Chronology and geochemistry of volcanic rocks from Manketouebo Formation in the Suolun area, central Da Hinggan Mountains and their tectonic implications
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摘要:
对大兴安岭中段索伦地区满克头鄂博组火山岩进行了岩石地球化学、锆石U-Pb及Hf同位素研究，讨论该地区火山岩的形成时代和构造背景。用LA-ICP-MS测得索伦地区满克头鄂博组2个流纹岩样品的锆石206Pb/238U年龄分别为138.0±1.5Ma和139.9±2.5Ma，表明火山岩的形成时代是早白垩世早期，而非晚侏罗世；地球化学数据显示其具有高硅、富碱、弱过铝质-过铝质（A/CNK=0.99~1.34）、分异程度高的特点，属于高钾钙碱性系列，相对富集轻稀土元素和部分大离子亲石元素（Rb、Th、U、K），亏损高场强元素（Nb、Ta、Ti、P）。锆石Hf同位素组成表明，该区满克头鄂博组火山岩具有较高的εHf（t）值（+4.06~+8.24），二阶段模式年龄为936~664Ma，暗示其可能起源于从亏损地幔增生的年轻地壳物质的部分熔融。结合区域地质资料分析，满克头鄂博组火山岩形成于造山后伸展环境，可能与蒙古-鄂霍茨克洋闭合后造山带的垮塌密切相关。
Abstract:In this study, the authors conducted detailed geochronological, geochemical and Hf isotopic researches on the volcanic rocks of the Manketouebo Formation from the Suolun area in the central Da Hinggan Mountains. LA-ICP-MS zircon U-Pb dating reveals that the Manketouebo volcanic rocks from the Suolun area were formed in 140~138Ma, i.e., the early Early Cretaceous rather than Late Jurassic as previously thought. Geochemical data show that the volcanic rocks are characterized by high silicon, rich alkali, weakly peraluminous nature (A/CNK=0.99~1.34) and high degree of differentiation, thus belonging to high-k calc-alkaline series. They are enriched in LILEs (Rb, Th, U, K) and LREEs, and depleted in HFSEs (Nb, Ta, Ti, P). Their zircon Hf isotopic compositions show that the Manketouebo volcanic rocks of the study area have relatively high εHf (t) values (+4.06~+8.24) with the two-stage model ages ranging from 936Ma to 664Ma, implying that they were probably derived from partial melting of juvenile crustal materials that accreted from the depleted mantle. According to the regional geologic data, it is concluded that the volcanic rocks of the Manketouebo Formation formed in a post-orogenic extensional setting, which was probably closely related to the collapse of orogenic belt after the closure of Mongol-Okhotsk Ocean.
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Keywords:
- central Da Hinggan Mountains /
- Manketouebo Formation /
- zircon U-Pb ages /
- Hf isotope /
- LA-ICP-MS
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致谢: 在成文过程中得到吉林大学马瑞和杨德明教授的帮助，修改过程中得了到吉林大学葛文春教授的悉心指导，实验数据处理上得到了吉林大学王智慧师姐、杜岳丹师兄的鼎力相助，在此一并致以衷心的感谢。
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图 1 研究区地质略图
F1—贺根山-黑河缝合带；F2—塔源-喜桂图缝合带
Figure 1. Geological sketch map of the study area
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图 2 MB2200样品锆石阴极发光（CL）图像（a）及U-Pb谐和图（b）
Figure 2. CL images (a) and U-Pb concordia diagram of zircons (b) from sample MB2200
