Zircon U-Pb ages and geochemical characteristics of the quartz monzonite diorite rocks from Hanmiao area in the southern segment of the Da Hinggan Mountains
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摘要:
为确定罕庙地区石英二长闪长岩的形成时代、成因及地质意义,对罕庙地区石英二长闪长岩体进行了岩相学、LAMC-ICP-MS锆石U-Pb年龄及地球化学研究。结果表明,石英二长闪长岩中的锆石为岩浆成因,206Pb/238U年龄加权平均值为134±1Ma,侵入时代属于早白垩世晚期。石英二长闪长岩中SiO2含量为63.44%~68.96%,K2O含量为2.04%~3.84%,Na2O/K2O值介于0.47~1.17之间,铝饱和指数A/CNK介于2.12~2.55之间,属于钙碱性-高钾钙碱性过铝质花岗岩类。微量元素特征为富集大离子亲石元素(如Rb、K)和活泼不相容元素(如Th、U),强烈亏损高场强元素(如Nb、Ta、P、Ti)。结合区域构造演化背景,该岩体受俯冲流体改造,与早白垩世晚期古太平洋板块斜向俯冲于欧亚大陆之下的弧后伸展减薄等综合作用有关。
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关键词:
- 石英二长闪长岩 /
- 地球化学 /
- LA-MC-ICP-MS锆石U-Pb年龄 /
- 大兴安岭
Abstract:In order to determine the geochronology, petrogenesis and tectonic background of the quartz monzonite diorite rocks in Hanmiao area, the authors conducted the research on petrology by means of LA-MC-ICP-MS zircon U-Pb geochronology and geochemistry. The results show that the zircons from the quartz monzonite diorite rocks are magmatic zircons, and the zircon 206Pb/238U dating yielded 134±1Ma(n=22, MSWD=0.42), suggesting late Early Cretaceous. The values of SiO2, K2O and Na2O/K2O are 63.44%~68.96%, 2.04%~3.84% and 0.47~1.17 respectively. The aluminum saturation indexes (A/CNK) range from 2.12 to 2.55. The rocks thus belong to calc-alkaline-high-K calc-alkaline series. The rocks are enriched in LILE (Rb, K) and incompatible elements(Th, U), strongly depleted in HFSE such as Nb, Ta, P and Ti. Combined with the study of regional tectonics the authors hold that the quartz monzonite diorite rocks might have been affected by subducted slab fluids. It was closely related to back-arc extension tectonics and lithospheric thinning after the subduction of Paleo-Pacific plate towards Eurasia plate.
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致谢: 野外工作中得到吉林大学地质调查研究院内蒙项目组的大力支持,审稿专家认真审阅并提出建设性意见,在此一并表示诚挚的感谢。
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图 6 SiO2-K2O图解[14]
Figure 6. SiO2-K2O diagram of the rocks
图 7 A/CNK-A/NK图解[15]
Figure 7. A/CNK-A/NK diagram of the rocks
图 9 SiO2-K2O/P2O5(a)和SiO2-K2O/TiO2(b)图解[18]
Figure 9. SiO2-K2O/P2O5(a) and SiO2-K2O/TiO2(b) diagrams of quartz monzonite diorite
图 10 Th/Zr-Nb/Zr(a)和Nb/Y-Rb/Y图解(b)[24]
Figure 10. Th/Zr-Nb/Zr(a) and Nb/Y-Rb/Y(b) diagrams
图 11 石英二长闪长岩(Y+Nb)-Rb(a)和Y-Nb图解(b)[26]
Figure 11. (Y+Nb)-Rb(a) and Y-Nb diagrams (b) of quartz monzonite diorite
表 1 石英二长闪长岩LA-MC-ICP-MS锆石U-Th-Pb同位素分析结果
Table 1 LA-MC-ICP-MS zircon U-Th-Pb analytical results of quartz monzonite diorite
