南秦岭封子山岩体的年代学、地球化学、Hf同位素特征及其地质意义
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摘要
对南秦岭封子山岩体进行了锆石U-Pb年代学、岩石地球化学以及Hf同位素的研究,以确定其形成时代、岩体成因及形成时的构造环境.LA-ICP-MS锆石U-Pb定年测试结果表明,该岩体形成于新元古代晚期(716～710Ma).锆石Hf同位素分析显示ε_(Hf)(t)为-3.16～1.17,二阶段模式年龄(TDM2)为1.84～1.52Ga.地球化学特征显示封子山岩体具高硅(62.92%～73.57%)、高钠(3.33%～4.22%),富集轻稀土元素,富集K、Rb、Ba、Th、U等大离子亲石元素,亏损Nb、Ta、Ti、P等高场强元素的特征,Eu显示弱负异常(δEu=0.79～0.95),为准铝质-弱过铝质中钾钙碱性I型花岗岩.结果表明,封子山岩体主要来源于陡岭群片麻岩的部分熔融.封子山岩体形成于裂谷扩张与小洋盆间杂并存的构造环境,是洋壳向陆壳俯冲作用的产物,可能是Rodinia超大陆聚合与裂解事件在该地区作用的响应.
This study presents zircon U-Pb dating,geochemistry and zircon Lu-Hf isotopic data for the Fengzishan granitic intrusion located in South Qinling to constrain its formation age,petrogenesis and tectonic setting.LA-ICP-MS zircon U-Pb dating results suggest that the Fengzishan granitic intrusion was formed in Late Neoproterozoic(716-710 Ma).Zircon Hf isotopic data show theε_(Hf)(t)values of-3.16-1.17 and TDM2 values of 1.84-1.52 Ga.Geochemical characteristics show that they are high in silica(62.92%-73.57%)and Na(3.33%-4.22%)contents and relatively enriched in light rare earth elements(LREE)and large ion lithophile elements(LILE)(e.g.K,Rb,Ba,Th,U),poor in high field strength elements(HFSE)(Nb,Ta,Ti,P)and slightly negative Eu anomalies(δEu=0.79-0.95),displaying metaluminous to weak peraluminous and medium potassium calc-alkaline I-type granites.These characteristics suggest that the magma was primarily derived from partial melting of gneiss of the Douling Group.The Fengzishan granitic intrusion was produced by subduction of oceanic crust into continental crust and was formed in the tectonic setting of rift expansion coexisting with small ocean basin.The formation of the Fengzishan granitoid was probably the response to the amalgamation and separation of the global Rodinia supercontinent.
This study presents zircon U-Pb dating,geochemistry and zircon Lu-Hf isotopic data for the Fengzishan granitic intrusion located in South Qinling to constrain its formation age,petrogenesis and tectonic setting.LA-ICP-MS zircon U-Pb dating results suggest that the Fengzishan granitic intrusion was formed in Late Neoproterozoic(716-710 Ma).Zircon Hf isotopic data show theε_(Hf)(t)values of-3.16-1.17 and TDM2 values of 1.84-1.52 Ga.Geochemical characteristics show that they are high in silica(62.92%-73.57%)and Na(3.33%-4.22%)contents and relatively enriched in light rare earth elements(LREE)and large ion lithophile elements(LILE)(e.g.K,Rb,Ba,Th,U),poor in high field strength elements(HFSE)(Nb,Ta,Ti,P)and slightly negative Eu anomalies(δEu=0.79-0.95),displaying metaluminous to weak peraluminous and medium potassium calc-alkaline I-type granites.These characteristics suggest that the magma was primarily derived from partial melting of gneiss of the Douling Group.The Fengzishan granitic intrusion was produced by subduction of oceanic crust into continental crust and was formed in the tectonic setting of rift expansion coexisting with small ocean basin.The formation of the Fengzishan granitoid was probably the response to the amalgamation and separation of the global Rodinia supercontinent.
引文
Barbarin,B.,1999.A Review of the Relationships between Granitoid Types,Their Origins and Their Geodynamic Environments.Lithos,46(3):605-626.https://doi.org/10.1016/s0024-4937(98)00085-1
Chappell,B.W.,White,A.J.R.,1974.Two Contrasting Granite Types.Pacific Geology,8:173-174.
Chen,J.L.,Guo,Y.S.,Fu,S.M.,2004.The Research Headway to Granitiod-Classification Review and Synthesis of ISMA Granitiod.Acta Geologica Gansu,13(1):67-73(in Chinese with English abstract).
Chen,Z.H.,2004.The Neoproterozoic Tectono-Thermal Events in the Eastern Qinling Orogen,and Their Geotectonic Significances(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Dong,Y.P.,Liu,X.M.,Zhang,G.W.,et al.,2012.Triassic Diorites and Granitoids in the Foping Area:Constraints on the Conversion from Subduction to Collision in the Qinling Orogen,China.Journal of Asian Earth Sciences,47:123-142.https://doi.org/10.1016/j.jseaes.2011.06.005
Dong,Y.P.,Sun,S.S.,Yang,Z.,et al.,2017.Neoproterozoic Subduction-Accretionary Tectonics of the South Qinling Belt,China.Precambrian Research,293:73-90.https://doi.org/10.1016/j.precamres.2017.02.015
Dong,Y.P.,Zhou,M.F.,Zhang,G.W.,et al.,2008.The Grenvillian Songshugou Ophiolite in the Qinling Mountains,Central China:Implications for the Tectonic Evolution of the Qinling Orogenic Belt.Journal of Asian Earth Sciences,32(5-6):325-335.https://doi.org/10.1016/j.jseaes.2007.11.010
Franzini,M.,Leoni,L.,Saitta,M.,1972.A Simple Method to Evaluate the Matrix Effects in X-Ray Fluorescence Analysis.X-Ray Spectrometry,1(4):151-154.https://doi.org/10.1002/xrs.1300010406
Gao,J.F.,Lu,J.J.,Lai,M.Y.,et al.,2003.Analysis of Trace Elements in Rock Samples Using HR-ICPMS.Journal of Nanjing University(Natural Sciences),39(6):844-850(in Chinese with English abstract).
Griffin,W.L.,Powell,W.J.,Pearson,N.J.,et al.,2008.GLIT-TER:Data Reduction Software for Laser Ablation ICP-MS.In:Sylvester,P.,ed.,Laser Ablation ICP-MS in the Earth Sciences:Current Practices and Outstanding Issues.Mineralogical Association of Canada,Vancouver,308-311.
Griffin,W.L.,Wang,X.,Jackson,S.E.,et al.,2002.Zircon Chemistry and Magma Mixing,SE China:In-Situ Analysis of Hf Isotopes,Tonglu and Pingtan Igneous Complexes.Lithos,61(3-4):237-269.https://doi.org/10.1016/s0024-4937(02)00082-8
Hu,F.Y.,Liu,S.W.,Santosh,M.,et al.,2016.Chronology and Tectonic Implications of Neoproterozoic Blocks in the South Qinling Orogenic Belt,Central China.Gondwana Research,30:24-47.https://doi.org/10.1016/j.gr.2015.01.006
Li,H.K.,Lu,S.N.,Chen,Z.H.,et al.,2003.Zircon U-Pb Geochronology of Rift-Type Volcanic Rocks of the Yaolinghe Group in the South Qinling Orogen.Geological Bulletin of China,22(10):775-781(in Chinese with English abstract).
