonic units of Xinjian (a) and geologic map of the Yingmailai intrusion (b)

      图  2  花岗岩中的细粒包体(包体和花岗岩有明显的界线)以及典型的岩相学特征

      a.粗粒黑云母钾长花岗岩中的暗色细粒包体,界线清晰(野外照片);b.粗粒黑云母钾长花岗岩中的浅色花岗质岩石包体(野外照片);c.暗色细粒包体中黑云母自形程度较高,而其他浅色矿物呈半自形或他形,显示出同结现象(正交偏光);d.中粗粒黑云母钾长花岗岩中的微斜长石斑晶(正交偏光);e.中粗粒黑云母钾长花岗岩的基质(正交偏光);f.粗粒二云母钾长花岗岩中的文象结构(正交偏光);g.粗粒二云母钾长花岗岩,自形程度较高的白云母分布在微斜长石中(正交偏光);h.粗粒二云母钾长花岗岩,黑云母自形程度高,白云母与其共生(正交偏光)

      Fig.  2.  Fine-granular xenolith in the granite (distinct boundary between granite and xenolith can be recognized) and typical petrographic features of the granite and xenolith

      图  3  英买来花岗岩和包体的Harker图解

      空心方框为花岗岩样品;实心方框为包体样品

      Fig.  3.  Harker diagram of the Yingmailai granites and xenoliths

      图  4  英买来花岗岩和包体的球粒陨石标准化曲线(球粒陨石标准化数据据Sun and McDonough, 1989)

      两条细虚线之间的区域代表前人测得的该地区钾长花岗岩稀土元素配分曲线范围,据姜常义等(1999);两条粗虚线之间的区域代表前人测得的南天山西段川乌鲁杂岩体稀土元素配分曲线范围,据黄河等(2010)

      Fig.  4.  Chindrite-normalized REE patterns of the Yingmailai granites and xenoliths

      图  5  英买来花岗岩和包体的洋脊花岗岩标准化曲线(标准化数据Pearce et al., 1984)

      Fig.  5.  ORG-normalized trace element patterns of the Yingmailai granites and xenoliths

      图  6  (87Sr/86Sr)t-εNd(t)

      图解其他地区的年龄数据据徐学义等(2005)

      Fig.  6.  (87Sr/86Sr)t versus εNd(t) diagram

      图  7  Nb-Y和Rb-(Y+Nb)图解(底图据Pearce et al., 1984)

      Fig.  7.  Diagrams of Nb versus Y and Rb versus Y+Nb

      表  1  英买来花岗岩体和包体的主量元素分析结果(%)

      Table  1.   Major element analyses of the Yingmailai granites and xenoliths

      样品 Q01 Q03 Q04 Q05 Q06 Q07 Q08 Q09 Qab01 Qab03 Qab05 Qabb
      SiO2 73.9 71.3 72.1 74.7 77.6 74.4 77 74.4 75.1 69.9 76.4 66.2
      TiO2 0.11 0.26 0.22 0.12 0.18 0.21 0.15 0.16 0.16 0.59 0.13 0.78
      Al2O3 13.6 13.91 13.62 13.3 11.25 12.75 11.86 12.51 12.56 13.5 11.91 14.12
      Fe2O3 1.33 3.27 2.67 1.22 1.88 2.22 1.67 1.64 1.58 5.81 1.63 8.23
      FeO 0.92 2.13 1.67 0.94 1.41 1.58 1.14 1.19 1.18 4.49 1.21 6.64
      MnO 0.03 0.06 0.05 0.02 0.03 0.03 0.02 0.02 0.02 0.08 0.03 0.11
      MgO 0.12 0.18 0.17 0.18 0.21 0.25 0.21 0.19 0.21 0.78 0.19 1.13
      CaO 0.84 1.33 1.09 0.75 0.69 0.96 0.81 0.85 0.73 1.88 0.45 2.04
      Na2O 3.39 3.39 3.15 2.96 2.6 2.97 2.74 2.91 2.78 3.73 2.42 4.04
      K2O 5.9 5.6 6.1 6.2 4.8 5.3 4.9 5.4 5.9 3 5.9 2.5
      P2O5 0.06 0.09 0.08 0.07 0.08 0.09 0.08 0.08 0.07 0.25 0.07 0.33
      LOI 0.68 0.49 0.41 0.5 0.38 0.56 0.64 0.54 0.47 0.91 0.5 0.86
      SUM 100 99.9 99.7 101.1 99.7 99.1 101.1 99.6 99.6 100.4 99.7 100.3
      A/KN 1.14 1.2 1.15 1.14 1.19 1.2 1.2 1.18 1.15 1.44 1.15 1.51
      A/CNK 1.011 0.99 0.988 1.024 1.048 1.028 1.048 1.028 1.024 1.057 1.067 1.082
      δ 2.774 2.845 2.956 2.672 1.587 2.197 1.733 2.172 2.333 1.671 2.061 1.841
      注:A/KN=Al2O3/(K2O+Na2O)(分子比);A/CNK=Al2O3/(Na2O+K2O+CaO)(分子比);δ=(K2O+Na2O)2/(SiO2-43).
      下载: 导出CSV

