张广才岭地块早-中二叠世镁铁质侵入岩体的年代学、地球化学及岩石成因

冯光英; 刘燊; 牛晓露; 杨经绥

doi:10.3799/dqkx.2018.721

张广才岭地块早-中二叠世镁铁质侵入岩体的年代学、地球化学及岩石成因

doi: 10.3799/dqkx.2018.721

1.
地幔研究中心, 国土资源部深地动力学重点实验室, 中国地质科学院地质研究所, 北京 100037
2.
大陆动力学国家重点实验室, 西北大学地质学系, 陕西西安 710069

基金项目:

国家自然科学基金项目 41573022

国家自然科学基金项目 41773029

国家自然科学基金项目 41373029

国家自然科学基金项目 41672063

国土资源部公益性行业专项项目 201511022

国家自然科学基金项目 41720104009

地质调查项目 DD20160023-01

国家自然科学基金项目 41373028

详细信息

作者简介:
冯光英(1983-), 女, 副研究员, 博士, 从事岩浆岩及地幔橄榄岩岩石学与地球化学研究

中图分类号: P597
计量
- 文章访问数: 3215
- HTML全文浏览量: 1289
- PDF下载量: 39
- 被引次数: 0
出版历程
- 收稿日期: 2017-12-20
- 刊出日期: 2018-04-15

Geochronology, Geochemistry and Petrogenesis of Early-Middle Permian Mafic Intrusion in Zhangguangcai Range, China

1.
Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

摘要

摘要: 双凤山基性侵入岩体位于松嫩-张广才岭地块南缘，其岩石组成主要为橄榄辉长岩.锆石LA-ICP-MS U-Pb定年显示该岩体形成于279±4 Ma.岩石矿物组成主要为橄榄石、单斜辉石、斜方辉石、高An值（80.1~87.9）斜长石以及以反应边形式存在的角闪石，矿物学特征指示其母岩浆为经历过充分流体交代的富水岩浆.全岩主微量元素组成揭示其源区物质组成为石榴子石二辉橄榄岩，部分熔融程度约20%，岩浆演化过程中经历了斜长石堆晶作用以及斜方辉石的结晶分异作用.全岩Sr-Nd同位素及锆石Hf同位素研究显示其（⁸⁷Sr/⁸⁶Sr）_i=0.705 2~0.706 1，并具有正的ε_Nd（t）值（0.9~1.3）和ε_Hf（t）值（0~10.2），表明其来源于亏损的地幔源区，并且岩浆上升过程中没有经历明显的地壳混染.微量元素和同位素特征综合反映岩浆源区经历了古亚洲洋俯冲沉积物熔体和流体交代作用的改造，但起主导作用的是流体.其地球化学特征总体显示MORB以及弧型玄武岩过渡的特征，暗示其形成于弧后伸展环境.研究区基性侵入岩地幔源区的不均一性主要受到古亚洲洋多期次俯冲作用析出熔/流体对上覆地幔楔不同程度的改造.
- 早-中二叠世 /
- 松嫩-张广才岭地块 /
- 镁铁质侵入岩 /
- 岩石成因 /
- 地球化学
Abstract: The Shuangfengshan mafic intrusion crops out in the southern margin of the Songnen-Zhangguangcai range. It is predominantly made of olivine gabbro, which yielded a crystallization age of 279±4 Ma (Early-Middle Permian). These rocks consist mainly of olivine, pyroxene, high-An (80.1-87.9) plagioclase and hornblende as reaction rim. The features of these minerals indicate a high-H₂O or water-saturated parental magma which experienced fluid metasomatism in the mantle source. Major and trace elements studies suggest that the mafic magma was derived from partial melting (~20%) of depleted garnet-lherzolite mantle source. Variable degrees of plagioclase accumulation and orthopyroxene crystal fractionation occurred in the process of magma evolution. They are also characterized by relatively low Sr isotopic ratio (0.705 2-0.706 1), positive ε_Nd(t) (0.9-1.3) and ε_Hf(t) (0-10.2) values, confirming that the Shuangfengshan mafic magma was derived from depleted mantle source and apparent crustal contamination was not found during magma upwelling. Combining trace elemental and isotopic results suggest that the parental magmas were likely derived from mantle wedge metasomatized by sedimentary melt and fluid from the subducted Paleo-Asian slab. Moreover, these rocks display transitional properties of MORB and arc basalt, conforming that the studied olivine gabbros were probably formed in back-arc extensional environment. And the mantle heterogeneity beneath the studied area was probably reduced by the multi-stage Paleozoic subduction of the Paleo-Asian Ocean.
- Early-Middle Permian /
- Songnen-Zhangguangcai range /
- mafic intrusion /
- petrogenesis /
- geochemistry