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图 3 P13-8-1样品锆石阴极发光（CL）图像（a）及U-Pb谐和图（b）
Figure 3. CL images (a) and U-Pb concordia diagrams of zircon (b) from sample P13-8-1
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图 4 满克头鄂博组火山岩含铝指数（a）和SiO2-P2O5图解（b）
Figure 4. Aluminous index (a) and SiO2-P2O5 diagrams (b) for the Manketouebo Formation volcanic rocks
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图 5 满克头鄂博组火山岩TAS图解（a）和SiO2-K2O图解（b）
Figure 5. TAS (a) and SiO2-K2O (b) diagrams for the Manketouebo Formation volcanic rocks
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图 7 满克头鄂博组火山岩锆石Hf同位素演化图解
Figure 7. Zircon Hf isotopic evolution diagram for the Manketouebo Formation volcanic rocks
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图 8 大兴安岭地区满克头鄂博组火山岩的年龄统计概率曲线图
Figure 8. Age probability statistical diagram for the volcanic rocks of the Manketouebo Formation in the Da Hinggan Mountains
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图 9 满克头鄂博组火山岩成因类型判别图
A—A型花岗岩；FG—高分异的Ⅰ型花岗岩；OGT—未见分异的I，S，M型花岗岩
Figure 9. Various chemical discrimination diagrams for the volcanic rocks of the Manketouebo Formation
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图 10 满克头鄂博组火山岩的(Y+Nb)-Rb（a）和R1-R2图解（b）
Figure 10. Plot of (Y+Nb)-Rb (a) and R1-R2 diagram (b) of the Manketouebo Formation volcanic rocks
表 1 索伦地区满克鄂博组火山岩LA-ICP-MS锆石U-Th-Pb分析结果
Table 1 LA-ICP-MS zircon U-Th-Pb dating results for the vocanic rocks of Manketouebo Formation from Suolun area
样品号及分析点号 含量/10-6 Th/U 同位素比值 年龄/Ma Th U Pb 207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U MB2200 1 125 158 4.4 0.79 0.0496±0.0031 0.1444±0.0089 0.02112±0.00045 177±102 137±8 135±3 2 57 103 2.8 0.55 0.0518±0.0055 0.1553±0.0159 0.02174±0.00071 279±172 147±14 139±4 3 199 178 5.5 1.12 0.0520±0.0038 0.1580±0.0113 0.02203±0.00056 287±118 149±10 140±4 4 128 153 4.3 0.84 0.0536±0.0050 0.1523±0.0138 0.02061±0.00064 356±150 144±12 132±4 5 140 166 4.8 0.84 0.0485±0.0025 0.1468±0.0074 0.02194±0.00041 128±81 139±7 140±3 6 90 112 3.1 0.80 0.0513±0.0061 0.1506±0.0174 0.02130±0.00079 256±192 143±15 136±5 7 144 163 4.6 0.89 0.0529±0.0037 0.1501±0.0101 0.02058±0.00049 327±111 142±9 131±3 8 74 112 3.1 0.66 0.0509±0.0035 0.1497±0.0100 0.02133±0.00050 238±111 142±9 136±3 9 113 158 4.4 0.72 0.0499±0.0027 0.1468±0.0078 0.02136±0.00041 190±88 139±7 136±3 10 78 135 3.7 0.58 0.0496±0.0034 0.1453±0.0096 0.02126±0.00048 177±109 138±9 136±3 11 141 166 5.0 0.85 0.0488±0.0023 0.1487±0.0069 0.02209±0.00039 142±76 141±6 141±2 12 95 136 4.0 0.70 0.0490±0.0032 0.1514±0.0098 0.02243±0.00050 148±106 143±9 143±3 13 135 224 6.3 