内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义
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摘要
晶洞花岗岩成因类型和大地构造背景等方面的研究,目前颇具争议.先前的研究认为晶洞碱长、正长花岗岩属于A型花岗岩,形成于伸展环境,近年来的研究发现其成因类型具多样性.报道了博克图晶洞花岗岩的岩石学、岩石地球化学、年代学等方面的特征.SHRIMP锆石U-Pb定年结果为140.8±2.2Ma,指示其属于早白垩世的产物.且其具有高SiO_2,高ALK(Na_2O+K_2O)(7.99%～8.43%),K_2O/Na_2O=1.0～1.1,以及低的FeOT(1.15%～1.30%).微量元素富Th、U、Cs、Rb,贫Ba、Sr、P、Ti,10 000*Ga/Al、总稀土含量以及Zr+Nb+Y+Ce值均低于A型花岗岩最低平均值,由此指示其应属于Ⅰ型花岗岩,Hf同位素特征显示其成分为新生地壳来源.动力学机制上,博克图晶洞花岗岩主要受制于早白垩世时期蒙古-鄂霍次克洋闭合作用.在东北地区岩石圈由增厚到减薄转换事件中,早期的新生地壳在地幔物质的底侵作用下发生低程度的部分熔融作用.
Genetic types and tectonic backgrounds of miarolitic granite are still controversial.Previous studies have suggested that miarolitic alkali feldspar granites and miarolitic syenite granites belong to A-type granite formed in extensional environment.However,recent studies have found the diversity of the genetic types.In this paper,the petrology,geochemistry and geochronology of Boketu miarolite pluton are present.The zircon SHRIMP U-Pb dating results yield an age of 140.8±2.2 Ma,belonging to the Early Cretaceous.The pluton is characterized by high SiO_2 content,and full high alkali content(7.99%-8.43%),with high K_2 O/Na_2 O(1.0-1.1);low total Fe content(1.15%-1.30%).On the primitive mantle-normalized spider diagrams,the granite is characterized by positive Th,U,Cs,Rb anomalies and negative Ba,Sr,P,Ti anomalies.10 000*Ga/Al ratio,the total rare earth content and Zr+Nb+Y+Ce values are lower than the minimum value of the A-type granites.It is indicated that it should belong to Ⅰ-type granite.Hf isotope compositions show the source of juvenile crust.It is mainly restricted by the closure of the Mongolian-Okhotsk ocean,during which the lithosphere transformation from thickening to thinning took place.The granites are formed by the low-degree partial melting of juvenile crust in the underplating of the mantle.
Genetic types and tectonic backgrounds of miarolitic granite are still controversial.Previous studies have suggested that miarolitic alkali feldspar granites and miarolitic syenite granites belong to A-type granite formed in extensional environment.However,recent studies have found the diversity of the genetic types.In this paper,the petrology,geochemistry and geochronology of Boketu miarolite pluton are present.The zircon SHRIMP U-Pb dating results yield an age of 140.8±2.2 Ma,belonging to the Early Cretaceous.The pluton is characterized by high SiO_2 content,and full high alkali content(7.99%-8.43%),with high K_2 O/Na_2 O(1.0-1.1);low total Fe content(1.15%-1.30%).On the primitive mantle-normalized spider diagrams,the granite is characterized by positive Th,U,Cs,Rb anomalies and negative Ba,Sr,P,Ti anomalies.10 000*Ga/Al ratio,the total rare earth content and Zr+Nb+Y+Ce values are lower than the minimum value of the A-type granites.It is indicated that it should belong to Ⅰ-type granite.Hf isotope compositions show the source of juvenile crust.It is mainly restricted by the closure of the Mongolian-Okhotsk ocean,during which the lithosphere transformation from thickening to thinning took place.The granites are formed by the low-degree partial melting of juvenile crust in the underplating of the mantle.
引文
Bonin,B.,2007.A-Type Granites and Related Rocks:Evolution of a Concept,Problems and Prospects.Lithos,97(1-2):1-29.https://doi.org/10.1016/j.lithos.2006.12.007
Chappell,B.W.,White,A.J.R.,1974.Two Contrasting Granite Types.Pacic Geology,8:173-174.
Chappell,B.W.,White,A.J.R.,2001.Two Contrasting Granite Types:25Years Later.Australian Journal of Earth Sciences,48(4):489-499.https://doi.org/10.1046/j.1440-0952.2001.00882.x
Chen,A.X.,Zhou,D.,Zhang,Q.K.,et al.,2018.Age,Geochemistry,and Tectonic Implications of Dulaerqiao Granite,Inner Mongolia.Journal of Earth Science,29(1):78-92.https://doi.org/10.1007/s12583-017-0817-6
Chen,C.Y.,Gao,Y.F.,Wu,H.B.,et al.,2016.Zircon U-Pb Chronology of Volcanic Rocks in the Hailaer Basin,NEChina and Its Geological Implications.Earth Science,41(8):1259-1274(in Chinese with English abstract).