Li,M.,2003.Study of the Geochemistry of Granitoid Intrusives of Douling Group in the East Qinling and Its Geological Significance(Dissertation).Northwest University,Xi'an(in Chinese with English abstract).
Li,Z.X.,Bogdanova,S.V.,Collins,A.S.,et al.,2008.Assembly,Configuration,and Break-up History of Rodinia:ASynthesis.Precambrian Research,160(1-2):179-210.https://doi.org/10.1016/j.precamres.2007.04.021
Li,Z.X.,Li,X.H.,Kinny,P.D.,et al.,1999.The Breakup of Rodinia:Did It Start with a Mantle Plume beneath South China?Earth and Planetary Science Letters,173(3):171-181.https://doi.org/10.1016/s0012-821x(99)00240-x
Li,Z.X.,Li,X.H.,Kinny,P.D.,et al.,2003.Geochronology of Neoproterozoic Syn-Rift Magmatism in the Yangtze Craton,South China and Correlations with Other Continents:Evidence for a Mantle Superplume That Broke up Rodinia.Precambrian Research,122(1-4):85-109.https://doi.org/10.1016/s0301-9268(02)00208-5
Li,X.H.,Li,W.X.,He,B.,2012.Building of the South China Block and Its Relevance to Assembly and Breakup of Rodinia Supercontinent:Observations,Interpretations and Tests.Bulletin of Mineralogy,Petrology and Geochemistry,31(6):543-559(in Chinese with English abstract).
Ling,W.L.,Cheng,J.P.,Wang,X.H.,et al.,2002.Geochemical Features of the Neoproterozoic Igneous Rocks from the Wudang Region and Their Implications for the Reconstruction of the Jinning Tectonic Evolution along the South Qinling Orogenic Belt.Acta Petrologica Sinica,18(1):25-36(in Chinese with English abstract).
Liu,B.X.,Nie,H.,Qi,Y.,et al.,2013.Genesis and Geological Significances of Neoproterozoic Granitoids in the North Qinling Terrain,SW Henan,China.Acta Petrologica Sinica,29(7):2437-2455(in Chinese with English abstract).
Liu,C.J.,Pei,X.Z.,Li,Z.C.,et al.,2012.Geochemical Features and Tectonic Setting of the Neoproterozoic Granitic Gneiss in Tianshui Area on the Northern Margin of West Qinling.Geological Bulletin of China,31(10):1588-1601(in Chinese with English abstract).
Liu,H.B.,Pei,X.Z.,Ding,S.P.,et al.,2006.LA-ICP-MS Zircon U-Pb Dating of the Neoproterozoic Granitic Gneisses in the Yuanlong Area,Tianshui City,West Qinling,China,and Their Geological Significance.Geological Bulletin of China,25(11):1315-1320(in Chinese with English abstract).
Liu,J.B.,Zhang,L.M.,2013.Neoproterozoic Low to Negativeδ18 O Volcanic and Intrusive Rocks in the Qinling Mountains and Their Geological Significance.Precambrian Research,230:138-167.https://doi.org/10.1016/j.precamres.2013.02.006
Lu,S.N.,1998.A Review of Advance in the Research on the Neoproterozoic Rodinia Supercontinent.Geological Review,44(5):489-495(in Chinese with English abstract).
Lu,S.N.,Chen,Z.H.,Li,H.K.,et al.,2005.Two Magmatic Belts of the Neoproterozoic in the Qinling Orogenic Belt.Acta Geologica Sinica,79(2):165-173(in Chinese with English abstract).
Lu,X.X.,Dong,Y.,Wei,X.D.,et al.,1999.The Age and Tectonic Significance of A-Type Granite in Tuwushan,East Qinling Mountains.Chinese Science Bulletin,44(9):975-978(in Chinese).
Ma,S.W.,Liu,C.F.,Xu,Z.Q.,et al.,2017.Geochronology,Geochemistry and Tectonic Significance of the Early Carboniferous Gabbro and Diorite Plutons in West Ujimqin,Inner Mongolia.Journal of Earth Science,28(2):249-264.https://doi.org/10.1007/s12583-016-0912-2
Mattauer,M.,Matte,P.,Malavieille,J.,et al.,1985.Tectonics of the Qinling Belt:Build-up and Evolution of Eastern Asia.Nature,317(6037):496-500.https://doi.org/10.1038/317496a0
Middlemost,E.A.K.,1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews,37(3-4):215-224.https://doi.org/10.1016/0012-8252(94)90029-9
Nie,H.,2016.Tectonothermal Events and Crustal Evolution in the Eastern South Qinling Block(Dissertation).University of Science and Technology of China,Hefei(in Chinese with English abstract).
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Peccerillo,A.,Taylor,S.R.,1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81.https://doi.org/10.1007/bf00384745
Pei,X.Z.,Ding,S.P.,Zhang,G.W.,et al.,2007.Zircons LA-ICP-MS U-Pb Dating of Neoproterozoic Granitoid Gneisses in the North Margin of West Qinling and Geological Implication.Acta Geologica Sinica,81(6):772-786(in Chinese with English abstract).
Pei,X.Z.,Zhang,W.J.,Wang,T.,et al.,1995.Geological Characteristics and Tectonic Evolution of the North Qinling Mountains Orogenic Belt.Northwestern Geology,16(4):8-12(in Chinese).
Ratschbacher,L.,Hacker,B.R.,Calvert,A.,et al.,2003.Tectonics of the Qinling(Central China):Tectonostratigraphy,Geochronology,and Deformation History.Tectonophysics,366(1-2):1-53.https://doi.org/10.1016/s0040-1951(03)00053-2
Shen,J.,Zhang,Z.Q.,Liu,D.Y.,1997.Sm-Nd,Rb-Sr,40 Ar/39 Ar,207 Pb/206 Pb Age of the Douling Metamorphic Complex from Eastern Qinling Orogenic Belt.Acta Geoscientia Sinica,18(3):248-254(in Chinese with English abstract).
Shi,Y.,Huang,Q.W.,Liu,X.J.,et al.,2018.Provenance and Tectonic Setting of the Supra-Crustal Succession of the Qinling Complex:Implications for the Tectonic Affinity of the North Qinling Belt,Central China.Journal of Asian Earth Sciences,158:112-139.https://doi.org/org/10.1016/j.jseaes.2018.02.011
Shi,Y.,Pei,X.L.,Castillo,P.R.,et al.,2017.Petrogenesis of the~500Ma Fushui Mafic Intrusion and Early Paleozoic Tectonic Evolution of the Northern Qinling Belt,Central China.Journal of Asian Earth Sciences,141:74-96.https://doi.org/org/10.1016/j.jseaes.2016.09.003
Shi,Y.,Yu,J.H.,Pei,X.L.,et al.,2014.Early Paleozoic Mantle-Derived Magmatism from the Qinling Complex of the Qinling Orogenic Belt.Journal of Guilin University of Technology,34(2):207-217(in Chinese with English abstract).