HTML全文

图 1 中亚造山带(a)及东北地区(b)构造简图；双凤山镁铁质侵入岩区域地质简图(c)

图b底图据Guo et al.(2016)；图c据吉林省地质局(1978)编区域地质调查报告辽源市幅

Fig. 1. Simplified tectonic maps of the Central Asian orogenic belt (a) and Northeast China (b) and simplified geological map of the studied area (c)

下载: 全尺寸图片幻灯片

图 2 双凤山橄榄辉长岩显微照片(a, b)及电子探针背散射电子图像(c, d)

Ol.橄榄石；Pl.斜长石；Cpx.单斜辉石；Opx.斜方辉石；Prg.韭闪石

Fig. 2. Photomicrographs (a, b) and back-scattered electron images (c, d) of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 3 双凤山橄榄辉长岩角闪石分类

图a底图据文献Leake et al.(1997)；图b底图据Beard and Barker(1989)

Fig. 3. Classification of hornblende of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 4 双凤山橄榄辉长岩代表性锆石阴极发光图及LA-ICP-MS U-Pb谐和年龄

Fig. 4. Representative cathodoluminescence (CL) images and the LA-ICP-MS U-Pb age for the zircon grains from the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 5 双凤山橄榄辉长岩TAS图解(a)、SiO₂-K₂O图解(b)、稀土元素配分模式图(c)及微量元素原始地幔标准化图解(d)

张广才岭构造带早二叠世基性火山岩和酸性火山岩主量元素数据引自Meng et al.(2011)；图d据Sun and McDonough(1989)

Fig. 5. TAS (a), SiO₂ vs. K₂O (b), chondrite-normalized REE patterns (c) and primitive mantle-normalized spider diagrams (d) of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 6 双凤山橄榄辉长岩Al₂O₃-Na₂O以及Al₂O₃-Eu/^*Eu图解

Fig. 6. Al₂O₃ vs. Na₂O (a) and Al₂O₃ vs. Eu/^*Eu (b) diagrams of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 7 双凤山橄榄辉长岩Sr-Nd-Hf同位素组成

延吉地区二叠纪基性侵入岩数据引自Guo et al.(2016)；三叠纪红旗岭橄榄辉石岩数据冯光英等(2011)；早侏罗世大稗子沟辉绿玢岩数据来自作者未发表数据；East CAOB.中亚造山带东段；YFTB.燕山褶皱系

Fig. 7. Sr-Nd isotopic compositions of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 8 双凤山橄榄辉长岩La/Yb-Sm/Yb (a)和Gd/Yb-Dy/Yb (b)图解

Fig. 8. La/Yb vs. Sm/Yb (a) and Gd/Yb vs. Dy/Yb (b) diagrams of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 9 双凤山橄榄辉长岩Th/Sm-Th/Ce (a), Th/Yb-Ba/La (b), Ba/La-ε_Nd(t) (c)和Ba/Nb-ε_Nd(t)(d)图解

亏损地幔(DM)的Nd同位素组成据贺根山蛇绿岩套中基性岩组分及内蒙古大石寨弧玄武岩(Miao et al., 2008；郭锋等，2009)；沉积物熔/流体的Nd同位素组成据全球海洋沉积物(GLOSS, Plank and Langmuir, 1998)；MORB据Sun and McDonough(1989)；延吉地区早中二叠世基性侵入岩据Guo et al.(2016)；其他参数参见Guo et al.(2016)

Fig. 9. Th/Sm vs. Th/Ce (a), Th/Yb vs. Ba/La (b), Ba/La-ε_Nd(t) (c) and Ba/Nb-ε_Nd(t) diagrams of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