0.60 0.0495±0.0030 0.1505±0.0090 0.02203±0.00049 176±97 142±8 140±3 14 102 136 4.0 0.75 0.0482±0.0027 0.1456±0.0080 0.02189±0.00043 113±88 138±7 140±3 15 99 138 4.0 0.71 0.0475±0.0025 0.1454±0.0076 0.02217±0.00042 79±82 138±7 141±3 16 192 185 5.4 1.04 0.0516±0.0036 0.1459±0.0099 0.02053±0.00050 268±111 138±9 131±3 17 124 156 4.6 0.79 0.0500±0.0026 0.1501±0.0077 0.02176±0.00043 197±83 142±7 139±3 18 101 139 4.0 0.73 0.0489±0.0026 0.1462±0.0075 0.02168±0.00042 144±82 139±7 138±3 19 83 117 3.4 0.71 0.0490±0.0027 0.1485±0.0080 0.02197±0.00044 150±88 141±7 140±3 20 123 151 4.5 0.82 0.0476±0.0024 0.1464±0.0072 0.02227±0.00040 83±77 139±6 142±3 21 91 124 3.6 0.74 0.0488±0.0028 0.1454±0.0081 0.02159±0.00043 141±90 138±7 138±3 22 71 94 2.8 0.75 0.0506±0.0065 0.1464±0.0181 0.02098±0.00087 223±202 139±16 134±5 P13-8-1 1 283 392 11.2 0.72 0.0487±0.0017 0.1538±0.0053 0.02290±0.00038 135±50 145±5 146±2 2 420 1118 28.2 0.38 0.0496±0.0026 0.1525±0.0078 0.02231±0.00046 177±82 144±7 142±3 3 262 450 12.5 0.58 0.0516±0.0032 0.1624±0.0099 0.02283±0.00053 268±98 153±9 146±3 4 493 1001 27.1 0.49 0.0480±0.0011 0.1524±0.0037 0.02302±0.00034 101±31 144±3 147±2 5 131 154 4.3 0.85 0.0518±0.0053 0.1543±0.0152 0.02161±0.00073 279±161 146±13 138±5 6 194 220 7.1 0.88 0.0520±0.0052 0.1605±0.0159 0.02236±0.00049 289±233 151±14 143±3 7 219 550 14.2 0.40 0.0489±0.0013 0.1510±0.0040 0.02238±0.00033 145±36 143±4 143±2 8 105 273 7.2 0.38 0.0484±0.0017 0.1518±0.0054 0.02274±0.00037 121±54 144±5 145±2 9 33 66 1.8 0.49 0.0493±0.0056 0.1512±0.0167 0.02222±0.00066 164±193 143±15 142±4 10 309 497 12.9 0.62 0.0541±0.0030 0.1559±0.0083 0.02091±0.00045 376±82 147±7 133±3 11 497 433 13.4 1.15 0.0488±0.0013 0.1509±0.0042 0.02241±0.00034 140±38 143±4 143±2 12 187 221 6.5 0.84 0.0490±0.0023 0.1526±0.0072 0.02259±0.00043 148±75 144±6 144±3 13 193 331 8.9 0.58 0.0519±0.0033 0.1568±0.0097 0.02192±0.00051 281±99 148±9 140±3 14 190 499 12.5 0.38 0.0527±0.0021 0.1566±0.0060 0.02153±0.00038 320±56 148±5 137±2 15 162 154 4.7 1.05 0.0491±0.0032 0.1497±0.0095 0.02208±0.00050 157±103 142±8 141±3 16 243 357 9.3 0.68 0.0543±0.0033 0.1554±0.0092 0.02075±0.00047 385±92 147±8 132±3 17 457 884 22.6 0.52 0.0533±0.0015 0.1552±0.0043 0.02109±0.00032 345±37 147±4 135±2 18 461 510 14.2 0.90 0.0544±0.0020 0.1551±0.0055 0.02067±0.00035 390±50 146±5 132±2 19 1479 1085 34.2 1.36 0.0488±0.0034 0.1405±0.0095 0.02088±0.00034 139±159 134±9 133±2 20 199 297 7.8 0.67 0.0538±0.0034 0.1544±0.0094 0.02079±0.00048 366±97 146±8 133±3 
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表 2 索伦地区满克头鄂博组火山岩主量、微量和稀土元素分析结果