Shi,Y.,Yu,J.H.,Santosh,M.,2013.Tectonic Evolution of the Qinling Orogenic Belt,Central China:New Evidence from Geochemical,Zircon U-Pb Geochronology and Hf Isotopes.Precambrian Research,231:19-60.https://doi.org/10.1016/j.precamres.2013.03.001
Shi,Y.,Yu,J.H.,Xu,X.S.,et al.,2009.Geochronology and Geochemistry of the Qinling Group in the Eastern Qinling Orogen.Acta Petrologica Sinica,25(10):2651-2670(in Chinese with English abstract).
Su,W.,Liu,J.B.,Chen,N.S.,et al.,2013.Geochronology and Tectonic Background of Magmatic and Metamorphic Events in the East Qinling-Dabie Mountains.Acta Petrologica Sinica,29(5):1573-1593,1847(in Chinese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Wang,X.C.,Li,X.H.,Li,W.X.,et al.,2008.The Bikou Basalts in the Northwestern Yangtze Block,South China:Remnants of 820-810 Ma Continental Flood Basalts?.Geological Society of America Bulletin,120(11-12):1478-1492.https://doi.org/10.1130/b26310.1
Wang,X.X.,Wang,T.,Zhang,C.L.,2015.Granitic Magmatism and Orogenic Belt Evolution in the Qinling Mountains Orogenic Belt.Science China Earth Sciences,45(8):1109-1125(in Chinese with English abstract).
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).
Xia,L.Q.,2014.The Geochemical Criteria to Distinguish Continental Basalts from Arc Related Ones.EarthScience Reviews,139:195-212.https://doi.org/10.1016/j.earscirev.2014.09.006
Xia,L.Q.,Xia,Z.C.,Xu,X.Y.,1996.Characteristics of Mid Late Proterozoic Volcanic Rocks and Cleavage of Precambrian Continental in Southern Qinling Mountains.Science China Earth Sciences,26(3):237-243(in Chinese).
Xu,B.,2001.Recent Study of the Rodinia Supercontinent Evolution and Its Main Goal.Geological Science and Technology Information,20(1):15-19(in Chinese with English abstract).
Xu,T.,Pei,X.Z.,Li,R.B.,et al.,2017.Ages and Geochemical Features of the Heigouxia Volcanic Rocks in the Mianxian-Lüeyang Area of South Qinling Orogen:Evidence for Existence and Subduction of Neoproterozoic Mianxian-Lüeyang Ocean.Geological Review,63(2):375-394(in Chinese with English abstract).
Xu,T.,Pei,X.Z.,Liu,C.J.,et al.,2016.Geochemical Features and Zircon LA-ICP-MS U-Pb Ages of the Neoproterozoic Zhangergou Metamorphic Andesitic Rocks in the Mianxian-Lüeyang Area of South Qinling Orogen:Evidence for Amalgamation of Rodinia Supercontinent.Geological Review,62(2):434-450(in Chinese with English abstract).
Yan,M.,Liu,S.W.,Li,Q.G.,et al.,2014.LA-ICP-MS Zircon U-Pb Chronology and Lu-Hf Isotopic Features of the Mihunzhen Pluton in the South Qinling Tectonic Belt.Acta Petrologica Sinica,30(2):390-400(in Chinese with English abstract).
Yang,B.H.,Zhang,C.L.,Li,L.,et al.,2011.Sr-Nd-Pb Isotopic Characteristics of the Granitoids in the Douling Complexes,Eastern Qinling,China and Its Geological Significance.Geological Bulletin of China,30(2-3):439-447(in Chinese with English abstract).
Yang,P.T.,Liu,S.W.,Li,Q.G.,et al.,2012.Emplacing Age of the Tiewadian Pluton in the South Qinling Tectonic Belt and Its Geological Implications.Acta Geologica Sinica,86(9):1525-1540(in Chinese with English abstract).
Zhang,B.R.,Gao,S.,Zhang,H.F.,et al.,2002.Geochemistry of Qinling Orogenic Belt.Science Press,Beijing(in Chinese).
Zhang,B.R.,Zhang,H.F.,Zhao,Z.D.,et al.,1996.Geochemical Subdivision and Evolution of the Lithosphere in East Qinling and Adjacent Regions-Implications for Tectonics.Science China Earth Sciences,26(3):201-208(in Chinese).
Zhang,C.L.,Li,M.,Wang,T.,et al.,2004.U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling.Acta Geologica Sinica(English Edition),78(1):83-95.https://doi.org/10.1111/j.1755-6724.2004.tb00678.x
Zhang,C.L.,Yu,Z.P.,Zhou,D.W.,1996.Geochemical Constraints on the Danfeng Ophiolite from the Metabasalts in Shangdan Zone of East Qinling.In:Han,S.,ed.,Symposium on Ophiolite and Geodynamics.Geological Society of China,Beijing,154-157(in Chinese).
Zhang,G.W.,Mei,Z.C.,Zhou,D.W.,et al.,1988.Formation and Evolution of the Qinling Orogenic Belt.Northwest University Press,Xi'an(in Chinese).
Zhang,G.W.,Meng,Q.R.,Lai,S.C.,1995.Structure and Tectonics of Qinling Orogenic Belt.Science in China(Series B),25(9):994-1003(in Chinese).
Zhang,G.W.,Yu,Z.P.,Dong,Y.P.,et al.,2000.On Precambrian Framework and Evolution of the Qinling Belt.Acta Petrologica Sinica,16(1):11-21(in Chinese with English abstract).
Zhang,G.W.,Zhang,B.R.,Yuan,X.C.,et al.,2001.Qinling Orogenic Belt and Continental Dynamics.Belt.Science Press,Beijing(in Chinese).
Zhang,H.F.,Ouyang,J.P.,Ling,W.L.,et al.,1996.Tectonic Division of Douling Massif of East Qinling by Pb Isotopic Compositional Characteristics.Earth Science,21(5):487-490(in Chinese with English abstract).
Zhang,H.F.,Zhang,B.R.,Luo,T.C.,1993.Geochemical Study of Genesis and Tectonic Setting for Late Proterozoic Granitoids,North Qinling,China.Earth Science,18(2):194-202(in Chinese with English abstract).
Zhang,Q.,Jiao,S.T.,Li,C.D.,et al.,2017.Granite and Continental Tectonics,Magma Thermal Field and Metallogenesis.Acta Petrologica Sinica,33(5):1524-1540(in Chinese with English abstract).
Zhang,Q.,Pan,G.Q.,Li,C.D.,et al.,2007.Are Discrimination Diagrams always Indicative of Correct Tectonic Settings of Granites?Some Crucial Questions on Granite Study(3).Acta Petrologica Sinica,23(11):2683-2698(in Chinese with English abstract).
Zhang,R.Y.,Sun,Y.,Zhang,X.,et al.,2016.Neoproterozoic Magmatic Events in the South Qinling Belt,China:Implications for Amalgamation and Breakup of the Rodinia Supercontinent.Gondwana Research,30:6-23.https://doi.org/10.1016/j.gr.2015.06.015
Zhang,S.G.,Wei,C.J.,Zhao,Z.R.,et al.,1996.Formation and Metamorphic Evolution of Douling Complex in East Qinling Mountains.Science China Earth Sciences,26(Suppl.):73-77(in Chinese).
Zhang,S.G.,Zhang,Z.Q.,Song,B.,et al.,2004.On the Existence of Neoarchean Materials in the Douling Complex,Eastern Qinling-Evidence from U-Pb SHRIMP and Sm-Nd Geochronology.Acta Geologica Sinica,78(6):800-806(in Chinese with English abstract).