测点编号 含量/10-6 Th/U 同位素比值 年龄/Ma Pb U Th 206Pb/238U 1σ 207Pb/235U 1σ 207Pb/206Pb 1σ 206Pb/238U 1σ 207Pb/235U 1σ 207Pb/206Pb 1σ 1 25 1137 850 0.75 0.0211 0.00021 0.1423 0.0023 0.0489 0.0007 135 1 135 2 142 34 2 11 549 222 0.40 0.0210 0.00024 0.1409 0.0052 0.0487 0.0017 134 2 134 5 135 82 3 13 603 227 0.38 0.0211 0.00022 0.1416 0.0034 0.0486 0.0011 135 1 134 3 131 55 4 10 478 169 0.35 0.0211 0.00022 0.1406 0.0036 0.0484 0.0012 134 1 134 3 119 59 5 17 786 320 0.41 0.0212 0.00022 0.1419 0.0025 0.0486 0.0008 135 1 135 2 130 38 6 10 423 162 0.38 0.0209 0.00022 0.1403 0.0024 0.0488 0.0008 133 1 133 2 138 38 7 21 919 577 0.63 0.0211 0.00024 0.1410 0.0042 0.0485 0.0011 135 2 134 4 122 55 8 11 505 179 0.35 0.0212 0.00022 0.1428 0.0031 0.0489 0.0010 135 1 136 3 143 48 9 10 480 168 0.35 0.0211 0.00022 0.1397 0.0045 0.0481 0.0015 134 1 133 4 104 74 10 14 679 264 0.39 0.0212 0.00022 0.1408 0.0027 0.0483 0.0009 135 1 134 3 112 43 11 11 536 208 0.39 0.0210 0.00021 0.1409 0.0030 0.0486 0.0010 134 1 134 3 126 49 12 13 603 237 0.39 0.0210 0.00022 0.1407 0.0032 0.0485 0.0011 134 1 134 3 125 52 13 21 967 408 0.42 0.0209 0.00021 0.1413 0.0022 0.0492 0.0007 133 1 134 2 155 33 14 14 642 205 0.32 0.0212 0.00021 0.1416 0.0034 0.0484 0.0011 135 1 134 3 119 54 15 13 610 225 0.37 0.0210 0.00021 0.1413 0.0030 0.0489 0.0010 134 1 134 3 144 49 16 18 818 320 0.39 0.0211 0.00022 0.1403 0.0028 0.0482 0.0009 135 1 133 3 111 45 17 14 633 408 0.64 0.0212 0.00021 0.1423 0.0042 0.0488 0.0014 135 1 135 4 137 67 18 11 473 241 0.51 0.0210 0.00022 0.1406 0.0035 0.0486 0.0011 134 1 134 3 131 53 19 12 583 248 0.43 0.0208 0.00021 0.1400 0.0028 0.0488 0.0009 133 1 133 3 137 44 21 13 621 289 0.46 0.0209 0.00021 0.1403 0.0029 0.0487 0.0010 133 1 133 3 132 46 22 17 765 504 0.66 0.0208 0.00021 0.1399 0.0036 0.0487 0.0012 133 1 133 3 134 58 23 5 217 122 0.56 0.0207 0.00024 0.1399 0.0131 0.0491 0.0046 132 2 133 12 152 219 表 2 石英二长闪长岩主量、微量和稀土元素分析结果
Table 2 Major, trace elements and REE compositions of quartz monzonite diorite
样品号 PM102-25YQ1 PM102-25YQ2 PM102-25YQ3 PM102-12YQ PM102-14YQ 样品号 PM102-25YQ1 PM102-25YQ2 PM102-25YQ3 PM102-12YQ PM102-14YQ Al2O3 15.16 14.01 14.71 14.29 14.6 Zr 277.72 200.12 259.35 249.59 241.40 CaO 1.24 1.56 2.05 1.11 1.22 Nb 13.84 7.48 8.98 11.84 10.94 Fe2O3 5.63 6.98 6.68 5.44 4.37 Ba 1077.10 407.69 364.62 646.60 680.74 K2O 3.84 2.17 2.04 3.03 3.38 La 32.12 22.09 26.72 30.36 26.62 MgO 1.3 2.48 2.9 1.44 1.33 Ce 60.18 46.02 54.43 61.55 53.55 MnO 0.09 0.11 0.11 0.09 0.1 Pr 7.91 5.72 7.00 7.57 6.74 Na2O 2.08 2.18 2.39 1.46 1.58 Nd 29.85 22.31 27.82 29.04 25.51 P2O5 0.14 0.14 0.16 0.08 0.08 Sm 6.13 5.06 6.17 6.09 5.30 SiO2 65.6 66.1 63.44 67.88 68.96 Eu 1.45 1.09 1.23 1.18 1.11 TiO2 0.67 0.67 0.71 0.68 0.7 Gd 5.81 4.87 5.83 5.86 5.31 FeO 2.66 1.31 2.76 1.99 1.98 Tb 0.86 0.74 0.86 0.88 0.79 H2O+ 3.4 0.3 3.7 4.32 2.62 Dy 5.18 