Table 2 Major, trace and rare earth elements compositions for the vocanic rocks of Manketouebo Formation from Suolun area
样号 P2-1-1 MB6014-1 MB5265-1 MB5217 MB4222 MB1022 MB2108-1 P13-5-1 P13-38-1 MB0872 MB1873 SiO2 72.88 70.09 73.60 71.77 71.64 71.41 72.86 76.69 73.03 75.65 74.79 TiO2 0.23 0.40 0.34 0.30 0.26 0.35 0.31 0.20 0.33 0.10 0.13 Al2O3 13.77 15.59 13.43 14.72 15.61 14.63 14.02 12.21 14.02 12.93 13.08 Fe2O3 2.65 1.94 0.95 1.40 1.46 1.63 1.27 1.01 1.18 1.02 1.06 FeO 0.75 0.70 1.03 0.75 0.66 0.42 0.85 0.22 0.50 0.32 0.58 FeOT 3.13 2.44 1.88 2.01 1.97 1.88 1.99 1.13 1.55 1.23 1.54 MnO 0.05 0.10 0.05 0.07 0.02 0.08 0.06 0.06 0.07 0.03 0.02 MgO 0.20 0.70 0.41 0.52 0.26 0.41 0.38 0.11 0.21 0.08 0.07 CaO 0.33 0.40 0.34 0.61 0.25 0.59 0.47 0.08 0.25 0.17 0.38 Na2O 4.59 4.07 4.05 4.23 4.20 4.41 4.27 4.22 4.34 4.26 4.20 K2O 4.61 3.86 4.78 4.16 4.70 4.71 4.21 4.81 5.06 4.93 5.21 P2O5 0.05 0.15 0.05 0.09 0.06 0.10 0.10 0.02 0.06 0.01 0.05 烧失量 0.63 1.76 0.82 1.15 1.50 1.04 1.01 0.29 0.78 0.41 0.38 总量 100.73 99.75 99.85 99.77 100.62 99.78 99.80 99.85 99.70 99.91 99.96 Li 19.30 20.73 14.20 19.51 6.38 15.98 19.75 2.79 13.94 5.21 12.30 Be 1.38 2.56 2.71 2.17 1.88 3.74 2.58 2.48 2.68 3.67 3.27 Sc 11.80 4.59 6.35 4.06 2.52 4.01 4.74 4.50 6.34 4.99 6.01 V 85.50 34.25 28.72 31.51 5.18 32.87 34.72 4.71 12.35 0.94 1.52 Cr 2.96 7.27 13.48 9.25 13.30 9.62 9.73 3.74 3.30 4.03 3.25 Co 8.50 3.57 2.34 2.67 0.46 2.54 2.69 0.16 0.62 0.64 0.71 Ni 2.88 1.18 6.05 1.33 6.42 4.86 2.51 1.80 1.28 0.61 0.27 Cu 10.70 6.34 9.54 6.17 2.51 8.60 8.20 1.20 2.15 1.29 0.99 Zn 101.00 54.73 42.98 49.53 42.80 55.73 116.83 62.08 60.04 92.38 46.28 Ga 20.20 18.57 21.83 18.45 18.10 21.02 19.52 18.43 19.82 19.46 18.42 Rb 95.70 100.72 94.21 114.05 115.00 126.35 143.15 128.14 113.65 187.20 182.50 Sr 488.00 279.51 87.74 226.28 213.00 153.93 217.46 10.76 108.10 28.75 39.35 Zr 329.00 151.56 235.64 189.51 301.00 223.51 153.35 248.09 283.49 170.14 210.88 Nb 8.85 7.95 12.14 8.78 7.54 15.97 8.23 13.94 9.35 8.95 11.27 Y 26.10 16.06 24.10 16.45 18.90 23.17 14.67 19.85 18.88 38.27 33.40 La 32.50 31.07 16.87 23.63 39.40 37.56 26.66 10.11 27.43 41.17 49.51 Ce 68.30 56.29 59.70 54.67 70.90 72.57 56.65 52.56 62.55 84.94 102.85 Pr 9.04 6.53 4.40 5.64 9.36 8.47 5.93 2.64 7.64 10.62 12.78 Nd 38.40 25.96 17.67 21.69 33.60 32.36 22.24 9.51 28.75 40.02 47.41 Sm 7.51 4.28 3.44 3.86 5.45 5.62 3.80 2.00 5.32 8.12 9.13 Eu 1.69 1.26 0.60 0.75 1.01 1.11 0.74 0.29 0.95 0.48 0.55 Gd 5.88 4.51 3.34 3.84 4.05 5.83 3.88 2.02 4.06 6.47 6.96 Tb 1.09 0.61 0.63 0.56 0.66 0.84 0.54 0.47 0.69 1.20 1.21 Dy 5.03 2.82 3.98 2.80 3.41 3.92 2.57 3.04 3.45 6.46 5.97 Ho 0.96 0.53 