Zhang,Z.Q.,Zhang,G.W.,Fu,G.M.,et al.,1996.The Age of Metamorphic Strata in Qinling Mountains and Their Tectonic Significance.Science China Earth Sciences,26(3):216-222(in Chinese).
Zhang,Z.Q.,Zhang,G.W.,Tang,S.H.,2002.Isotope Chronology of Metamorphic Strata in Southern Qinling Mountains.Geological Publishing House,Beijing(in Chinese).
Zhang,Z.Q.,Zhang,Q.,1995.Geochemistry of Metamorphosed Late Proterozoic Kuanping Ophiolite in the Northern Qinling,China.Acta Petrologica Sinica,11(Suppl.1):165-176(in Chinese with English abstract).
Zhao,J.H.,Asimow,P.D.,Zhou,M.F.,et al.,2017.An Andean-Type Arc System in Rodinia Constrained by the Neoproterozoic Shimian Ophiolite in South China.Precambrian Research,296:93-111.https://doi.org/org/10.1016/j.precamres.2017.04.017
Zhao,Z.R.,Wan,Y.S.,Zhang,S.G.,et al.,1995.The Geochemical Features of the Douling Metamorphic Complex.Acta Petrologica Sinica,11(2):148-159(in Chinese with English abstract).
Zhu,X.Y.,2010.Evolution and Provenance of the Basement in the Eastern Qinling Orogen,China:Evidence from Geochemistry and Zircon U-Pb Geochronology(Dissertation).Chinese Academy of Sciences,Beijing(in Chinese with English abstract).
Zhu,X.Y.,Chen,F.K.,Nie,H.,et al.,2014.Neoproterozoic Tectonic Evolution of South Qinling,China:Evidence from Zircon Ages and Geochemistry of the Yaolinghe Volcanic Rocks.Precambrian Research,245:115-130.https://doi.org/10.1016/j.precamres.2014.02.005
陈建林,郭原生,付善明,2004.花岗岩研究进展---ISMA花岗岩类分类综述.甘肃地质学报,13(1):67-73.
陈志宏,2004.秦岭造山带东部新元古代热-构造事件及其地质意义(博士学位论文).北京:中国地质科学院.
高剑峰,陆建军,赖鸣远,等,2003.岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学版),39(6):844-850.
李怀坤,陆松年,陈志宏,等,2003.南秦岭耀岭河群裂谷型火山岩锆石U-Pb年代学.地质通报,22(10):775-781.
李淼,2003.东秦岭陡岭群中新元古代花岗岩体的地球化学特征及其地质意义(硕士学位论文).西安:西北大学.
李献华,李武显,何斌,2012.华南陆块的形成与Rodinia超大陆聚合-裂解---观察、解释与检验.矿物岩石地球化学通报,31(6):543-559.
凌文黎,程建萍,王歆华,等,2002.武当地区新元古代岩浆岩地球化学特征及其对南秦岭晋宁期区域构造性质的指示.岩石学报,18(1):25-36.
刘丙祥,聂虎,齐玥,等,2013.豫西南地区北秦岭地体新元古代花岗岩类岩石成因及其地质意义.岩石学报,29(7):2437-2455.
刘成军,裴先治,李佐臣,等,2012.西秦岭北缘天水地区新元古代花岗质片麻岩地球化学特征及其形成环境.地质通报,31(10):1588-1601.
刘会彬,裴先治,丁仨平,等,2006.西秦岭天水市元龙地区新元古代花岗质片麻岩锆石LA-ICP-MS U-Pb定年及其地质意义.地质通报,25(11):1315-1320.
陆松年,1998.新元古时期Rodinia超大陆研究进展述评.地质论评,44(5):489-495.
陆松年,陈志宏,李怀坤,等,2005.秦岭造山带中两条新元古代岩浆岩带.地质学报,79(2):165-173.
卢欣祥,董有,尉向东,等,1999.东秦岭吐雾山A型花岗岩的时代及其构造意义.科学通报,44(9):975-978.
聂虎,2016.南秦岭东段构造热事件与地壳演化(博士学位论文).合肥:中国科学技术大学.
裴先治,丁仨平,张国伟,等,2007.西秦岭北缘新元古代花岗质片麻岩的LA-ICP-MS锆石U-Pb年龄及其地质意义.地质学报,81(6):772-786.
裴先治,张维吉,王涛,等,1995.北秦岭造山带的地质特征及其构造演化.西北地质,16(4):8-12.
沈洁,张宗清,刘敦一,1997.东秦岭陡岭群变质杂岩Sm-Nd、Rb-Sr、40 Ar/39 Ar、207 Pb/206 Pb年龄.地球学报,18(3):248-254.
时毓,于津海,裴小利,等,2014.秦岭造山带中秦岭杂岩的早古生代幔源岩浆作用.桂林理工大学学报,34(2):207-217.
时毓,于津海,徐夕生,等,2009.秦岭造山带东段秦岭岩群的年代学和地球化学研究.岩石学报,25(10):2651-2670.
苏文,刘景波,陈能松,等,2013.东秦岭-大别山及其两侧的岩浆和变质事件年代学及其形成的大地构造背景.岩石学报,29(5):1573-1593,1847.
王晓霞,王涛,张成立,等,2015.秦岭造山带花岗质岩浆作用与造山带演化.中国科学:地球科学,45(8):1109-1125.
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.
夏林圻,夏祖春,徐学义,等,1996.南秦岭中-晚元古代火山岩性质与前寒武纪大陆裂解.中国科学(D辑:地球科学),26(3):237-243.
徐备,2001.Rodinia超大陆构造演化研究的新进展和主要目标.地质科技情报,20(1):15-19.
徐通,裴先治,李瑞保,等,2017.南秦岭勉略构造带黑沟峡火山岩年代学及地球化学特征---新元古代勉略洋盆存在及俯冲的记录.地质论评,63(2):375-394.
徐通,裴先治,刘成军,等,2016.南秦岭勉略构造带张儿沟新元古代变安山岩地球化学特征及锆石LA-ICP-MSU-Pb年龄---Rodinia超大陆聚合事件的记录.地质论评,62(2):434-450.
阎明,刘树文,李秋根,等,2014.南秦岭迷魂阵岩体LA-ICP-MS锆石U-Pb年代学和Lu-Hf同位素特征.岩石学报,30(2):390-400.
杨斌虎,张成立,李雷,等,2011.东秦岭陡岭杂岩花岗岩的Sr-Nd-Pb同位素特征及其地质意义.地质通报,30(Z1):439-447.
杨朋涛,刘树文,李秋根,等,2012.南秦岭铁瓦殿岩体的成岩时代及地质意义.地质学报,86(9):1525-1540.
张本仁,高山,张宏飞,等,2002.秦岭造山带地球化学.北京:科学出版社.
张本仁,张宏飞,赵志丹,等,1996.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义.中国科学(D辑),26(3):201-208.
张成立,于在平,周鼎武,1996.东秦岭商丹带变质玄武岩地球化学特征对丹凤蛇绿岩的限制.见:韩松,编,蛇绿岩与地球动力学研讨会.北京:中国地质学会,154-157.
张国伟,梅志超,周鼎武,等,1988.秦岭造山带的形成及其演化.西安:西北大学出版社.
