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新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄、成因演化及地质意义

宋鹏, 童英, 王涛, 黄河, 张建军, 黄伟

宋鹏, 童英, 王涛, 黄河, 张建军, 黄伟. 2018: 新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄、成因演化及地质意义. 地质通报, 37(5): 790-804.
引用本文: 宋鹏, 童英, 王涛, 黄河, 张建军, 黄伟. 2018: 新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄、成因演化及地质意义. 地质通报, 37(5): 790-804.
SONG Peng, TONG Ying, WANG Tao, HUANG He, ZHANG Jianjun, HUANG Wei. 2018: Zircon U-Pb ages, genetic evolution and geological significance of Carboniferous granites in the Harlik Mountain, East Tianshan, Xinjiang. Geological Bulletin of China, 37(5): 790-804.
Citation: SONG Peng, TONG Ying, WANG Tao, HUANG He, ZHANG Jianjun, HUANG Wei. 2018: Zircon U-Pb ages, genetic evolution and geological significance of Carboniferous granites in the Harlik Mountain, East Tianshan, Xinjiang. Geological Bulletin of China, 37(5): 790-804.

新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄、成因演化及地质意义

基金项目: 

国家自然科学基金-新疆联合基金重点支持项目《北疆及邻区深部新老地壳时空分布构架及其成矿制约》 U1403291

中国地质调查局项目《显生宙重大岩浆事件调查与岩浆岩试点填图》 DD20160123

《中国岩浆岩综合研究》 DD20160345

详细信息
    作者简介:

    宋鹏(1988-), 男, 在读博士生, 从事花岗岩与大地构造研究。E-mail:songpengyx@foxmail.com

    通讯作者:

    童英(1974-), 男, 博士, 研究员, 从事花岗岩地球动力学研究。E-mail:yingtong@cags.ac.cn

  • 中图分类号: P597;P534.45

Zircon U-Pb ages, genetic evolution and geological significance of Carboniferous granites in the Harlik Mountain, East Tianshan, Xinjiang

  • 摘要:

    新疆北部广泛发育的石炭纪—二叠纪花岗质岩石一直是中亚造山带西段研究的热点之一。新获得东天山哈尔里克地区小铺黑云母二长花岗岩和沁城南含角闪石二长花岗岩LA-ICP-MS锆石U-Pb年龄分别为316±4Ma和320±3Ma。地球化学特征显示,小铺岩体为弱过铝质高钾钙碱性I型花岗岩,沁城南岩体为准铝质高钾钙碱性A型花岗岩。小铺岩体的εHft)值为+8.0~+13.8,沁城南岩体则更高,达到+10.8~+16.7,对应的地壳模式年龄(TDMc)分别为822~450Ma和641~268Ma,反映源区为年轻地壳物质。结合区域同时代产出的基性岩,指示这些年轻物质很可能与新的幔源基性底侵岩浆有关,为北疆哈尔里克地区石炭纪后碰撞地壳垂向生长提供了新证据。此外,沁城南岩体具有A型特征花岗岩的出现,进一步揭示晚石炭世为碰撞-后碰撞的重要构造转换期。

    Abstract:

    Extensively developed granitoids in northern Xinjiang have constituted one of the hotspots in the study of granite in the western Central Asian Orogenic Belt. LA-ICP-MS zircon U-Pb analysis of the Xiaopu biotite monzogranite and Qinchengnan hornblende monzogranite in the Harlic area yielded crystallization ages of 316±4Ma and 320±3Ma. Their petrological and geochemical characteristics show that Xiaopu pluton belongs to high-K calc-alkaline and weakly peraluminous series of I-type granite, whereas the Qinchengnan pluton belongs to high-K calc-alkaline and metaluminous series with A-type granite characteristics. The Xiaopu pluton has positive zircon εHf (t) values of +8.0~+13.8, and the Qinchengnan pluton has higher εHf (t) values up to +10.8~+16.7, with corresponding Hf model ages (TDMc) of 822~450Ma and 641~268Ma, respectively. These isotopic compositions indicate that young crust served as the main source of the granite generation. Combined with coeval basic rocks with similar isotopic compositions in this region, it can be believed that these young granites might have been related to the new mantle-derived basic magma underplating and exhibited the post-collision vertical growth. Additionally, the Qinchengnan granites have A-type granite characteristics, thus providing a further evidence for the transition period of Late Carboniferous from collision to post-collision settings.