0.87 0.53 0.67 0.79 0.52 0.72 0.70 1.30 1.16 Er 2.46 1.66 2.76 1.78 1.94 2.47 1.63 2.08 1.85 3.59 3.13 Tm 0.45 0.26 0.50 0.30 0.31 0.39 0.25 0.42 0.34 0.66 0.55 Yb 2.50 1.70 3.27 1.97 2.17 2.64 1.74 2.71 2.16 4.07 3.37 Lu 0.36 0.29 0.53 0.35 0.35 0.45 0.24 0.64 0.46 0.76 0.65 Ba 961.00 918.94 487.63 891.22 1088.00 668.03 734.91 141.82 973.28 332.22 418.32 Hf 7.97 5.35 7.98 6.75 7.80 8.24 6.22 7.80 8.25 8.30 10.07 Ta 0.50 0.76 0.87 0.80 0.65 1.10 0.68 0.88 0.58 0.73 0.83 Pb 13.10 19.62 12.97 19.80 18.20 18.96 47.97 26.08 21.14 21.45 19.85 Th 6.95 5.92 5.84 9.02 8.84 13.21 18.43 10.22 7.86 19.05 17.66 U 1.81 2.65 2.44 2.99 2.71 2.82 2.13 2.60 1.97 1.97 3.01 ΣREE 176.17 137.75 118.58 122.36 173.28 175.02 127.39 89.19 146.35 209.85 245.23 LREE/
HREE8.41 10.14 6.46 9.10 11.78 9.10 10.20 6.37 9.67 7.56 9.66 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 索伦地区满克头鄂博组火山岩（MB2200）锆石Hf同位素分析结果
Table 3 Zircon Hf isotopic data for the volcanic rocks(MB2200)of Manketouebo Formation from Suolun area
测点号 t/Ma 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf* 2σm εHf(0) εHf(t) 2σ TDM1 TDM2 fLu/Hf 1 138 0.061979 0.001818 0.282867 0.000011 3.36 6.15 0.4 559 796 -0.95 2 138 0.053014 0.001596 0.282886 0.000010 4.02 6.92 0.4 528 750 -0.95 3 138 0.054904 0.001686 0.282806 0.000011 1.21 4.13 0.4 644 930 -0.95 4 138 0.045824 0.001269 0.282821 0.000011 1.73 4.52 0.4 616 899 -0.96 5 138 0.056810 0.001678 0.282887 0.000010 4.07 6.99 0.4 527 747 -0.95 6 138 0.051318 0.001520 0.282924 0.000012 5.39 8.24 0.4 471 664 -0.95 7 138 0.048658 0.001423 0.282847 0.000010 2.65 5.4 0.4 581 842 -0.96 8 138 0.062385 0.001863 0.282855 0.000010 2.95 5.76 0.4 576 822 -0.94 9 138 0.067899 0.002068 0.282813 0.000013 1.46 4.26 0.4 641 918 -0.94 10 138 0.059064 0.001683 0.282889 0.000011 4.14 6.97 0.4 525 745 -0.95 11 138 0.067034 0.002195 0.282817 0.000016 1.6 4.49 0.6 637 907 -0.93 12 138 0.074233 0.002512 0.282805 0.000021 1.16 4.06 0.7 661 936 -0.92
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周新华, 英基丰, 张连昌, 等.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约[J].地球科学, 2009, 34(1):1-10. http://mall.cnki.net/magazine/Article/DQKX200901002.htm 张超, 杨伟红, 和钟铧, 等.大兴安岭中南段塔尔气地区满克头鄂博组流纹岩年代学和地球化学研究[J].世界地质, 2014, 33(2):255-265. http://www.cqvip.com/QK/94166X/201402/50165528.html 纪政, 葛文春, 杨浩, 等.大兴安岭中段满克头鄂博组火山岩年代学与地球化学[J].吉林大学学报(地球科学版), 2015, (S1):206. http://cdmd.cnki.com.cn/Article/CDMD-10183-1014296204.htm 林强, 元钟宽.中国东北地区中生代火山岩的大地构造意义[J].地质科学, 1998, (2):129-139. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX802.000.htm 葛文春, 林强, 孙德有, 等.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据[J].