张国伟,孟庆任,赖绍聪,等,1995.秦岭造山带的结构构造.中国科学(B辑),25(9):994-1003.
张国伟,于在平,董云鹏,等,2000.秦岭区前寒武纪构造格局与演化问题探讨.岩石学报,16(1):11-21.
张国伟,张本仁,袁学诚,等,2001.秦岭造山带与大陆动力学.北京:科学出版社.
张宏飞,欧阳建平,凌文黎,等,1996.从Pb同位素组成特征论东秦岭陡岭块体的构造归属.地球科学,21(5):487-490.
张宏飞,张本仁,骆庭川,1993.北秦岭新元古代花岗岩类成因与构造环境的地球化学研究.地球科学,18(2):194-202.
张旗,焦守涛,李承东,等,2017.花岗岩与大陆构造、岩浆热场与成矿.岩石学报,33(5):1524-1540.
张旗,潘国强,李承东,等,2007.花岗岩构造环境问题:关于花岗岩研究的思考之三.岩石学报,23(11):2683-2698.
张寿广,张宗清,宋彪,等,2004.东秦岭陡岭杂岩中存在新太古代物质组成---SHRIMP锆石U-Pb和Sm-Nd年代学证据.地质学报,78(6):800-806.
张寿广,魏春景,赵子然,等,1996.东秦岭陡岭杂岩的形成与变质演化.中国科学(D辑:地球科学),26(S1):73-77.
张宗清,张国伟,付国民,等,1996.秦岭变质地层年龄及其构造意义.中国科学(D辑:地球科学),26(3):216-222.
张宗清,张国伟,唐索寒,2002.南秦岭变质地层同位素年代学.北京:地质出版社.
张宗清,张旗,1995.北秦岭晚元古代宽坪蛇绿岩中变质基性火山岩的地球化学特征.岩石学报,11(S1):165-176.
赵子然,万渝生,张寿广,等,1995.早元古陡岭群变质杂岩的岩石地球化学特征.岩石学报,11(2):148-159.
祝禧艳,2010.东秦岭造山带基底演化与属性:地球化学和年代学证据(博士学位论文).北京:中国科学院.
Chappell,B.W.,White,A.J.R.,1974.Two Contrasting Granite Types.Pacific Geology,8:173-174.
Chen,J.L.,Guo,Y.S.,Fu,S.M.,2004.The Research Headway to Granitiod-Classification Review and Synthesis of ISMA Granitiod.Acta Geologica Gansu,13(1):67-73(in Chinese with English abstract).
Chen,Z.H.,2004.The Neoproterozoic Tectono-Thermal Events in the Eastern Qinling Orogen,and Their Geotectonic Significances(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Dong,Y.P.,Liu,X.M.,Zhang,G.W.,et al.,2012.Triassic Diorites and Granitoids in the Foping Area:Constraints on the Conversion from Subduction to Collision in the Qinling Orogen,China.Journal of Asian Earth Sciences,47:123-142.https://doi.org/10.1016/j.jseaes.2011.06.005
Dong,Y.P.,Sun,S.S.,Yang,Z.,et al.,2017.Neoproterozoic Subduction-Accretionary Tectonics of the South Qinling Belt,China.Precambrian Research,293:73-90.https://doi.org/10.1016/j.precamres.2017.02.015
Dong,Y.P.,Zhou,M.F.,Zhang,G.W.,et al.,2008.The Grenvillian Songshugou Ophiolite in the Qinling Mountains,Central China:Implications for the Tectonic Evolution of the Qinling Orogenic Belt.Journal of Asian Earth Sciences,32(5-6):325-335.https://doi.org/10.1016/j.jseaes.2007.11.010
Franzini,M.,Leoni,L.,Saitta,M.,1972.A Simple Method to Evaluate the Matrix Effects in X-Ray Fluorescence Analysis.X-Ray Spectrometry,1(4):151-154.https://doi.org/10.1002/xrs.1300010406
Gao,J.F.,Lu,J.J.,Lai,M.Y.,et al.,2003.Analysis of Trace Elements in Rock Samples Using HR-ICPMS.Journal of Nanjing University(Natural Sciences),39(6):844-850(in Chinese with English abstract).
Griffin,W.L.,Powell,W.J.,Pearson,N.J.,et al.,2008.GLIT-TER:Data Reduction Software for Laser Ablation ICP-MS.In:Sylvester,P.,ed.,Laser Ablation ICP-MS in the Earth Sciences:Current Practices and Outstanding Issues.Mineralogical Association of Canada,Vancouver,308-311.
Griffin,W.L.,Wang,X.,Jackson,S.E.,et al.,2002.Zircon Chemistry and Magma Mixing,SE China:In-Situ Analysis of Hf Isotopes,Tonglu and Pingtan Igneous Complexes.Lithos,61(3-4):237-269.https://doi.org/10.1016/s0024-4937(02)00082-8
Hu,F.Y.,Liu,S.W.,Santosh,M.,et al.,2016.Chronology and Tectonic Implications of Neoproterozoic Blocks in the South Qinling Orogenic Belt,Central China.Gondwana Research,30:24-47.https://doi.org/10.1016/j.gr.2015.01.006
Li,H.K.,Lu,S.N.,Chen,Z.H.,et al.,2003.Zircon U-Pb Geochronology of Rift-Type Volcanic Rocks of the Yaolinghe Group in the South Qinling Orogen.Geological Bulletin of China,22(10):775-781(in Chinese with English abstract).
Li,M.,2003.Study of the Geochemistry of Granitoid Intrusives of Douling Group in the East Qinling and Its Geological Significance(Dissertation).Northwest University,Xi'an(in Chinese with English abstract).
Li,Z.X.,Bogdanova,S.V.,Collins,A.S.,et al.,2008.Assembly,Configuration,and Break-up History of Rodinia:ASynthesis.Precambrian Research,160(1-2):179-210.https://doi.org/10.1016/j.precamres.2007.04.021
Li,Z.X.,Li,X.H.,Kinny,P.D.,et al.,1999.The Breakup of Rodinia:Did It Start with a Mantle Plume beneath South China?Earth and Planetary Science Letters,173(3):171-181.https://doi.org/10.1016/s0012-821x(99)00240-x
Li,Z.X.,Li,X.H.,Kinny,P.D.,et al.,2003.Geochronology of Neoproterozoic Syn-Rift Magmatism in the Yangtze Craton,South China and Correlations with Other Continents:Evidence for a Mantle Superplume That Broke up Rodinia.Precambrian Research,122(1-4):85-109.https://doi.org/10.1016/s0301-9268(02)00208-5
Li,X.H.,Li,W.X.,He,B.,2012.Building of the South China Block and Its Relevance to Assembly and Breakup of Rodinia Supercontinent:Observations,Interpretations and Tests.Bulletin of Mineralogy,Petrology and Geochemistry,31(6):543-559(in Chinese with English abstract).
Ling,W.L.,Cheng,J.P.,Wang,X.H.,et al.,2002.Geochemical Features of the Neoproterozoic Igneous Rocks from the Wudang Region and Their Implications for the Reconstruction of the Jinning Tectonic Evolution along the South Qinling Orogenic Belt.Acta Petrologica Sinica,18(1):25-36(in Chinese with English abstract).
Liu,B.X.,Nie,H.,Qi,Y.,et al.,2013.Genesis and Geological Significances of Neoproterozoic Granitoids in the North Qinling Terrain,SW Henan,China.Acta Petrologica Sinica,29(7):2437-2455(in Chinese with English abstract).