  • 致谢: 感谢中国地质科学院地质研究所贾孝新硕士和中国地质大学(北京)张义、王玮、许元全、刘鹏杰、陈林君硕士在数据测试中提供的帮助,以及评审专家对本文提出的宝贵修改意见。
  • 图  1   北疆及邻区地质简图(花岗岩图据参考文献;主要构造划分据参考文献[13-14])

    Figure  1.   Geological sketch map of North Xinjiang

    图  2   哈尔里克山地质图(据参考文献[16]修改)

    Figure  2.   Geological map of the Harlik Mountain

    图  3   小铺黑云母二长花岗岩(a)和沁城南含角闪石二长花岗岩(b)显微照片

    Qz—石英;Pl—斜长石;Kf—钾长石

    Figure  3.   Photomicrographs of granites from Xiaopu (a) and Qinchengnan (b)

    图  4   小铺黑云母二长花岗岩(T12716-1.2)和沁城南含角闪石二长花岗岩(T12716-8.4)锆石阴极发光(CL)图像

    (图中实线圆圈为年龄分析点位,虚线圆圈为Hf同位素分析点位)

    Figure  4.   Zircon CL images of Xiaopu and Qinchengnan granites

    图  5   小铺黑云二长花岗岩(a)和沁城南含角闪石二长花岗岩(b)锆石U-Pb年龄谐和图

    Figure  5.   Zircon U-Pb concordia diagrams of Xiaopu (a) and Qinchengnan (b) granites

    图  6   哈尔里克山花岗岩类SiO2-K2O(a)和A/CNK-A/NK图解(b)

    (a、b底图分别据参考文献[29][30],数据来源于参考文献[19]和本文)

    Figure  6.   SiO2 versus K2O (a) and A/CNK versus A/NK (b) diagrams for the granitoids in the Harlik Mountain

    图  7   小铺和沁城南花岗岩稀土元素球粒陨石标准化分布型式(a)和微量元素原始地幔标准化蛛网图(b)

    (球粒陨石和原始地幔标准化数据据参考文献[31],小铺东花岗岩数据据参考文献[21])

    Figure  7.   Chondrite-normalized REE patterns (a) and primitive-mantle normalized spidergrams (b) of Xiaopu and Qinchengnan granites

    图  8   小铺花岗岩和沁城南花岗岩A型花岗岩判别图解(底图据参考文献[35])

    I & S—I型和S型花岗岩分布区;FG—分异的I & S型花岗岩分布区;OGT—未分异的I、S & M型花岗岩分布区

    Figure  8.   Discrimination diagrams of A-type granite for Xiaopu and Qinchengnan granites

    图  9   小铺和沁城南花岗岩100(MgO+TFeO+TiO2)/SiO2-(Al2O3+CaO)/(TFeO+Na2O+K2O)图解

    (底图据参考文献[36])

    Figure  9.   100(MgO+TFeO+TiO2)/SiO2 versus (Al2O3+CaO)/(TFeO+Na2O+K2O) diagram of Xiaopu and Qinchengnan granites

    图  10   哈尔里克山地区花岗质岩石的εHf(t)随年龄变化图解(a)及Hf模式年龄TDMC频率分布直方图(b)

    (数据来源于参考文献[19, 23]和本文)

    Figure  10.   206Pb/238U age versus εHf(t) value (a) and frequency distribution histogram of Hf model ages (TDMC) (b) for zircons from the granitic rocks in the Harlik Mountain

    表  1   哈尔里克地区花岗岩LA-ICP-MS锆石U-Th-Pb测试结果

    Table  1   LA-ICP-MS zircon U-Th-Pb dating results for representative granites from the Harlik area