岩石学报, 1999, 15(3):396-407. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98199903008 谢鸣谦.拼贴板块构造及其驱动机理——中国东北及邻区的大地构造演化[M].北京:科学出版社, 2000:137-150. Fan W M, Guo F, Wang Y J, et al. Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains, northeastern China[J]. Journal of Volcanology and Geothermal Research, 2003, 121(1):115-135. https://www.sciencedirect.com/science/article/pii/S0377027302004158
Meng Q R. What drove Late Mesozoic extension of the northern China-Mongolia tract?[J]. Tectonophysics, 2003, 369(3):155-174. https://www.sciencedirect.com/science/article/pii/S0040195103001951
蒋国源, 权恒. 大兴安岭根河、海拉尔盆地中生代火山岩[C]//中国地质科学院沈阳地质矿产研究所文集(17), 1988: 78. 赵国龙, 杨桂林, 王忠, 等.大兴安岭中南部中生代火山岩[J].北京:地质出版社, 1989:1-252. http://cdmd.cnki.com.cn/Article/CDMD-10491-2009153771.htm 邵济安, 牟保磊, 何国琦, 等.华北北部在古亚洲域与古太平洋域构造叠加过程中的地质作用[J].中国科学(地球科学), 1997, 27(5):390-394. http://www.oalib.com/paper/4151672 Ji Z, Ge W C, Wang Q H, et al. Petrogenesis of Early Cretaceous volcanic rocks of the Manketouebo Formation in the Wuchagou region, central Great Xing'an Range, NE China, and tectonic implications:geochronological, geochemical, and Hf isotopic evidence[J]. International Geology Review, 2016, 58(5):556-573. doi: 10.1080/00206814.2015.1095132
葛文春, 吴福元, 周长勇, 等.兴蒙造山带东段斑岩型Cu, Mo矿床成矿时代及其地球动力学意义[J].科学通报, 2007, 52(20):2407-2417. doi: 10.3321/j.issn:0023-074x.2007.20.012 Ge W C, Wu F Y, Zhou C Y, et al. Porphyry Cu-Mo deposits in the eastern Xing'an-Mongolian Orogenic Belt:Mineralization ages and their geodynamic implications[J]. Chinese Science Bulletin, 2007, 52(24):3416-3427. doi: 10.1007/s11434-007-0466-8
葛文春, 吴福元, 周长勇.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J].科学通报, 2005, 50(12):1239-1247. doi: 10.3321/j.issn:0023-074X.2005.12.015 Ge W, Wu F, Zhou C, et al. Emplacement age of the Tahe granite and its constraints on the tectonic nature of the Ergun block in the northern part of the Da Hinggan Range[J]. Chinese Science Bulletin, 2005, 50(18):2097-2105. doi: 10.1360/982005-207
Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30. doi: 10.1016/j.jseaes.2010.11.014
Wu F, Sun D, Li H, et al. A-type granites in northeastern China:age and geochemical constraints on their petrogenesis[J]. Chemical Geology, 2002, 187(1):143-173.
孙德有, 吴福元, 张艳斌.西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据[J].吉林大学学报(地球科学版), 2004, 34(2):174-181. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200402003 Xiao W J, Windley B F, Han C M, et al. End Permian to mid-Triassic termination of the southern Central Asian Orogenic Belt[J]. International Journal of Earth Sciences, 2009, 98(1):1189-1217.
