Petrological, geochemical and chronologic characteristics of the intrusive bodies on the south side of Karamaili ophiolite belt in eastern Junngar
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摘要:
东准噶尔卡拉麦里蛇绿岩带南侧分布有大量的石炭纪侵入体，主要出露于五彩城、滴水泉一带及野马站地区。通过对卡拉麦里断裂以南侵入体岩石类型、锆石年代学、地球化学的综合分析，划分出早石炭世后碰撞I型花岗岩类及晚石炭世陆内双峰式侵入岩（碱长花岗岩+角闪辉长岩）。结合断裂以北黄羊山、老鸦泉岩体新近发表的数据及区域内火山岩的研究成果，对卡拉麦里地区石炭纪-二叠纪构造-岩浆演化过程给出了新认识，即卡拉麦里地区从后碰撞到陆内伸展的构造转换时间为早石炭世末期-晚石炭世早期，后碰撞阶段岩浆岩以钙碱性I型花岗岩、玄武安山岩、安山岩为特点，陆内伸展阶段以典型的双峰式岩浆岩（辉长岩+花岗岩、玄武岩+流纹岩）及A型花岗岩为特点，卡拉麦里地区具有正εNd值的花岗岩类来源于亏损地幔形成的年轻地壳的部分熔融。
Abstract:There are many Carboniferous intrusive bodies on the south side of Karamaili ophiolite belt in eastern Junngar, which are mainly distributed in Wucaicheng area and Dishuiquan-Yemazhan zone. Based on the study of the characteristics of the intrusive bod-ies such as rock types, zircon geochronology and geochemistry, we can distinguish the early Carboniferous post-collisional I-type gra-nitic rocks from the late Carboniferous intra-continental bimodal rock associations (K-feldspar granite and hornblende-gabbro). Combined with the recently published data for Laoyaquan pluton, Huangyangshan pluton and volcanic rocks in Karamaili area, the au-thors have reached some new conclusions about the tectonic-magmatic evolution in Karamaili from Carboniferous to Permian. Firstly, the tectonic transition from post-collision to intra-continent extension may have occurred between early and late Carboniferous. The post-collisional igneous rocks are characterized by calc-alkaline I-type granite, basalt andesite and andesite, and the intra-continent extensional rock types are mainly composed of bimodal rock associations and A-type granite. Secondly, the granitoids in Karamaili are characterized by positive Nd values, suggesting that they were most probably from the young crust formed by depleted mantle.
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Keywords:
- eastern Junngar /
- Karamaili /
- tectonic-magmatic evolution /
- granite /
- post-collision /
- intra-continent extension
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图 2 卡拉麦里断裂以南侵入体地质图（底图据参考文献①修改）
Q—第四系；J-K—侏罗系-白垩系；P1-2s—二叠系胜利沟组；C2b—上石炭统巴塔玛依内山组；C1j—下石炭统姜巴斯套组；C1t—下石炭统塔木岗组；D3-C1ka—上泥盆统-下石炭统克安库都克组；D2b—中泥盆统北塔山组；D1-2k—泥盆系卡拉麦里组；S—志留系
Figure 2. Geological map of the intrusive bodies south of Karamaili ophiolite belt in eastern Junngar
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图 3 野马站石英二长闪长岩的野外岩貌特征（a）及镜下特征（+）（b）
Pl—斜长石；Kf—碱性长石；Qz—石英；Am—角闪石
Figure 3. The outcrops (a) and microscopic features (b) of quartz monzodiorite in Yemazhan
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图 4 卡拉麦里断裂以南侵入岩QAP分类图解（底图据参考文献[29]）