    测点含量/10-6Th/U同位素比值年龄/Ma
    232Th238U207Pb/206Pb207Pb/235U206Pb/238U207Pb/206Pb207Pb/235U206Pb/238U
    小铺黑云母二长花岗岩(T12716-1.2)
    1541630.330.051730.002020.35460.01530.049730.0014927387308113139
    21202070.580.055850.001990.38190.01540.049600.0014844677328113129
    31542500.620.054390.001870.37660.01470.050230.0014938775325113169
    43145220.600.055940.001490.41010.01360.053180.0015545058349103349
    51363500.390.054400.001650.38970.01400.051960.0015338766334103279
    61953480.560.056920.001900.40830.01560.052040.0015548873348113279
    71504760.320.053250.001480.38440.01300.052350.0015334062330103299
    81653580.460.053400.001590.36070.01280.049000.0014334666313103089
    91302810.460.055410.001890.38180.01480.049980.0014942874328113149
    101122720.410.053190.001720.36840.01380.050240.0014833772319103169
    11361030.350.065230.003480.44430.02460.049410.001587821083731731110
    121402290.610.054540.002330.35840.01650.047670.0014639393311123009
    1355714910.370.053450.001200.36300.01090.049270.001413485031583109
    141283510.360.054480.001680.35950.01310.047860.0014039168312103019
    151072580.410.053800.001930.36140.01460.048740.0014436279313113079
    16622300.270.049690.001860.34250.01430.050000.0014718185299113159
    172564190.610.051650.001550.34480.01230.048420.001412706830193059
    181041690.610.058250.003000.38790.02090.048310.00152539109333153049
    19882400.360.053840.002200.37160.01660.050060.0015036489321123159
    2046714120.330.054090.001250.39750.01210.053310.001533755134093359
    21782230.350.050760.002330.35670.01760.050970.00154230103310133219
    222067410.280.053510.001430.36170.01200.049030.001423515931493099
    231152340.490.050640.002190.34670.01620.049660.0014822597302123129
    2440413760.290.052270.001360.37620.01220.052210.001512975832493289
    252519860.250.053780.001910.37880.01520.051090.0015136278326113219
    26311170.260.063500.005250.46050.03830.052600.001817251663852733111
    27702120.330.054360.003220.39480.02420.052680.001633861283381833110
    28491920.250.051250.005140.33940.03420.048050.001632522152972630310
    29171928340.610.434780.009253.54350.10170.059120.0017140343115372337010
    301293150.410.053430.002560.37740.01920.051230.001553471053251432210
    沁城南含角闪石二长花岗岩(T12716-8.4)
    11482820.530.048890.001710.34100.01340.050590.0014614380298103189
    22425620.430.051700.001360.36690.01180.051480.001462725931793249
    33055260.580.055660.001420.39410.01250.051350.001464395633793239
    42464680.530.224010.004811.99860.05690.064720.0018430103411151940411
    52404160.580.050170.001440.35730.01220.051660.001472036531093259
    62134210.500.054270.001560.38210.01300.051070.0014638263329103219
    72063970.520.054930.001530.39000.01300.051510.0014740960334103249
    81983860.510.054960.001590.39200.01340.051740.0014841063336103259
    92194200.520.052950.001480.37810.01270.051800.001483266232693269
    101663400.490.051080.001570.36600.01310.051980.0014924569317103279
    111473190.460.051080.001630.35950.01320.051050.0014724572312103219
    122143820.560.052010.001470.36880.01250.051430.001472866331993239
    132404180.570.056690.001570.40700.01350.052080.0014847960347103279
    142213760.590.053610.001520.37370.01260.050570.001443556332293189
    151302450.530.050950.001720.35060.01340.049910.0014423976305103149
    161983440.580.053860.001560.38430.01320.051750.0014836564330103259
    171612980.540.053260.001700.38190.01400.052010.0014934071328103279
    181241910.650.052600.002000.36760.01540.050680.0014831284318113199
    192124220.500.065290.001780.38840.01270.043150.001237845633392728
    202534750.530.052680.001410.36230.01180.049880.001413156031493149
    212404400.540.050320.001400.34610.01150.049890.001422106330293149
    224185420.770.051780.001400.37120.01210.052000.001482766132193279
    231732720.640.053570.001720.36450.01340.049350.0014235371316103119
    244846590.730.053190.001330.36790.01140.050180.001423375631883169
    25881870.470.046310.002300.31760.01660.049750.0014614115280133139
    262354280.550.053460.001450.37100.01220.050340.001433486032093179
    274306540.660.052920.001300.37310.01150.051130.001443265532283219
    282524250.590.052770.001460.36700.01220.050440.001433196231793179
    292053680.560.052020.001540.36050.01250.050260.001432866631393169
    302915580.520.054200.001370.37630.01180.050350.001423795632493179
    下载: 导出CSV