Wu F Y, Zhao G C, Sun D Y, et al. The Hulan Group:its role in the evolution of the Central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences, 2007, 30(3):542-556. https://www.sciencedirect.com/science/article/pii/S136791200700034X
Anderson T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical geology, 2002, 192(1):59-79. https://www.sciencedirect.com/science/article/pii/S000925410200195X
Ludwig K. Users manual for Isoplot/Ex (rev. 2.49):A geochronological toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 2001:1-55. http://edu.wanfangdata.com.cn/Periodical/Detail/kxtb200316001
Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology[J]. Chemical Geology, 2006, 234(1):105-126. https://www.deepdyve.com/lp/university-of-chicago-press/2-7-ga-crustal-growth-in-the-north-china-craton-evidence-from-zircon-u-zCx5B0waK2
Veevers J J, Saeed A, Belousova E A, et al. U-Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton[J]. Earth-Science Reviews, 2005, 68(3):245-279. https://www.sciencedirect.com/science/article/pii/S001282520400056X
Yuan H L, Gao S, Dai M N, et al. Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICPMS[J]. Chemical Geology, 2008, 247(1):100-118. http://jcsservices.in/pdf/Huan_Fontaine_Chem_Geology.pdf
刘颖, 刘海臣.用ICP-MS准确测定岩石样品中的40余种微量元素[J].地球化学, 1996, 25(6):552-558. http://www.cnki.com.cn/Article/CJFDTotal-DQHX606.003.htm Belousova E, Griffin W L, O'Reilly S Y, et al. Igneous zircon:trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-622. doi: 10.1007/s00410-002-0364-7
Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological society of America bulletin, 1989, 101(5):635-643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2
Irvine T N J, Baragar W. A guide to the chemical classification of the common volcanic rocks[J]. Canadian Journal of Earth Sciences, 1971, 8(5):523-548. doi: 10.1139/e71-055
Peccerillo A, Taylor S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63-81. doi: 10.1007/BF00384745
Boynton W V. Geochemistry of the rare earth elements: Meteorite studies[C]//Henderson P. Rare Earth Elements Geochemistry. Amsterdam: Elsevier, 1984: 63-114.
Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313-345. doi: 10.1144/GSL.SP.1989.042.01.19
孙德有, 苟军, 任云生, 等.满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究[J].岩石学报, 2011, 27(10):3083-3094. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20111023&journal_id=ysxb 李鹏川, 李世超, 刘正宏, 等.内蒙古林西地区满克头鄂博组火山岩形成时代及构造环境[J].世界地质, 2016, 35(1):77-88. http://www.cqvip.com/QK/94166X/201601/668532841.html 司秋亮, 崔天日, 唐振, 等.大兴安岭中段柴河地区玛尼吐组火山岩年代学, 地球化学及岩石成因[J].吉林大学学报(地球科学版), 2015, (2):389-403. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb201502006 Ying J F, Zhou X H, Zhang L C, et al. Geochronological framework of Mesozoic volcanic rocks in the Great Xing'an Range, NE China, and their geodynamic implications[J]. Journal of Asian Earth Sciences, 2010, 39(6):786-793. doi: 10.1016/j.jseaes.2010.04.035
Zhang J H, Gao S, Ge W C, et al. Geochronology of the Mesozoic volcanic rocks in the Great Xing'an Range, northeastern China:implications for subduction-induced delamination[J]. Chemical Geology, 2010, 276(3):144-165. http://www.cas.cn/ky/kyjz/201010/W020101027324792058348.pdf
杜洋, 刘正宏, 崔维龙, 等.大兴安岭克一河地区满克头鄂博组火山岩形成时代, 地球化学特征及地质意义[J].世界地质, 2017, 36(1):54-65. http://cdmd.cnki.com.cn/Article/CDMD-10183-1014296204.htm Mcdonough W F, Sun S. The composition of the Earth[J]. Chemical Geology, 1995, 120(3):223-253. https://www.deepdyve.com/lp/elsevier/the-composition-of-the-earth-dbOgYb6Wlo
Taylor S R, McLennan S M. The continental crust:its composition and evolution[M]. London:Blackwell, 1985:57-72.
Wilson M. Igneous Petrogenesis[M]. London:Unwin Hywin, 1989.