1—富石英花岗岩；2—碱长花岗岩；3a—正长花岗岩；3b—二长花岗岩；4—花岗闪长岩；5—英云闪长岩、斜长花岗岩；6*—碱长石英正长岩；7*—石英正长岩；8*—石英二长岩；9*—石英二长闪长岩；10*—石英闪长岩；6—碱长正长岩；7—正长岩；8—二长岩；9—二长闪长岩；10—闪长岩
Figure 4. QAP classification diagram for the intrusive rocks from the south of Karamaili ophiolite belt
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图 5 野马站石英二长闪长岩锆石CL图像(a)及锆石U-Pb年龄谐和图(b)
Figure 5. CL imaging of zircons from Yemazhan quartz monzobiorite (a) and U-Pb age concordia plots of zircons from Yemazhan quartz monzobiorite (b)
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图 6 侵入岩SiO2-K2O图解(a)[34]和TAS图解(b)[35]
1—橄榄辉长岩；2a—碱性辉长岩；2b—亚碱性辉长岩；3—辉长闪长岩；4—闪长岩；5—花岗闪长岩；6—花岗岩；7—硅英岩；8—二长辉长岩；9—二长闪长岩；10—二长岩；11—石英二长岩；12—正长岩；13—副长石辉长岩；14—副长石二长闪长岩；15—副长石二长正长岩；16—副长正长岩；17—副长深成岩
Figure 6. SiO2-K2O diagram and TAS diagram for the intrusive bodies from the south of Karamaili ophiolite belt
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图 7 微量元素蛛网图（a）和稀土元素配分曲线（b）（底图据参考文献[36]，数据来源及图例同图 6）
Figure 7. Spider diagram of trace elements and chondrite-normalized REE patterns
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图 9 卡拉麦地区花岗岩的εNd（t）特征
Figure 9. εNd(t)characteristics for the granitic rocks of Karamaili area
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图 10 卡拉麦里地区花岗岩构造判别图
a—R1-R2判别图[43]；1—幔源花岗岩；2—板块碰撞前消减地区花岗岩；3—板块碰撞后隆起花岗岩；4—晚造山期花岗岩；5—非造山花岗岩；6—地壳熔融的花岗岩（同碰撞）；7—造山后期花岗岩。R1=4Si-11(Na+K)-2(Fe+Ti)；R2=6Ca+2Mg+Al；b—C-FM图解。FM=100×(TFeO+MgO)/(Al2O3+Na2O+K2O+TFeO+MgO+ CaO)；C=100×CaO/(Al2O3+Na2O+K2O+TFeO+MgO+CaO)[44]；c—M-F图解：F=100×TFeO/(Al2O3+Na2O+K2O+TFeO+MgO)，M=100×MgO/(Al2O3+Na2O+K2O+TFeO+MgO)[44]；IAG—岛弧花岗岩类；CAG—大陆弧花岗岩类；CCG—大陆碰撞花岗岩类；POG—后造山花岗岩类；RRG—与裂谷有关的花岗岩类；CEUG—与大陆的造陆抬升有关的花岗岩类（数据来源及图例同图 6）
Figure 10. Tectonic setting determinant diagram of the granites of the area of Karamaili
表 1 野马站石英二长闪长岩LA-ICP-MS锆石U-Th-Pb定年数据
Table 1 LA-ICP-MS zircon U-Th-Pb data for Yemazhan quartz monzobiorite
分析号 Pb Th U Th/U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 206Pb/238U 1σ /10-6 比值 比值 比值 年龄/Ma 055-5-01 14.07 167 212 0.79 0.0521 0.0025 0.382 0.0179 0.0528 0.0007 332 4 055-5-02 9.37 83.1 154 0.54 0.0562 0.0032 0.397 0.0220 0.0513 0.0008 323 5 055-5-03 7.77 67.8 125 0.54 0.0526 0.0038 0.378 0.0251 0.0526 0.0008 331 5 055-5-04 8.49 79.4 135 0.59 0.0547 0.0036 0.396 0.0255 0.0526 0.0008 331 5 055-5-05 10.30 86.6 164 0.53 0.0491 0.0030 0.360 0.0214 0.0538 0.0012 338 7 055-5-06 5.23 43.7 82.8 0.53 0.0564 0.0040 0.410 0.0284 0.0537 0.0012 337 7 055-5-07 6.81 73.5 105 0.70 0.0529 0.0036 0.374 0.0244 0.0517 0.0010 325 6 055-5-08 8.47 75.7 139 0.55 0.0518 0.0034 0.375 0.0239 0.0522 0.0009 328 5 055-5-09 7.39 64.9 117 0.55 0.0564 0.0040 0.401 