      表  2  英买来花岗岩体和包体的微量元素分析结果(10-6)

      Table  2.   Trace element analyses of the Yingmailai granites and xenoliths

      样品 Q01 Q03 Q04 Q05 Q06 Q07 Q08 Q09 Qab01 Qab03 Qab05 Qabb
      La 54.5 39.3 83.1 42.2 73.2 31.3 34.3 26.7 45 32.3 24.9 32.8
      Ce 102 78.3 157 90.4 153 64.3 75 59.4 96.9 69.7 55.7 72.1
      Pr 19.6 12.8 25.3 14.4 26.2 10.8 11.7 9.28 15.6 11.3 8.71 11.7
      Nd 38.1 32 54.6 32 57.1 25.1 26.6 21.3 38.1 26.3 19.7 28.8
      Sm 8.38 7.36 8.45 7.21 8.63 5.75 5.86 4.89 8.32 5.67 4.11 6.63
      Eu 3.17 1.96 1.88 0.465 0.408 0.475 0.303 0.224 0.422 0.362 0.205 0.361
      Gd 11.5 10.7 12 7.02 11.5 7.2 6.46 4.82 8.1 7.89 5.02 9.51
      Tb 1.62 1.59 1.55 1 1.51 1.1 0.841 0.622 1.12 1.23 0.801 1.61
      Dy 7.83 7.65 7.51 5.11 7.24 6.04 3.83 3 5.94 6.44 4.58 8.28
      Ho 1.36 1.34 1.15 0.958 1.25 1.14 0.641 0.532 1.11 1.07 0.943 1.45
      Er 3.15 3.08 2.97 2.39 3.06 2.9 1.48 1.32 2.81 2.53 2.59 3.26
      Tm 0.654 0.596 0.482 0.357 0.421 0.425 0.2 0.19 0.413 0.322 0.376 0.417
      Yb 3.15 3.1 2.99 2.08 2.39 2.4 1.07 1.08 2.39 1.59 1.98 2.02
      Lu 0.461 0.442 0.426 0.303 0.339 0.347 0.152 0.162 0.162 0.345 0.211 0.251
      Ba 734 783 762 244 268 315 180 138 219 137 150 145
      Cu 176 27.1 85.1 300 235 286 61.2 38.8 19.6 50.6 47.4 167
      Sr 49.2 67.2 66.3 33.9 29.5 54.1 25.4 41.8 30.4 29.8 16.8 28.9
      V 6.26 5.19 4.44 6.09 6.04 6.49 4.52 3.29 4.16 21 3.38 34.2
      Zn 91.8 86.6 88.1 77 63.6 372 548 260 67.3 121 48.2 219
      Co 0.487 0.811 0.62 0.674 0.965 1.98 1.19 1.27 0.8 3.45 0.545 6.21
      Ga 48.7 49.5 47.3 20.2 22 24.2 21.5 12.1 18.7 15.2 12.8 18.7
      Rb 101 154 158 162 151 158 107 87.4 152 173 132 222
      Th 22.4 25.9 29.9 29.9 67.5 53.1 34.3 23.7 35.2 31.2 16.2 24.8
      U 3.42 3.91 2.84 2.04 5.49 10 2.22 7.46 2.86 0.986 1.11 0.55
      Cr 17.3 30.3 14.6 14.6 11.5 24 19.5 21.5 12.6 25.7 10.5 13.4
      Ni 2.41 1.69 1.62 2.22 1.66 4.68 14.5 0.223 2.03 2.86 1.78 4.7
      Zr 3.34 11.2 13.8 4.67 3.05 6.7 2.58 3.75 2.98 7.16 0.63 3.33
      Nb 22.3 39.3 29.4 14.3 20.0 22.7 16.4 16.7 17.8 23.5 17.8 23.1
      Hf 0.911 1.84 2.33 1.07 0.366 1.02 0.367 0.486 0.319 0.927 0.098 0.256
      Ta 1.25 1.34 1.20 0.98 1.18 0.99 1.27 1.60 0.83 0.90 0.76 0.71
      W 5.92 2.92 2.53 2.47 2.02 38.4 3.69 33.3 7.84 5.29 2.16 3.23
      Y 35.9 58.9 55.8 21.4 28.4 25.6 14.4 12.3 24.7 23.6 22.6 31.4
      ∑REE 255.48 200.22 359.41 205.89 346.25 159.28 168.44 133.52 226.39 167.05 129.83 179.19
      LREE 225.75 171.72 330.33 186.68 318.54 137.73 153.76 121.79 204.34 145.63 113.33 152.39
      HREE 29.73 28.50 29.08 19.22 27.71 21.55 14.67 11.73 22.05 21.42 16.50 26.80
      LREE/HRE 7.59 6.03 11.36 9.71 11.50 6.39 10.48 10.39 9.27 6.80 6.87 5.69
      (La/Yb)n 9.56 7.65 15.92 12.89 19.50 8.01 21.32 15.84 25.84 8.73 11.40 12.41
      δEu 1.00 0.68 0.58 0.20 0.13 0.23 0.15 0.14 0.16 0.17 0.14 0.14
      δCe 1.79 1.48 1.54 1.51 1.60 1.54 1.48 1.48 1.48 1.51 1.48 1.48
      下载: 导出CSV