Bea F, Fershtater G B, Corretge L G, et al. The geochemistry of phosphorus in granite rocks and the effect of aluminium[J]. Lithos, 1992:43-56. https://www.sciencedirect.com/science/article/pii/002449379290033U
吴福元, 李献华, 郑永飞, 等. Lu-Hf同位素体系及其岩石学应用[J].岩石学报, 2007(2):3-38. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200702002.htm Shao J A, Zang S X, Mou B L, et al. Extensional tectonics and asthenospheric upwelling in the orogenic belt:A case study from Hinggan-Mongolia orogenic belt[J]. Chinese Science Bulletin, 1994, 39(6):533-537. https://www.sciencedirect.com/science/article/pii/S0031920116300073
林强, 葛文春, 孙德有.中国东北地区中生代火山岩的大地构造意义[J].地质科学, 1998, 2:129-139. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX802.000.htm 林强, 葛文春, 曹林, 等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学, 2003, 32(3):208-222. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200303001.htm 邵济安, 张履桥.大兴安岭中南段中生代的构造热演化[J].中国科学(D辑), 1998, 28(3):193-200. http://www.oalib.com/paper/4151523 邵济安, 张履桥, 牟保磊.大兴安岭中生代伸展造山过程中的岩浆作用[J].地学前缘, 1999, 6(4):339-347 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy199904017 邵济安, 李献华, 张履桥, 等.南口-古崖居中生代双峰式岩墙群形成机制的地球化学制约[J].地球化学, 2001, 30(6):517-524. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqhx200106003 葛文春, 林强.大兴安岭中生代两类流纹岩成因的地球化学研究[J].地球科学:中国地质大学学报, 2000, 25(2):172-178. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002012.htm 葛文春, 李献华, 林强, 等.呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义[J].地质科学, 2001, 36(2):176-183. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200102005.htm 董玉, 葛文春, 杨浩, 等. 大兴安岭中段早白垩世白音高老组火山岩年代学与地球化学研究[C]//中国地球科学联合学术年会. 2014. 陈飞, 和钟铧, 张春蕾, 等.内蒙古塔尔气地区花岗斑岩的形成时代与岩石成因[J].地质通报, 2016, 35(5):776-789. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?file_no=20160513&flag=1 张旗.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?[J].岩石矿物学杂志, 2013, 32(1):113-128. http://www.oalib.com/paper/4337786 Xu W L, Ji W Q, Pei F P, et al. Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces, NE China:Chronologe, Geochemistry, and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2009, (3):392-402. https://www.researchgate.net/publication/316766787_Triassic_volcanism_along_the_eastern_margin_of_the_Xing'an_Massif_NE_China_Constraints_on_the_spatial-temporal_extent_of_the_Mongol-Okhotsk_tectonic_regime
赵大鹏, 雷建设, 唐荣余.中国东北长白山火山的起源:地震层析成像证据[J].科学通报, 2004, 49(14):1439-1446. doi: 10.3321/j.issn:0023-074X.2004.14.017 张旗.大陆花岗岩的地球动力学意义[J].岩石矿物学杂志, 2014, 33(4):785-798. http://www.cqvip.com/QK/94932X/201404/661725742.html 李宇, 丁磊磊, 许文良, 等.孙吴地区中侏罗世白云母花岗岩的年代学与地球化学:对蒙古-鄂霍茨克洋闭合时间的限定[J].岩石学报, 2015, 31(1):56-66. https://www.researchgate.net/profile/Wl_Xu/publication/279318920_Geochronology_and_geochemistry_of_muscovite_granite_in_Sunwu_area_NE_China_Implications_for_the_timing_of_closure_of_the_Mongol-Okhotsk_Ocean/links/5657c66b08ae4988a7b58335.pdf?origin=publication_list Hirose K. Melting experiments on lherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts[J]. Geology, 1997, 25(1):42-44. doi: 10.1130/0091-7613(1997)025<0042:MEOLKU>2.3.CO;2
黄始琪, 董树文, 张福勤, 等.蒙古-鄂霍茨克构造带中段构造变形及动力学特征[J].地球学报, 2014, 35(4):415-424. doi: 10.3975/cagsb.2014.04.03
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