Liu,C.J.,Pei,X.Z.,Li,Z.C.,et al.,2012.Geochemical Features and Tectonic Setting of the Neoproterozoic Granitic Gneiss in Tianshui Area on the Northern Margin of West Qinling.Geological Bulletin of China,31(10):1588-1601(in Chinese with English abstract).
Liu,H.B.,Pei,X.Z.,Ding,S.P.,et al.,2006.LA-ICP-MS Zircon U-Pb Dating of the Neoproterozoic Granitic Gneisses in the Yuanlong Area,Tianshui City,West Qinling,China,and Their Geological Significance.Geological Bulletin of China,25(11):1315-1320(in Chinese with English abstract).
Liu,J.B.,Zhang,L.M.,2013.Neoproterozoic Low to Negativeδ18 O Volcanic and Intrusive Rocks in the Qinling Mountains and Their Geological Significance.Precambrian Research,230:138-167.https://doi.org/10.1016/j.precamres.2013.02.006
Lu,S.N.,1998.A Review of Advance in the Research on the Neoproterozoic Rodinia Supercontinent.Geological Review,44(5):489-495(in Chinese with English abstract).
Lu,S.N.,Chen,Z.H.,Li,H.K.,et al.,2005.Two Magmatic Belts of the Neoproterozoic in the Qinling Orogenic Belt.Acta Geologica Sinica,79(2):165-173(in Chinese with English abstract).
Lu,X.X.,Dong,Y.,Wei,X.D.,et al.,1999.The Age and Tectonic Significance of A-Type Granite in Tuwushan,East Qinling Mountains.Chinese Science Bulletin,44(9):975-978(in Chinese).
Ma,S.W.,Liu,C.F.,Xu,Z.Q.,et al.,2017.Geochronology,Geochemistry and Tectonic Significance of the Early Carboniferous Gabbro and Diorite Plutons in West Ujimqin,Inner Mongolia.Journal of Earth Science,28(2):249-264.https://doi.org/10.1007/s12583-016-0912-2
Mattauer,M.,Matte,P.,Malavieille,J.,et al.,1985.Tectonics of the Qinling Belt:Build-up and Evolution of Eastern Asia.Nature,317(6037):496-500.https://doi.org/10.1038/317496a0
Middlemost,E.A.K.,1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews,37(3-4):215-224.https://doi.org/10.1016/0012-8252(94)90029-9
Nie,H.,2016.Tectonothermal Events and Crustal Evolution in the Eastern South Qinling Block(Dissertation).University of Science and Technology of China,Hefei(in Chinese with English abstract).
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Peccerillo,A.,Taylor,S.R.,1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81.https://doi.org/10.1007/bf00384745
Pei,X.Z.,Ding,S.P.,Zhang,G.W.,et al.,2007.Zircons LA-ICP-MS U-Pb Dating of Neoproterozoic Granitoid Gneisses in the North Margin of West Qinling and Geological Implication.Acta Geologica Sinica,81(6):772-786(in Chinese with English abstract).
Pei,X.Z.,Zhang,W.J.,Wang,T.,et al.,1995.Geological Characteristics and Tectonic Evolution of the North Qinling Mountains Orogenic Belt.Northwestern Geology,16(4):8-12(in Chinese).
Ratschbacher,L.,Hacker,B.R.,Calvert,A.,et al.,2003.Tectonics of the Qinling(Central China):Tectonostratigraphy,Geochronology,and Deformation History.Tectonophysics,366(1-2):1-53.https://doi.org/10.1016/s0040-1951(03)00053-2
Shen,J.,Zhang,Z.Q.,Liu,D.Y.,1997.Sm-Nd,Rb-Sr,40 Ar/39 Ar,207 Pb/206 Pb Age of the Douling Metamorphic Complex from Eastern Qinling Orogenic Belt.Acta Geoscientia Sinica,18(3):248-254(in Chinese with English abstract).
Shi,Y.,Huang,Q.W.,Liu,X.J.,et al.,2018.Provenance and Tectonic Setting of the Supra-Crustal Succession of the Qinling Complex:Implications for the Tectonic Affinity of the North Qinling Belt,Central China.Journal of Asian Earth Sciences,158:112-139.https://doi.org/org/10.1016/j.jseaes.2018.02.011
Shi,Y.,Pei,X.L.,Castillo,P.R.,et al.,2017.Petrogenesis of the~500Ma Fushui Mafic Intrusion and Early Paleozoic Tectonic Evolution of the Northern Qinling Belt,Central China.Journal of Asian Earth Sciences,141:74-96.https://doi.org/org/10.1016/j.jseaes.2016.09.003
Shi,Y.,Yu,J.H.,Pei,X.L.,et al.,2014.Early Paleozoic Mantle-Derived Magmatism from the Qinling Complex of the Qinling Orogenic Belt.Journal of Guilin University of Technology,34(2):207-217(in Chinese with English abstract).
Shi,Y.,Yu,J.H.,Santosh,M.,2013.Tectonic Evolution of the Qinling Orogenic Belt,Central China:New Evidence from Geochemical,Zircon U-Pb Geochronology and Hf Isotopes.Precambrian Research,231:19-60.https://doi.org/10.1016/j.precamres.2013.03.001
Shi,Y.,Yu,J.H.,Xu,X.S.,et al.,2009.Geochronology and Geochemistry of the Qinling Group in the Eastern Qinling Orogen.Acta Petrologica Sinica,25(10):2651-2670(in Chinese with English abstract).
Su,W.,Liu,J.B.,Chen,N.S.,et al.,2013.Geochronology and Tectonic Background of Magmatic and Metamorphic Events in the East Qinling-Dabie Mountains.Acta Petrologica Sinica,29(5):1573-1593,1847(in Chinese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Wang,X.C.,Li,X.H.,Li,W.X.,et al.,2008.The Bikou Basalts in the Northwestern Yangtze Block,South China:Remnants of 820-810 Ma Continental Flood Basalts?.Geological Society of America Bulletin,120(11-12):1478-1492.https://doi.org/10.1130/b26310.1
Wang,X.X.,Wang,T.,Zhang,C.L.,2015.Granitic Magmatism and Orogenic Belt Evolution in the Qinling Mountains Orogenic Belt.Science China Earth Sciences,45(8):1109-1125(in Chinese with English abstract).
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).
Xia,L.Q.,2014.The Geochemical Criteria to Distinguish Continental Basalts from Arc Related Ones.EarthScience Reviews,139:195-212.https://doi.org/10.1016/j.earscirev.2014.09.006
Xia,L.Q.,Xia,Z.C.,Xu,X.Y.,1996.Characteristics of Mid Late Proterozoic Volcanic Rocks and Cleavage of Precambrian Continental in Southern Qinling Mountains.Science China Earth Sciences,26(3):237-243(in Chinese).
Xu,B.,2001.Recent Study of the Rodinia Supercontinent Evolution and Its Main Goal.Geological Science and Technology Information,20(1):15-19(in Chinese with English abstract).
Xu,T.,Pei,X.Z.,Li,R.B.,et al.,2017.Ages and Geochemical Features of the Heigouxia Volcanic Rocks in the Mianxian-Lüeyang Area of South Qinling Orogen:Evidence for Existence and Subduction of Neoproterozoic Mianxian-Lüeyang Ocean.Geological Review,63(2):375-394(in Chinese with English abstract).