图 10 双凤山橄榄辉长岩构造判别图

a.Hf/3-Th-Ta图解，据Wood(1980)；b.Al₂O₃-MgO-FeO^T图解，据Pearce et al.(1977)

Fig. 10. Tectonic discrimination diagrams of the Shuangfengshan olivine gabbros

下载: 全尺寸图片幻灯片

参考文献(85)

[1]	Beard, J.S., Barker, F., 1989.Petrology and Tectonic Significance of Gabbros, Tonalites, Shoshonites, and Anorthosites in a Late Paleozoic Arc-Root Complex in the Wrangellia Terrane, Southern Alaska.The Journal of Geology, 97(6):667-683. https://doi.org/10.1086/629351
[2]	Crawford, A.J., Falloon, T.J., Eggins, S., 1987.The Origin of Island Arc High-Alumina Basalts.Contributions to Mineralogy and Petrology, 97(3):417-430. https://doi.org/10.1007/bf00372004
[3]	Danyushevsky, L.V., Carroll, M.R., Falloon, T.J., 1997.Origin of High-An Plagioclase in Tongan High-Ca Boninites:Implications for Plagioclase Melt Equilibria at Low P(H₂O).The Canadian Mineralogist, 35(2):313-326 http://www.mendeley.com/research/origin-highan-plagioclase-tongan-highca-boninites-implications-plagioclasemelt-equilibria-low-ph2o/
[4]	Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665. https://doi.org/10.1038/347662a0
[5]	Deng, J.F., 1987.Petrographical Facies Equilibrium and Petrogenesis.Wuhan College of Geology Press, Wuhan, 45-63 (in Chinese).
[6]	Duncan, A.R., 1987.The Karoo Igneous Province-A Problem Area for Inferring Tectonic Setting from Basalt Geochemistry.Journal of Volcanology and Geothermal Research, 32(1-3):13-34. https://doi.org/10.1016/0377-0273(87)90034-5
[7]	Elhlou, S., Belousova, E., Griffin, W.L., et al., 2006.Trace Element and Isotopic Composition of GJ-Red Zircon Standard by Laser Ablation.Geochimica et Cosmochimica Acta, 70(18):A158. https://doi.org/10.1016/j.gca.2006.06.1383
[8]	Feng, G.Y., Liu, S., Feng, C.X., et al., 2011.Zircon U-Pb Age, Sr-Nd-Hf Isotope Geochemistry and the Petrogenesis of the Ultramafic Pluton in Hongqiling, Jilin Province.Acta Petrologica Sinica, 27(6):1594-1606 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201106003.htm
[9]	Fournelle, J., Marsh, B.D., 1991.Shishaldin Volcano-Aleutian High-Alumina Basalts and the Question of Plagioclase Accumulation.Geology, 19(3):234-237.https://doi.org/10.1130/0091-7613(1991)019<0234:svahab>2.3.co;2 doi: 10.1130/0091-7613(1991)019<0234:svahab>2.3.co;2
[10]	Ge, M.H., Zhang, J.J., Liu, K., et al., 2016.Geochemistry and Geochronology of the Blueschist in the Heilongjiang Complex and Its Implications in the Late Paleozoic Tectonics of Eastern NE China.Lithos, 261:232-249. https://doi.org/10.1016/j.lithos.2015.11.019
[11]	Ge, S.S., Zhai, M.G., Safonova, I., et al., 2015.Whole-Rock Geochemistry and Sr-Nd-Pb Isotope Systematics of the Late Carboniferous Volcanic Rocks of the Awulale Metallogenic Belt in the Western Tianshan Mountains (NW China):Petrogenesis and Geodynamical Implications.Lithos, 228-229:62-77. https://doi.org/10.1016/j.lithos.2015.04.019
[12]	Guo, F., Fan, W.M., Li, C.W., et al., 2009.Early Paleozoic Subduction of the Paleo-Asian Ocean:Geochronological and Geochemical Evidence from the Dashizhai Basalts, Inner Mongolia.Science in China (Earth Sciences), 39 (5):569-579 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg200907006&dbname=CJFD&dbcode=CJFQ