4.49 5.18 5.36 4.75 烧失量 4.26 3.6 4.83 4.5 3.68 Ho 1.12 0.97 1.11 1.15 1.03 总计 101.8 98.01 101.63 101.81 100.92 Er 3.44 2.85 3.33 3.44 3.10 Na2O+K2O 4.49 4.96 5.92 4.35 4.42 Tm 0.54 0.44 0.50 0.53 0.49 Na2O/K2O 0.48 0.47 0.54 1.01 1.17 Yb 3.59 2.96 3.35 3.54 3.22 A/CNK 2.55 2.36 2.12 2.37 2.27 Lu 0.53 0.43 0.48 0.49 0.47 Li 100.65 70.91 72.96 77.78 73.58 Y 30.25 25.46 28.79 29.80 26.53 Be 2.60 3.14 2.68 3.36 1.97 Hf 7.93 5.83 7.49 7.70 7.35 V 96.86 108.10 131.26 141.15 132.29 Ta 1.01 0.60 0.69 1.05 0.88 Cr 35.96 125.49 162.01 93.94 85.17 Th 11.51 8.02 9.10 13.91 12.56 Co 8.14 12.54 16.55 5.64 4.03 U 2.93 2.05 2.21 3.30 2.91 Ni 19.12 76.24 102.73 46.47 33.43 LREE/HREE 6.39 6.21 6.53 5.76 5.97 Ga 24.70 19.52 24.03 23.49 21.83 (La/Yb)N 6.16 5.93 6.41 5.35 5.72 Rb 136.65 90.98 106.54 150.61 136.09 δEu 0.60 0.63 0.73 0.66 0.62 Sr 179.18 179.67 229.60 147.90 143.88 δCe 0.97 0.96 0.90 0.98 0.95 -
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(3/4):542-556. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200801002024.htm
欧阳荷根.大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景[D].中国地质大学(北京)博士学位论文, 2013. Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids innortheastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30. doi: 10.1016/j.jseaes.2010.11.014
孟恩, 许文良, 杨德彬, 等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义[J].岩石学报, 2011, 27(4):1209-1226. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201104029.htm Wang T, Zheng Y D, Zhang J J. Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia:Perspectives from metamorphic core complexes[J].Tectonics, 2011, 30(6):7-33. http://cn.bing.com/academic/profile?id=efe40333885ec524fcd656eea115a562&encoded=0&v=paper_preview&mkt=zh-cn
邵济安, 张履桥, 肖庆辉, 等.中生代大兴安岭的隆起——一种可能的陆内造山机制[J].岩石学报, 2005, 3:789-794. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200503018 邱瑞照, 李廷栋, 周肃, 等.中国大陆岩石圈物质组成及演化[M].北京:地质出版社, 2006:288. 邹滔.内蒙古敖仑花斑岩型钼矿床岩浆演化与成矿机理研究[D].昆明理工大学博士学位论文, 2012. 李怀坤, 耿建珍, 郝爽, 等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J].矿物学报, 2009, 29(1):600-601. http://d.old.wanfangdata.com.cn/Conference/7298171 李怀坤, 朱士兴, 相振群, 等.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束[J].岩石学报, 2010, 26(7):2131-2141. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201007015 Ludwig K R.User's Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Execl[J]. Berkeley Geochronolgy Center Special Publication, 2003, 4:1-70. https://searchworks.stanford.edu/view/6739593
柳小明.华北克拉通中生代壳幔交换作用的地球化学研究[D].西北大学硕士学位论文, 2004. 李长民.锆石成因矿物学与锆石微区定年综述[J].地质调查与研究, 2009, 33(3):161-174. doi: 10.3969/j.issn.1672-4135.2009.03.001 Peccerillo A, Taylor A R.Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58:63-81. doi: 10.1007/BF00384745
Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological Society of American Bulletin, 1989, 101:635-643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2
Weaver B L.The origin of Ocean Island Basalt end member compositions:trace elelment and Isotopic constraints[J].Earth Planet. Sci Lett. 1991, 104:381-397. doi: 10.1016/0012-821X(91)90217-6
马星华, 陈斌, 赖勇, 等.内蒙古敖仑花斑岩钼矿床成岩成矿年代学及地质意义[J].岩石学报, 2009, 25(11):2939-2950. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200911023 吴华英, 张连昌, 周新华, 等.大兴安岭中段晚中生代安山岩年代学和地球化学特征及成因分析[J].岩石学报, 2008, 24(6):1339-1352. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200806017 陈义贤等著.辽西及邻区中生代火山岩——年代学、地球化学和构造背景[M].北京:地震出版社, 1997. Gill J B. Orogenic andesites and plate tectonics[M]. New York:Springer, 1981:385-389.
Sun S S, Mcdonough W F. Chemical and Isotopic Systematics of Oceanic Basaits: Implication for Mantle Composition and Processes[M]. GeologicalSociety Special Publication, 1989: 313-345.
Tatsumi Y, Hamilton D L, Nesbitt R W. Chemical characteristics of fluid phase released from a subductedlithosphere and origin of arc magmas:evidence from high pressure experiments and natural rocks[J]. Journal of Volcanology and Geothermal Research, 1986, 29(1):293-309. http://www.sciencedirect.com/science/article/pii/0377027386900491
Arculus R J, Powell R.Source component mixing in theregion of arc magma generation[J]. Journal of Geophysical Research, 1986, 91(6):5913-5926. doi: 10.1029/JB091iB06p05913/abstract
Kepezhinskas P, McDermott F, Defant M J, et al. Trace element and Sr-Nd-Pb isotopic constraints on athreecomponent model of Kamchatka arc petrogenesis[J]. Geochimica et Cosmochimica Acta, 1997, 61(3):577-600. doi: 10.1016/S0016-7037(96)00349-3
郭锋, 范蔚茗, 王岳军, 等.大兴安岭南段晚中生代双峰式火山作用[J].岩石学报, 2001, 17(1):161-168. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200101017 Pearce J A, Harris B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretations of granitic rocks[J]. J. Petrol., 1984, 25:956-983. doi: 10.1093/petrology/25.4.956
邵济安, 张履桥.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):339-346. doi: 10.3321/j.issn:1005-2321.1999.04.017 林强, 葛文春, 孙德有, 等.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, 2:3-13. http://cdmd.cnki.com.cn/Article/CDMD-10183-2008061652.htm 许文良, 王枫, 裴福萍, 等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报, 2013, 29(2):339-353. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302001 Maruyama S.Pacific-type orogeny revisited:Miyashirotype orogeny proposed[J]. Island Arc, 1997, 6:91-120. doi: 10.1111/iar.1997.6.issue-1
辽宁省第二区域地质测量队四连.中华人民共和国区域地质矿产报告书(矿产部分): 1: 20万协里府幅(L-50-XXXⅥ), 1971. 安庆河, 何长胜, 刘传宝, 等.内蒙古自治区赤峰市1: 5万区域矿产地质调查报告.内蒙古自治区第十地质矿产勘查开发院, 2009.