Xu,T.,Pei,X.Z.,Liu,C.J.,et al.,2016.Geochemical Features and Zircon LA-ICP-MS U-Pb Ages of the Neoproterozoic Zhangergou Metamorphic Andesitic Rocks in the Mianxian-Lüeyang Area of South Qinling Orogen:Evidence for Amalgamation of Rodinia Supercontinent.Geological Review,62(2):434-450(in Chinese with English abstract).
Yan,M.,Liu,S.W.,Li,Q.G.,et al.,2014.LA-ICP-MS Zircon U-Pb Chronology and Lu-Hf Isotopic Features of the Mihunzhen Pluton in the South Qinling Tectonic Belt.Acta Petrologica Sinica,30(2):390-400(in Chinese with English abstract).
Yang,B.H.,Zhang,C.L.,Li,L.,et al.,2011.Sr-Nd-Pb Isotopic Characteristics of the Granitoids in the Douling Complexes,Eastern Qinling,China and Its Geological Significance.Geological Bulletin of China,30(2-3):439-447(in Chinese with English abstract).
Yang,P.T.,Liu,S.W.,Li,Q.G.,et al.,2012.Emplacing Age of the Tiewadian Pluton in the South Qinling Tectonic Belt and Its Geological Implications.Acta Geologica Sinica,86(9):1525-1540(in Chinese with English abstract).
Zhang,B.R.,Gao,S.,Zhang,H.F.,et al.,2002.Geochemistry of Qinling Orogenic Belt.Science Press,Beijing(in Chinese).
Zhang,B.R.,Zhang,H.F.,Zhao,Z.D.,et al.,1996.Geochemical Subdivision and Evolution of the Lithosphere in East Qinling and Adjacent Regions-Implications for Tectonics.Science China Earth Sciences,26(3):201-208(in Chinese).
Zhang,C.L.,Li,M.,Wang,T.,et al.,2004.U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling.Acta Geologica Sinica(English Edition),78(1):83-95.https://doi.org/10.1111/j.1755-6724.2004.tb00678.x
Zhang,C.L.,Yu,Z.P.,Zhou,D.W.,1996.Geochemical Constraints on the Danfeng Ophiolite from the Metabasalts in Shangdan Zone of East Qinling.In:Han,S.,ed.,Symposium on Ophiolite and Geodynamics.Geological Society of China,Beijing,154-157(in Chinese).
Zhang,G.W.,Mei,Z.C.,Zhou,D.W.,et al.,1988.Formation and Evolution of the Qinling Orogenic Belt.Northwest University Press,Xi'an(in Chinese).
Zhang,G.W.,Meng,Q.R.,Lai,S.C.,1995.Structure and Tectonics of Qinling Orogenic Belt.Science in China(Series B),25(9):994-1003(in Chinese).
Zhang,G.W.,Yu,Z.P.,Dong,Y.P.,et al.,2000.On Precambrian Framework and Evolution of the Qinling Belt.Acta Petrologica Sinica,16(1):11-21(in Chinese with English abstract).
Zhang,G.W.,Zhang,B.R.,Yuan,X.C.,et al.,2001.Qinling Orogenic Belt and Continental Dynamics.Belt.Science Press,Beijing(in Chinese).
Zhang,H.F.,Ouyang,J.P.,Ling,W.L.,et al.,1996.Tectonic Division of Douling Massif of East Qinling by Pb Isotopic Compositional Characteristics.Earth Science,21(5):487-490(in Chinese with English abstract).
Zhang,H.F.,Zhang,B.R.,Luo,T.C.,1993.Geochemical Study of Genesis and Tectonic Setting for Late Proterozoic Granitoids,North Qinling,China.Earth Science,18(2):194-202(in Chinese with English abstract).
Zhang,Q.,Jiao,S.T.,Li,C.D.,et al.,2017.Granite and Continental Tectonics,Magma Thermal Field and Metallogenesis.Acta Petrologica Sinica,33(5):1524-1540(in Chinese with English abstract).
Zhang,Q.,Pan,G.Q.,Li,C.D.,et al.,2007.Are Discrimination Diagrams always Indicative of Correct Tectonic Settings of Granites?Some Crucial Questions on Granite Study(3).Acta Petrologica Sinica,23(11):2683-2698(in Chinese with English abstract).
Zhang,R.Y.,Sun,Y.,Zhang,X.,et al.,2016.Neoproterozoic Magmatic Events in the South Qinling Belt,China:Implications for Amalgamation and Breakup of the Rodinia Supercontinent.Gondwana Research,30:6-23.https://doi.org/10.1016/j.gr.2015.06.015
Zhang,S.G.,Wei,C.J.,Zhao,Z.R.,et al.,1996.Formation and Metamorphic Evolution of Douling Complex in East Qinling Mountains.Science China Earth Sciences,26(Suppl.):73-77(in Chinese).
Zhang,S.G.,Zhang,Z.Q.,Song,B.,et al.,2004.On the Existence of Neoarchean Materials in the Douling Complex,Eastern Qinling-Evidence from U-Pb SHRIMP and Sm-Nd Geochronology.Acta Geologica Sinica,78(6):800-806(in Chinese with English abstract).
Zhang,Z.Q.,Zhang,G.W.,Fu,G.M.,et al.,1996.The Age of Metamorphic Strata in Qinling Mountains and Their Tectonic Significance.Science China Earth Sciences,26(3):216-222(in Chinese).
Zhang,Z.Q.,Zhang,G.W.,Tang,S.H.,2002.Isotope Chronology of Metamorphic Strata in Southern Qinling Mountains.Geological Publishing House,Beijing(in Chinese).
Zhang,Z.Q.,Zhang,Q.,1995.Geochemistry of Metamorphosed Late Proterozoic Kuanping Ophiolite in the Northern Qinling,China.Acta Petrologica Sinica,11(Suppl.1):165-176(in Chinese with English abstract).
Zhao,J.H.,Asimow,P.D.,Zhou,M.F.,et al.,2017.An Andean-Type Arc System in Rodinia Constrained by the Neoproterozoic Shimian Ophiolite in South China.Precambrian Research,296:93-111.https://doi.org/org/10.1016/j.precamres.2017.04.017
Zhao,Z.R.,Wan,Y.S.,Zhang,S.G.,et al.,1995.The Geochemical Features of the Douling Metamorphic Complex.Acta Petrologica Sinica,11(2):148-159(in Chinese with English abstract).
Zhu,X.Y.,2010.Evolution and Provenance of the Basement in the Eastern Qinling Orogen,China:Evidence from Geochemistry and Zircon U-Pb Geochronology(Dissertation).Chinese Academy of Sciences,Beijing(in Chinese with English abstract).
Zhu,X.Y.,Chen,F.K.,Nie,H.,et al.,2014.Neoproterozoic Tectonic Evolution of South Qinling,China:Evidence from Zircon Ages and Geochemistry of the Yaolinghe Volcanic Rocks.Precambrian Research,245:115-130.https://doi.org/10.1016/j.precamres.2014.02.005
陈建林,郭原生,付善明,2004.花岗岩研究进展---ISMA花岗岩类分类综述.甘肃地质学报,13(1):67-73.