      表  3  英买来花岗岩体和包体的Sr和Nd同位素成分

      Table  3.   Sr and Nd isotopic compositions of the Yingmailai granites and xenoliths

      样品 Q01 Q03 Q04 Q05 Q06 Q07 Q08 Q09 Qab 01 Qab 03 Qab 05 Qabb
      Rb(10-6) 107.2 155.1 160.5 158.9 148.7 161.5 110.9 90.23 149.8 170.7 129.8 226.2
      Sr(10-6) 51.23 69.76 63.85 34.71 30.25 52.81 27.32 39.89 29.15 28.53 15.45 31.23
      87Rb/86Sr 6.055 6.781 7.062 14.13 15.14 8.632 12.39 6.139 14.94 17.12 23.18 22.71
      87Sr/86Sr 0.737603 0.740051 0.737133 0.764298 0.765357 0.743812 0.75803 0.735034 0.76403 0.772631 0.795005 0.793691
      (87Sr/86Sr)t 0.715850 0.715689 0.711762 0.713534 0.710964 0.7128 0.713517 0.712979 0.710356 0.711125 0.711728 0.712102
      Sm(10-6) 7.998 7.235 8.172 7.504 7.954 5.841 5.702 4.775 5.568 5.524 4.156 6.498
      Nd(10-6) 37.23 31.45 53.78 31.96 56.33 23.76 26.81 20.99 33.87 6.094 20.18 27.33
      147Sm/144Nd 0.1209 0.1201 0.1108 0.1112 0.1013 0.1204 0.1208 0.1195 0.1305 0.1328 0.1259 0.1231
      143Nd/144Nd 0.512205 0.512184 0.512217 0.512208 0.512186 0.512179 0.512195 0.512187 0.512441 0.512429 0.512398 0.512323
      (143Nd/144Nd)t 0.512001 0.511981 0.51203 0.51202 0.512015 0.511976 0.511991 0.511985 0.512221 0.512205 0.512185 0.512115
      εNd(t) -5.96 -6.34 -5.39 -5.58 -5.68 -6.45 -6.15 -6.26 -1.67 -1.98 -2.35 -3.73
      注:年龄校正采用t=258Ma;(143Nd/144Nd)CHUR=0.512638;(147Sm/144Nd)CHUR=0.1967;λSr=1.39×10-11/a;λSm=6.54×10-12/a.
      下载: 导出CSV

      表  4  英买来岩体和A型花岗岩特征比较

      Table  4.   Comparison of the Yingmailai intrusion with A type of granite

      英买来岩体 A型花岗岩 参考文献
      Na2O+K2O 7.5~9.3 7~11% Eby(1990)谭俊等(2008)
      CaO 0.7~1.3 <1.8%
      FeO*/MgO 5~12 8~80
      KN/A 0.83~0.88 >0.85 Whalen(1987)
      Zr+Nb+Ce+Y 92~256×10-6 >350×10-6
      稀土总量 134~359×10-6 平均219.03×10-6
      稀土配分形式 “V”字型,重稀土分馏明显 “V”字型,重稀土分馏不明显
      (Ga/Al)×10000 1.8~6.7 >2.5
      下载: 导出CSV
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