0.0261 0.0533 0.0010 335 6 055-5-10 7.10 59.5 113 0.53 0.0524 0.0037 0.390 0.0258 0.0540 0.0009 339 6 055-5-11 12.70 158 197 0.80 0.0540 0.0037 0.384 0.0250 0.0521 0.0008 327 5 055-5-12 7.46 66.3 119 0.56 0.0567 0.0034 0.419 0.0232 0.0536 0.0009 337 5 055-5-13 7.28 63.2 119 0.53 0.0573 0.0037 0.403 0.0252 0.0521 0.0009 327 6 055-5-14 9.46 84.1 155 0.54 0.0520 0.0031 0.373 0.0216 0.0517 0.0007 325 4 055-5-15 61.4 92.6 171 0.54 0.0504 0.0031 0.373 0.0235 0.0528 0.0008 332 5 055-5-16 8.46 75.1 137 0.55 0.0614 0.0039 0.435 0.0260 0.0523 0.0009 328 6 055-5-17 16.93 192 261 0.74 0.0555 0.0028 0.402 0.0201 0.0525 0.0007 330 4 055-5-18 8.40 69.2 134 0.52 0.0559 0.0036 0.406 0.0256 0.0529 0.0008 332 5 055-5-19 8.43 70.9 135 0.53 0.0568 0.0034 0.411 0.0249 0.0530 0.0008 333 5 055-5-20 7.38 55.5 117 0.48 0.0570 0.0038 0.417 0.0269 0.0538 0.0009 338 5 055-5-21 8.83 73.3 138 0.53 0.0629 0.0044 0.448 0.0311 0.0532 0.0010 334 6 055-5-22 15.78 193 244 0.79 0.0547 0.0028 0.387 0.0189 0.0515 0.0007 324 4 055-5-23 8.20 69.6 129 0.54 0.0603 0.0039 0.444 0.0291 0.0535 0.0009 336 5 
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表 2 野马站石英二长闪长岩全岩主量、微量和稀土元素数据
Table 2 Whole-rock major, trace, and rare earth elements of Yemazhan quartz monzobiorite
样品号 SiO2 TiO2 Al2O3 Fe2O3 FeO MnO MgO CaO Na2O K2O P2O5 H2O+ CO2 烧失量 024-2-1 62.23 0.89 15.73 1.83 3.82 0.11 2.69 4.69 3.04 2.74 0.16 1.65 0.24 5.47 055-5-1 62.36 0.91 16.04 2.08 3.58 0.10 2.58 4.92 3.45 2.09 0.17 1.42 0.05 5.45 样品号 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Y ΣREE 024-2-1 20.0 44.2 5.93 25.3 5.64 1.31 5.32 0.911 5.34 1.09 3.14 0.486 3.04 0.462 29.4 152 055-5-1 14.72 33.45 4.50 19.77 4.83 1.09 4.63 0.74 4.49 0.88 2.67 0.39 2.65 0.39 24.0 119.2 样品号 Be Ni Sc V Pb Cr Co Rb Cs Ta Nb Hf Zr Th U Ba Sr Ga 024-2-1 1.35 8.48 17.1 135 10.2 36.4 16.8 98.6 2.50 0.43 6.23 6.11 183 9.07 2.23 480 322 22.2 055-5-1 1.77 10.21 14.34 142.7 9.23 25.8 18.20 74.22 3.19 0.43 6.32 7.7 180.0 4.58 1.66 353.7 320.9 22.35 注：主量元素含量单位为%；微量和稀土元素含量为10-6
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表 3 卡拉麦里地区花岗岩及石英二长闪长岩的Nd同位素数据
Table 3 Nd isotopic composition of the granitic rocks and Yemazhan quartz monzobiorite from the Karamaili area
产地 五彩城 滴水泉一带 野马泉 黄羊山 苏吉泉 （t=341Ma）[10] （t=321Ma)[28] （t=331Ma）（本文） （t=302Ma）[23] （t=302Ma）[25] （t=304Ma）[23] εNd(t) 5.46 5.95 5.41 5.52 5.9 3.70 6.40 5.52 5.90 6.40 5.52 5.90 6.40 5.52 TDM2Nd/Ga 650 611 654 630 598 787 618 578 732 610 700 554 579 587 注：同位素校正公式：εNd(t)=（[ 143Nd/144Nd）样品/（143Nd/144Nd）CHUR（t）-1]×104, （143Nd/144Nd）CHUR（t）=0.512638-0.1967×（eλt-1）；λSm-Nd=6.54×10-12·a-1
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