[13]	Guo, F., Li, H.X., Fan, W.M., et al., 2015.Early Jurassic Subduction of the Paleo-Pacific Ocean in NE China:Petrologic and Geochemical Evidence from the Tumen Mafic Intrusive Complex.Lithos, 224-225:46-60. https://doi.org/10.1016/j.lithos.2015.02.014
[14]	Guo, F., Li, H.X., Fan, W.M., et al., 2016.Variable Sediment Flux in Generation of Permian Subduction-Related Mafic Intrusions from the Yanbian Region, NE China.Lithos, 261:195-215. https://doi.org/10.1016/j.lithos.2015.11.030
[15]	Guo, K.C., Zhang, W.L., Yang, X.P., et al., 2011.Origin of Early Permian A-Type Granite in the Wudaogou Area, Heihe City.Journal of Jilin University (Earth Science Edition), 41(4):1077-1083 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ201104017.htm
[16]	Hofmann, A.W., 1997.Mantle Geochemistry:The Message from Oceanic Volcanism.Nature, 385(6613):219-229. https://doi.org/10.1038/385219a0
[17]	Hou, K.J., Li, Y.H., Tian, Y.R., 2009.In Situ U-Pb Zircon Dating Using Laser Ablation-Multi Ion Counting-ICP-MS.Mineral Deposits, 28(4):481-492 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200904009.htm
[18]	Jian, P., Liu, D.Y., Kröner, A., et al., 2008.Time Scale of an Early to Mid-Paleozoic Orogenic Cycle of the Long-Lived Central Asian Orogenic Belt, Inner Mongolia of China:Implications for Continental Growth.Lithos, 101(3-4):233-259. https://doi.org/10.1016/j.lithos.2007.07.005
[19]	Johnson, K.T.M., 1998.Experimental Determination of Partition Coefficients for Rare Earth and High-Field-Strength Elements between Clinopyroxene, Garnet, and Basaltic Belt at High Pressures.Contributions to Mineralogy and Petrology, 133:60-68. doi: 10.1007/s004100050437
[20]	Leake, B.E., Woolley, A.R., Arps, C.E.S., et al., 1997.Nomenclature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names.Mineralogical Magazine, 35:219-246. https://doi.org/10.1180/minmag.1997.061.405.13
[21]	Liu, S., Hu, R.Z., Gao, S., et al., 2010.Zircon U-Pb Age and Sr-Nd-Hf Isotope Geochemistry of Permian Granodiorite and Associated Gabbro in the Songliao Block, NE China and Implications for Growth of Juvenile Crust.Lithos, 114(3-4):423-436. https://doi.org/10.1016/j.lithos.2009.10.009
[22]	Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004
[23]	Ludwig, K.R., 2003.User's Manual for Isoplot/Ex, Version 3.00.A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication, Berkeley, 4:1-70.
[24]	McKenzie, D., O'Nions, R.K., 1991.Partial Melt Distributions from Inversion of Rare Earth Element Concentrations.Journal of Petrology, 32(5):1021-1091. https://doi.org/10.1093/petrology/32.5.1021
[25]	Meng, E., Xu, W.L., Pei, F.P., et al., 2011.Permian Bimodal Volcanism in the Zhangguangcai Range of Eastern Heilongjiang Province, NE China:Zircon U-Pb-Hf Isotopes and Geochemical Evidence.Journal of Asian Earth Sciences, 41(2):119-132. https://doi.org/10.1016/j.jseaes.2011.01.005
[26]	Meng, E., Xu, W.L., Yang, D.B., et al., 2008.Chronology of Late Paleozoic Volcanism in Eastern and Southeastern Margin of Jiamusi Massif and Its Tectonic Implications.Chinese Science Bulletin, 53(8):956-965 (in Chinese).
[27]	Meng, J., Liu, X.Y., Liang, Y.H., et al., 2017.U-Pb Dating and Trace Elements Composition of Tadong Group from Jilin Province and Their Geological Implication.Earth Science, 42(4):502-510 (in Chinese with English abstract).