    表  2   哈尔里克地区花岗岩主量、微量和稀土元素组成

    Table  2   Major, trace and rare earth elements compositions of granites from the Harlik area

    含量小铺黑云母二长花岗岩(316Ma)沁城南含角闪石二长花岗岩(320Ma)
    T12716-1.1T12716-1.2T12716-1.3T12716-1.4T12716-8.2T12716-8.3T12716-8.4T12716-8.5
    SiO272.8371.3871.7868.4267.7172.2671.8872.07
    Al2O314.0414.8614.2016.1517.0013.8713.9614.04
    Fe2O3T2.242.222.842.662.232.512.742.67
    MgO0.330.310.410.400.160.170.180.17
    CaO1.571.991.882.580.910.730.750.68
    Na2O4.074.174.134.687.035.525.615.59
    K2O3.643.833.423.453.853.803.853.92
    TiO20.190.190.240.240.170.190.200.19
    P2O50.050.060.070.060.040.030.040.02
    MnO0.070.070.090.080.070.110.130.12
    烧失量0.800.700.801.100.500.600.400.30
    总计99.8599.8199.8299.8299.6899.7899.7799.78
    A/CNK1.041.021.021.000.980.960.950.96
    Mg#25.5624.5525.1725.9514.3313.6313.2812.92
    La18.6022.2020.9031.4010.2042.2044.1042.70
    Ce40.1048.9046.9063.3025.6089.6096.8091.50
    Pr4.005.074.746.733.499.7710.759.98
    Nd14.9020.2017.7024.8016.1038.4040.8036.80
    Sm2.473.783.924.464.367.086.936.79
    Eu1.071.121.011.231.810.900.871.02
    Gd2.503.403.854.124.715.766.556.16
    Tb0.400.550.650.630.850.870.920.90
    Dy2.223.163.973.735.135.035.165.28
    Ho0.430.590.790.731.141.071.081.01
    Er1.411.692.022.083.462.952.963.27
    Tm0.200.240.300.290.500.450.460.49
    Yb1.121.511.771.923.452.903.183.22
    Lu0.200.230.290.250.640.520.560.56
    Y13.2017.0019.4018.2029.5025.8026.3027.20
    ΣREE89.62112.64108.81145.6781.44207.50221.12209.68
    δEu1.300.940.790.861.210.420.390.47
    (La/Yb)N11.9110.558.4711.732.1210.449.959.51
    Ba992.001195.001029.00990.002145.001218.001220.001205.00
    Co2.302.802.802.801.001.101.401.10
    Cs1.101.101.201.500.900.800.701.10
    Ga14.9015.8015.9017.1020.4016.6017.4017.00
    Hf4.504.404.704.6011.308.109.108.80
    Nb4.604.406.205.503.203.904.104.50
    Rb69.0069.1067.0063.9056.2035.4035.8036.10
    Sr198.20226.40213.20260.9051.4036.0038.6033.80
    Ta0.200.200.500.300.400.300.200.30
    Th3.604.703.905.603.704.504.304.90
    U0.600.400.500.501.401.601.401.30
    V21.0022.0023.0016.008.009.008.009.00
    Zr153.30154.20173.40174.10589.40428.90495.00442.60
    Zn28.0038.0063.0036.008.0019.0023.0017.00
    Ni1.701.301.601.400.901.001.300.90
    Cu2.702.403.102.402.602.302.201.60
    Pb5.405.505.805.102.302.903.102.90
    注:主量元素含量单位为%,微量和稀土元素含量为10-6
    下载: 导出CSV

    表  3   哈尔里克地区花岗岩锆石Hf同位素测试结果

    Table  3   Zircon Hf isotopic compositions of representative granites from the Harlik area