陈志宏,2004.秦岭造山带东部新元古代热-构造事件及其地质意义(博士学位论文).北京:中国地质科学院.
高剑峰,陆建军,赖鸣远,等,2003.岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学版),39(6):844-850.
李怀坤,陆松年,陈志宏,等,2003.南秦岭耀岭河群裂谷型火山岩锆石U-Pb年代学.地质通报,22(10):775-781.
李淼,2003.东秦岭陡岭群中新元古代花岗岩体的地球化学特征及其地质意义(硕士学位论文).西安:西北大学.
李献华,李武显,何斌,2012.华南陆块的形成与Rodinia超大陆聚合-裂解---观察、解释与检验.矿物岩石地球化学通报,31(6):543-559.
凌文黎,程建萍,王歆华,等,2002.武当地区新元古代岩浆岩地球化学特征及其对南秦岭晋宁期区域构造性质的指示.岩石学报,18(1):25-36.
刘丙祥,聂虎,齐玥,等,2013.豫西南地区北秦岭地体新元古代花岗岩类岩石成因及其地质意义.岩石学报,29(7):2437-2455.
刘成军,裴先治,李佐臣,等,2012.西秦岭北缘天水地区新元古代花岗质片麻岩地球化学特征及其形成环境.地质通报,31(10):1588-1601.
刘会彬,裴先治,丁仨平,等,2006.西秦岭天水市元龙地区新元古代花岗质片麻岩锆石LA-ICP-MS U-Pb定年及其地质意义.地质通报,25(11):1315-1320.
陆松年,1998.新元古时期Rodinia超大陆研究进展述评.地质论评,44(5):489-495.
陆松年,陈志宏,李怀坤,等,2005.秦岭造山带中两条新元古代岩浆岩带.地质学报,79(2):165-173.
卢欣祥,董有,尉向东,等,1999.东秦岭吐雾山A型花岗岩的时代及其构造意义.科学通报,44(9):975-978.
聂虎,2016.南秦岭东段构造热事件与地壳演化(博士学位论文).合肥:中国科学技术大学.
裴先治,丁仨平,张国伟,等,2007.西秦岭北缘新元古代花岗质片麻岩的LA-ICP-MS锆石U-Pb年龄及其地质意义.地质学报,81(6):772-786.
裴先治,张维吉,王涛,等,1995.北秦岭造山带的地质特征及其构造演化.西北地质,16(4):8-12.
沈洁,张宗清,刘敦一,1997.东秦岭陡岭群变质杂岩Sm-Nd、Rb-Sr、40 Ar/39 Ar、207 Pb/206 Pb年龄.地球学报,18(3):248-254.
时毓,于津海,裴小利,等,2014.秦岭造山带中秦岭杂岩的早古生代幔源岩浆作用.桂林理工大学学报,34(2):207-217.
时毓,于津海,徐夕生,等,2009.秦岭造山带东段秦岭岩群的年代学和地球化学研究.岩石学报,25(10):2651-2670.
苏文,刘景波,陈能松,等,2013.东秦岭-大别山及其两侧的岩浆和变质事件年代学及其形成的大地构造背景.岩石学报,29(5):1573-1593,1847.
王晓霞,王涛,张成立,等,2015.秦岭造山带花岗质岩浆作用与造山带演化.中国科学:地球科学,45(8):1109-1125.
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.
夏林圻,夏祖春,徐学义,等,1996.南秦岭中-晚元古代火山岩性质与前寒武纪大陆裂解.中国科学(D辑:地球科学),26(3):237-243.
徐备,2001.Rodinia超大陆构造演化研究的新进展和主要目标.地质科技情报,20(1):15-19.
徐通,裴先治,李瑞保,等,2017.南秦岭勉略构造带黑沟峡火山岩年代学及地球化学特征---新元古代勉略洋盆存在及俯冲的记录.地质论评,63(2):375-394.
徐通,裴先治,刘成军,等,2016.南秦岭勉略构造带张儿沟新元古代变安山岩地球化学特征及锆石LA-ICP-MSU-Pb年龄---Rodinia超大陆聚合事件的记录.地质论评,62(2):434-450.
阎明,刘树文,李秋根,等,2014.南秦岭迷魂阵岩体LA-ICP-MS锆石U-Pb年代学和Lu-Hf同位素特征.岩石学报,30(2):390-400.
杨斌虎,张成立,李雷,等,2011.东秦岭陡岭杂岩花岗岩的Sr-Nd-Pb同位素特征及其地质意义.地质通报,30(Z1):439-447.
杨朋涛,刘树文,李秋根,等,2012.南秦岭铁瓦殿岩体的成岩时代及地质意义.地质学报,86(9):1525-1540.
张本仁,高山,张宏飞,等,2002.秦岭造山带地球化学.北京:科学出版社.
张本仁,张宏飞,赵志丹,等,1996.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义.中国科学(D辑),26(3):201-208.
张成立,于在平,周鼎武,1996.东秦岭商丹带变质玄武岩地球化学特征对丹凤蛇绿岩的限制.见:韩松,编,蛇绿岩与地球动力学研讨会.北京:中国地质学会,154-157.
张国伟,梅志超,周鼎武,等,1988.秦岭造山带的形成及其演化.西安:西北大学出版社.
张国伟,孟庆任,赖绍聪,等,1995.秦岭造山带的结构构造.中国科学(B辑),25(9):994-1003.
张国伟,于在平,董云鹏,等,2000.秦岭区前寒武纪构造格局与演化问题探讨.岩石学报,16(1):11-21.
张国伟,张本仁,袁学诚,等,2001.秦岭造山带与大陆动力学.北京:科学出版社.
张宏飞,欧阳建平,凌文黎,等,1996.从Pb同位素组成特征论东秦岭陡岭块体的构造归属.地球科学,21(5):487-490.
张宏飞,张本仁,骆庭川,1993.北秦岭新元古代花岗岩类成因与构造环境的地球化学研究.地球科学,18(2):194-202.
张旗,焦守涛,李承东,等,2017.花岗岩与大陆构造、岩浆热场与成矿.岩石学报,33(5):1524-1540.
张旗,潘国强,李承东,等,2007.花岗岩构造环境问题:关于花岗岩研究的思考之三.岩石学报,23(11):2683-2698.
张寿广,张宗清,宋彪,等,2004.东秦岭陡岭杂岩中存在新太古代物质组成---SHRIMP锆石U-Pb和Sm-Nd年代学证据.地质学报,78(6):800-806.
张寿广,魏春景,赵子然,等,1996.东秦岭陡岭杂岩的形成与变质演化.中国科学(D辑:地球科学),26(S1):73-77.
张宗清,张国伟,付国民,等,1996.秦岭变质地层年龄及其构造意义.中国科学(D辑:地球科学),26(3):216-222.
张宗清,张国伟,唐索寒,2002.南秦岭变质地层同位素年代学.北京:地质出版社.
张宗清,张旗,1995.北秦岭晚元古代宽坪蛇绿岩中变质基性火山岩的地球化学特征.岩石学报,11(S1):165-176.
赵子然,万渝生,张寿广,等,1995.早元古陡岭群变质杂岩的岩石地球化学特征.岩石学报,11(2):148-159.
祝禧艳,2010.东秦岭造山带基底演化与属性:地球化学和年代学证据(博士学位论文).北京:中国科学院.