[28]	Miao, L.C., Fan, W.M., Liu, D.Y., et al., 2008.Geochronology and Geochemistry of the Hegenshan Ophiolitic Complex:Implications for Late-Stage Tectonic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China.Journal of Asian Earth Sciences, 32(5-6):348-370. https://doi.org/10.1016/j.jseaes.2007.11.005
[29]	Mitchell, J.N., Scoates, J.S., Frost, C.D., 1995.High-Al Gabbros in the Laramie Anorthosite Complex, Wyoming:Implications for the Composition of Melts Parental to Proterozoic Anorthosite.Contributions to Mineralogy and Petrology, 119(2-3):166-180. https://doi.org/10.1007/s004100050034
[30]	O'Neill, H.S.C., Jenner, F.E., 2012.The Global Pattern of Trace-Element Distributions in Ocean Floor Basalts.Nature, 491(7426):698-704. https://doi.org/10.1038/nature11678
[31]	Panjasawatwong, Y., Danyushevsky, L.V., Crawford, A.J., et al., 1995.An Experimental Study of the Effects of Melt Composition on Plagioclase-Melt Equilibria at 5 and 10 kbar:Implications for the Origin of Magmatic High-An Plagioclase.Contributions to Mineralogy and Petrology, 118(4):420-432. https://doi.org/10.1007/s004100050024
[32]	Peacock, S.M., 1993.The Importance of Blueschist→Eclogite Dehydration Reactions in Subducting Oceanic Crust.Geological Society of America Bulletin, 105(5):684-694.https://doi.org/10.1130/0016-7606(1993)105<0684:tiobed>2.3.co;2 doi: 10.1130/0016-7606(1993)105<0684:tiobed>2.3.co;2
[33]	Pearce, T.H., Gorman, B.E., Birkett, T.C., 1977.The Relationship between Major Element Chemistry and Tectonic Environment of Basic and Intermediate Volcanic Rocks.Earth and Planetary Science Letters, 36(1):121-132. https://doi.org/10.1016/0012-821x(77)90193-5
[34]	Pei, F.P., Wang, Z.W., Cao, H.H., et al., 2014.Petrogenesis of the Early Paleozoic Tonalite in the Central Jilin Province:Evidence from Zircon U-Pb Chronology and Geochemistry.Acta Petrologica Sinica, 30(7):2009-2019 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201407014.htm
[35]	Pei, F.P., Zhang, Y., Wang, Z.W., et al., 2016.Early-Middle Paleozoic Subduction-Collision History of the South-Eastern Central Asian Orogenic Belt:Evidence from Igneous and Metasedimentary Rocks of Central Jilin Province, NE China.Lithos, 261:164-180. https://doi.org/10.1016/j.lithos.2015.12.010
[36]	Plank, T., Langmuir, C.H., 1998.The Chemical Composition of Subducting Sediment and Its Consequences for the Crust and Mantle.Chemical Geology, 145(3-4):325-394. https://doi.org/10.1016/s0009-2541(97)00150-2
[37]	Polat, A., Appel, P.W.U., Fryer, B.J., 2011.An Overview of the Geochemistry of Eoarchean to Mesoarchean Ultramafic to Mafic Volcanic Rocks, SW Greenland:Implications for Mantle Depletion and Petrogenetic Processes at Subduction Zones in the Early Earth.Gondwana Research, 20(2-3):255-283. https://doi.org/10.1016/j.gr.2011.01.007
[38]	Rollinson, H. R., 1993. Using Geochemical Data: Evaluation, Presentation, Interpretation. Longman Scientific & Technical, Harlow, United Kindom, 352.
[39]	Sengör, A.M.C., Natal'in, B.A., Burtman, V.S., 1993.Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia.Nature, 364:299-307. doi: 10.1038/364299a0