    测点号年龄/Ma176Yb/177Hf176Lu/177Hf176Hf/177HfεHf(t)TDM/MaTDMC/MafLu/Hf
    小铺黑云母二长花岗岩
    T12716-1-23120.0694460.0016770.2828900.00002610.7523644-0.95
    T12716-1-43340.2027730.0047510.2828300.0000548.3665812-0.86
    T12716-1-63270.1950210.0046140.2829870.00004013.8416456-0.86
    T12716-1-73290.0491020.0013610.2829190.00002812.1477565-0.96
    T12716-1-83080.1211810.0029040.2829830.00003013.7401450-0.91
    T12716-1-93140.0510770.0013110.2829270.00003312.1465554-0.96
    T12716-1-103160.0364450.0009150.2828900.00002610.9512632-0.97
    T12716-1-123000.0762840.0018580.2828950.00002510.6519643-0.94
    T12716-1-133100.0679110.0017890.2828420.0000308.9594756-0.95
    T12716-1-143010.0431400.0010860.2829530.00002712.8425500-0.97
    T12716-1-163150.0377770.0010300.2828080.0000268.0631822-0.97
    T12716-1-173050.0706230.0018240.2829790.00002013.6396449-0.95
    T12716-1-183040.0571670.0015340.2829090.00002511.2493604-0.95
    T12716-1-193150.0485550.0012680.2828800.00002110.5531660-0.96
    T12716-1-213210.0265240.0006810.2828370.0000159.2583746-0.98
    T12716-1-233120.0545000.0013830.2828850.00001710.6526652-0.96
    T12716-1-243280.0776010.0019990.2828530.0000149.6582725-0.94
    T12716-1-273310.0331280.0007690.2828480.0000189.8569716-0.98
    T12716-1-303220.0702640.0015290.2829210.00002012.0476567-0.95
    沁城南含角闪石二长花岗岩
    T12716-8-13180.1082560.0029680.2829830.00001713.8402446-0.91
    T12716-8-23240.0998010.0028950.2829590.00001613.1437497-0.91
    T12716-8-33230.1567750.0042970.2829950.00001914.1400435-0.87
    T12716-8-53250.2042860.0054670.2829510.00002712.3485551-0.84
    T12716-8-63210.1928430.0050080.2829380.00003011.9499576-0.85
    T12716-8-113210.0918360.0027400.2829620.00002313.2431489-0.92
    T12716-8-123230.1383010.0036720.2830640.00003516.7286268-0.89
    T12716-8-133270.1506350.0040700.2829880.00002113.9408447-0.88
    T12716-8-143180.1505590.0039440.2829870.00002113.8407450-0.88
    T12716-8-153140.1200820.0033010.2829340.00001711.9481566-0.90
    T12716-8-163250.1971420.0051640.2830290.00003415.1355368-0.84
    T12716-8-183190.0534380.0017200.2829810.00001814.1391433-0.95
    T12716-8-203140.1726480.0046900.2829090.00001710.8540641-0.86
    T12716-8-213140.1881880.0049180.2830430.00002815.5330337-0.85
    T12716-8-243160.1233790.0035910.2829400.00002712.1476555-0.89
    T12716-8-253130.0671880.0020840.2829840.00002613.9392436-0.94
    T12716-8-283170.1692370.0045240.2830080.00002314.4382412-0.86
    T12716-8-293160.1637770.0042550.2830110.00001814.5374402-0.87
    T12716-8-303170.0698960.0019550.2829340.00001412.3463545-0.94
    注:εHf(t)={[(176Hf/177Hf)S-(176Lu/177Hf)S×(eλt-1)]/[(176Hf/177Hf)CHUR, 0-(176Lu/177Hf)CHUR×(eλt-1)]-1}×10000;TDM=1/λ×ln{1+[(176Hf/177Hf)S-(176Hf/177Hf)DM]/[(176Lu/177Hf)S-(176Lu/177Hf)DM]}; TDMC=1/λ×ln{1+[(176Hf/177Hf)S, t-(176Hf/177Hf)DM, t]/[(176Lu/177Hf)C-(176Lu/177Hf)DM]}+t, 其中, s为样品, (176Hf/177Hf)CHUR, 0=0.282772和(176Lu/177Hf)CHUR=0.0332[32], (176Hf/177Hf)DM=0.28325和(176Lu/177Hf)DM=0.0384[33]t为锆石结晶年龄, λ=1.865×10-11 year-1[34]; (176Lu/177Hf)C=0.015
    下载: 导出CSV
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