[40]	Shao, J.A., Li, Y.F., Tang, K.D., 2013.Restoration of the Orogenic Processes of Zhangguangcai Range.Acta Petrologica Sinica, 29(9):2959-2970 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20130901
[41]	Sinton, C.W., Christie, D.M., Coombs, V.L., et al., 1993.Near-Primary Melt Inclusions in Anorthite Phenocrysts from the Galapagos Platfrom.Earth and Planetary Science Letters, 119(4):527-537. doi: 10.1016/0012-821X(93)90060-M
[42]	Su, B.X., Qin, K.Z., Santosh, M., et al., 2013.The Early Permian Mafic-Ultramafic Complexes in the Beishan Terrane, NW China:Alaskan-Type Intrusives or Rift Cumulates?Journal of Asian Earth Sciences, 66:175-187. https://doi.org/10.1016/j.jseaes.2012.12.039
[43]	Su, B.X., Qin, K.Z., Sun, H., et al., 2012.Subduction-Induced Mantle Heterogeneity beneath Eastern Tianshan and Beishan:Insights from Nd-Sr-Hf-O Isotopic Mapping of Late Paleozoic Mafic-Ultramafic Complexes.Lithos, 134-135:41-51. doi: 10.1016/j.lithos.2011.12.011
[44]	Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oeanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345. doi: 10.1144/GSL.SP.1989.042.01.19
[45]	Takagi, D., Sato, H., Nakagawa, M., 2005.Experimental Study of a Low-Alkali Tholeiite at 1-5kbar:Optimal Condition for the Crystallization of High-An Plagioclase in Hydrous Arc Tholeiite.Contributions to Mineralogy and Petrology, 149(5):527-540. doi: 10.1007/s00410-005-0666-7
[46]	Tatsumi, Y., Eggins, S., 1995. Subduction Zone Magmatism. Blackwell Science, Cambridge, 211.
[47]	Tatsumi, Y., Takahashi, T., 2006.Operation of Subduction Factory and Production of Andesite.Journal of Mineralogical and Petrological Sciences, 101(3):145-153. doi: 10.2465/jmps.101.145
[48]	Taylor, S.R., McLennan, S.M., 1985.The Continental Crust:Its Composition and Evolution, an Examination of the Geochemical Record Preserved in Sedimentary Rocks.Blackwell Scientific Publication, Oxford, 46.
[49]	Wang, Y.J., Zhao, G.C., Fan, W.M., et al., 2007a.LA-ICP-MS U-Pb Zircon Geochronology and Geochemistry of Paleoproterozoic Mafic Dykes from Western Shandong Province:Implications for Back-Arc Basin Magmatism in the Eastern Block, North China Craton.Precambrian Research, 154(1-2):107-124. doi: 10.1016/j.precamres.2006.12.010
[50]	Wang, Y.X., Yang, J.D., Chen, J., et al., 2007b.The Sr and Nd Isotopic Variations of the Chinese Loess Plateau during the Past 7Ma:Implications for the East Asian Winter Monsoon and Source Areas of Loess.Palaeogeography, Palaeoclimatology, Palaeoecology, 249(3-4):351-361. doi: 10.1016/j.palaeo.2007.02.010
[51]	Windley, B.F., Alexeiev, D., Xiao, W.J., et al., 2007.Tectonic Models for Accretion of the Central Asian Orogenic Belt.Journal of the Geological Society, 164(1):31-47. doi: 10.1144/0016-76492006-022
[52]	Wood, D.A., 1980.The Application of a Th-Hf-Ta Diagram to Problems of Tectonomagmatic Classification and to Establishing the Nature of Crustal Contamination of Basaltic Lavas of the British Tertiary Volcanic Province.Earth and Planetary Science Letters, 50 (1):11-30. https://doi.org/10.1016/0012-821x(80)90116-8
[53]	Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200702002.htm
[54]	Wu, F.Y., Ye, M., Zhang, S.H., 1995.Geodynamic Model of the Manzhouli-Suifenhe Geoscience Transect.Earth Science, 20(5):535-539 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dqkx505.009.htm
[55]	Xu, W.L., Wang, F., Meng, E., et al., 2012.Paleozoic-Early Mesozoic Tectonic Evolution in the Eastern Heilongjiang Province, NE China:Evidence from Igneous Rock Association and U-Pb Geochronology of Detrital Zircons.Journal of Jilin University (Earth Science Edition), 42(5):1378-1389 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ201205012.htm
[56]	Yang, J.H., Wu, F.Y., Shao, J.A., et al., 2006.In-Situ U-Pb Dating and Hf Isotopic Analyses of Zircons from Volcanic Rocks of the Houcheng and Zhangjiakou Formations in the Zhang-Xuan Area, Northeast China.Earth Science, 31(1):71-80 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200601011.htm
[57]	Ye, M., Zhang, S.H., Wu, F.Y., 1994.The Classification of the Paleozoic Tectonic Units in the Area Crossed by M-S GGT.Journal of Changchun University of Earth Sciences, 24(3):241-245 (in Chinese with English abstract).
[58]	Yu, J.J., Hou, X.G., Ge, W.C., et al., 2013.Magma Mixing Genesis of the Early Permian Liulian Pluton at the Northeastern Margin of the Jiamusi Massif in NE China:Evidences from Petrography, Geochronology and Geochemistry.Acta Petrologica Sinica, 9(9):2971-2986 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201309002.htm
[59]	Zeng, Z.G., Zhang, Y.X., Chen, Z.X., et al., 2016.Geological Tectonics, Magmatism and Seafloor Hydrothermal Activity in the Back-Arc Basins of the Western Pacific.Studia Marina Sinica, (0):3-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HKJK201600003.htm
[60]	Zhang, Z.C., Mao, J.W., Saunders, A.D., et al., 2009.Petrogenetic Modeling of Three Mafic-Ultramafic Layered Intrusions in the Emeishan Large Igneous Province, SW China, Based on Isotopic and Bulk Chemical Constraints.Lithos, 113(3-4):369-392. https://doi.org/10.1016/j.lithos.2009.04.023
[61]	Zhao, J.H., Zhou, M.F., 2007.Geochemistry of Neoproterozoic Mafic Intrusions in the Panzhihua District (Sichuan Province, SW China):Implications for Subduction-Related Metasomatism in the Upper Mantle.Precambrian Research, 152(1-2):27-47. doi: 10.1016/j.precamres.2006.09.002
[62]	Zhao, S., Xu, W.L., Tang, J., et al., 2016.Neoproterozoic Magmatic Event and Tectonic Attribution of the Erguna Massif:Constraints from Geochronological, Geochemical and Hf Isotopic Data of Intrusive Rocks.Earth Science, 41(11):1803-1829 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201611001.htm
[63]	Zhao, Z.F., Dai, L.Q., Zheng, Y.F., 2015.Two Types of the Crust-Mantle Interaction in Continental Subduction Zone.Science China:Earth Sciences, 45(7):900-915 (in Chinese). doi: 10.1007/s11430-015-5136-0
[64]	Zhao, Z.H., Wang, Q., Xiong, X.L., 2004.Complex Mantle-Crust Interaction in Subduction Zone.Bulletin of Mineralogy, Petrology and Geochemistry, 23(4):277-284 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KYDH200404001.htm
[65]	Zhong, H., Zhu, W.G., Hu, R.Z., et al., 2009.Zircon U-Pb Age and Sr-Nd-Hf Isotope Geochemistry of the Panzhihua A-Type Syenitic Intrusion in the Emeishan Large Igneous Province, Southwest China and Implications for Growth of Juvenile Crust.Lithos, 110(1-4):109-128. https://doi.org/10.1016/j.lithos.2008.12.006
[66]	Zhou, J.B., Wilde, S.A., Zhang, X.Z., et al., 2009.The Onset of Pacific Margin Accretion in NE China:Evidence from the Heilongjiang High Pressure Metamorphic Belt.Tectonophysics, 478:230-246. https://doi.org/10.1016/j.tecto.2009.08.009
[67]	邓晋福, 1987.岩石相平衡与岩石成因.武汉:武汉地质学院出版社, 45-63.
[68]	冯光英, 刘燊, 冯彩霞, 等, 2011.吉林红旗岭超基性岩体的锆石U-Pb年龄、Sr-Nd-Hf同位素特征及岩石成因.岩石学报, 27(6):1594-1606. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201106003&dbname=CJFD&dbcode=CJFQ
[69]	郭锋, 范蔚茗, 李超文, 等, 2009.早古生代古亚洲洋俯冲作用:自内蒙古大石寨玄武岩的年代学与地球化学证据.中国科学(地球科学), 39(5):569-579. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk200905004&dbname=CJFD&dbcode=CJFQ
[70]	郭奎城, 张文龙, 杨晓平, 等, 2011.黑河市五道沟地区早二叠世A型花岗岩成因.吉林大学学报(地球科学版), 41(4):1077-1083. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz201104017&dbname=CJFD&dbcode=CJFQ
[71]	侯可军, 李延河, 田有荣, 2009.LA-MC-ICP-MS锆石微区原味U-Pb定年技术.矿床地质, 28(4):481-492. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kcdz200904009&dbname=CJFD&dbcode=CJFQ
[72]	孟恩, 许文良, 杨德彬, 等, 2008.佳木斯地块东缘及东南缘二叠纪火山作用:锆石U-Pb年代学、地球化学及其构造意义.科学通报, 53(8):956-965. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb200808016&dbname=CJFD&dbcode=CJFQ
[73]	孟杰, 刘晓旸, 梁一鸿, 等, 2017.吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义.地球科学, 42(4):502-510. http://www.earth-science.net/WebPage/Article.aspx?id=3562
[74]	裴福萍, 王志伟, 曹花花, 等, 2014.吉林省中部地区早古生代英云闪长岩的成因:锆石U-Pb年代学和地球化学证据.岩石学报, 30(7):2009-2019. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201407014&dbname=CJFD&dbcode=CJFQ
[75]	邵济安, 李永飞, 唐克东, 2013.张广才岭造山过程的重构及其大地构造意义.岩石学报, 29(9):2959-2970. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201309001&dbname=CJFD&dbcode=CJFQ
[76]	吴福元, 李献华, 郑永飞, 等, 2007.Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200702002&dbname=CJFD&dbcode=CJFQ
[77]	吴福元, 叶茂, 张世红, 1995.中国满洲里-绥芬河地学断面域的地球动力学模型.地球科学, 20(5):535-539. http://www.earth-science.net/WebPage/Article.aspx?id=329
[78]	许文良, 王枫, 孟恩, 等, 2012.黑龙江省东部古生代-早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据.吉林大学学报(地球科学版), 42(5):1378-1389. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz201205012&dbname=CJFD&dbcode=CJFQ
[79]	杨进辉, 吴福元, 邵济安, 等, 2006.冀北张-宣地区后城组、张家口组火山岩锆石U-Pb年龄和Hf同位素.地球科学, 31(1):71-80. http://www.earth-science.net/WebPage/Article.aspx?id=1539
[80]	叶茂, 张世红, 吴福元, 1994.中国满洲里-绥芬河地学断面域古生代构造单元及其地质演化.长春地质学院学报, 24(3):241-245. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz403.000&dbname=CJFD&dbcode=CJFQ
[81]	于介江, 侯雪刚, 葛文春, 等, 2013.佳木斯地块东北缘早二叠世六连岩体的岩浆混合成因:岩相学、年代学和地球化学证据.岩石学报, 29(9):2971-2986. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201309002&dbname=CJFD&dbcode=CJFQ
[82]	曾志刚, 张玉祥, 陈祖兴, 等, 2016.西太平洋典型弧后盆地的地质构造、岩浆作用与热液活动.海洋科学集刊, (0):3-36. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=hkjk201600003&dbname=CJFD&dbcode=CJFQ
[83]	赵硕, 许文良, 唐杰, 等.2016.额尔古纳地块新元古代岩浆作用与微陆块构造属性:来自侵入岩锆石U-Pb年代学、地球化学和Hf同位素的制约.地球科学, 41(11):1803-1829. http://www.earth-science.net/WebPage/Article.aspx?id=3381
[84]	赵振华, 王强, 熊小林, 2004.俯冲带复杂的壳幔相互作用.矿物岩石地球化学通报, 23(4):277-284. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kydh200404001&dbname=CJFD&dbcode=CJFQ
[85]	赵子福, 戴立群, 郑永飞, 2015.大陆俯冲带两类壳幔相互作用.中国科学:地球科学, 45(7):900-915. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk201507002&dbname=CJFD&dbcode=CJFQ