Collins,W.J.,Beams,S.D.,White,A.J.R.,et al.,1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200.https://doi.org/10.1007/bf00374895
Davis,G.A.,Zheng,Y.D.,Wang,C.,et al.,2001.Mesozoic Tectonic Evolution of the Yanshan Fold and Thrust Belt,with Emphasis on Hebei and Liaoning Provinces,Northern China.Memoir of the Geological Society of America,194(194):171-197.https://doi.org/10.1130/0-8137-1194-0.171
Deng,J.F.,Luo,Z.H.,Su,S.G.,et al.,2004.Rock Origin,Tectonic Environment and Mineralization.Geological Publishing House,Bejing(in Chinese).
Deng,J.F.,Zhao,H.L.,Mo,X.X.,et al.,1996.Continent RootsPlume Tectonic of China-Key to the Continental Dynamics.Geological Publishing House,Beijng(in Chinese).
Dickinson,W.R.,1971.Plate Tectonics in Geologic History.Science,174(4005):107-113.https://doi.org/10.1126/science.174.4005.107
Didier,J.,Lameyre,J.,1969.Les Granites du Massif Central Fran9ais:Etude Comparée des Leucogranites et Granodiorites.Contributions to Mineralogy and Petrology,24(3):219-238.https://doi.org/10.1007/bf00376049
Dong,S.W.,Li,T.D.,Zhong,D.L.,et al.,2009.Recent Progress and Perspective of the Research on J-K East Asian Multi-Direction Convergent Tectonics.Bulletin of National Natural Science Foundation of China,23(5):281-286(in Chinese with English abstract).
Eby,G.N.,1990.The A-Type Granitoids:A Review of Their Occurrence and Chemical Characteristics and Speculations on Their Petrogenesis.Lithos,26(1-2):115-134.https://doi.org/10.1016/0024-4937(90)90043-z
Hong,D.W.,Wang,S.G.,Xie,X.L.,et al.,2000.Genesis of Positiveε(Nd,t)Granitoids in the Da HingganMts.-Mongolia Orogenic Belt and Growth Continental Crust.Earth Science Frontiers,7(2):441-456(in Chinese with English abstract).
Hou,K.J.,Li,Y.H.,Xie,G.Q.,2007.LA-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon.Journal ofChinese MassSpectrometry Society,28(Suppl.):26-28(in Chinese with English abstract).
King,P.L.,White,A.J.R.,Chappell,B.W.,et al.,1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt,Southeastern Australia.Journal of Petrology,38(3):371-391.https://doi.org/10.1093/petroj/38.3.371
Li,J.Y.,Guo,F.,Li,C.W.,et al.,2014.Neodymium Isotopic Variations of Late Paleozoic to Mesozoic I-and A-Type Granitoids in NE China:Implications for Tectonic Evolution.Acta Petrologica Sinica,30(7):1995-2008(in Chinese with English abstract).
Li,J.Y.,Zhang,J.,Yang,T.N.,et al.,2009.Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas.Journal of Jilin University(Earth Science Edition),39(4):584-605(in Chinese with English abstract).
Li,P.Z.,Yu,J.S.,1993.Nianzishan Miarolitic Alkaline Granite Stock,Heilongjiang-Its Ages and Geological Implications.Geochimica,22(4):389-398(in Chinese with English abstract).
Lin,Q.,Ge,W.C.,Wu,F.Y.,et al.,2004.Geochemistry of Mesozoic Granites in Da Hinggan Ling Ranges.Acta Petrologica Sinica,20(3):403-412(in Chinese with English abstract).
Liu,C.,Deng,J.F.,Xu,L.Q.,et al.,2011.A Preliminary Frame of Magma-Tectonic-Mo Metallogenic Events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains Areas.Earth Science Frontiers,18(3):166-178(in Chinese with English abstract).
Liu,C.S.,Chen,X.M.,Chen,P.R.,et al.,2003.Subdivision,Discrimination Criteria and Genisis for A Type Rock Suites.Geological Journal of China Universities,9(4):573-591(in Chinese with English abstract).
Loiselle,M.C.,Wones,D.R.,1979,Characteristics and Origin of Anorogenic Granites.Geol.Soc.Am.Abstr.with Progr.,11,468.
Luo,Z.H.,Huang,Z.M.,Ke,S.,2007.An Overview of Granitoid.Geological Review,53(S1):180-226(in Chinese with English abstract).
Ma,C.Q.,1989.Magma-Dynamical Conditions on Crystallization Differentiation.Earth Science,14(3):245-252(in Chinese with English abstract).
Ma,Y.F.,Liu,Y.J.,Wen,Q.B.,et al.,2017.Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm.at Central Part of Great Xing'an Range.Earth Science,42(12):2146-2173(in Chinese with English abstract).
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Mo,S.G.,Han,M.L.,Li,J.Y.,2005.Compositions and Orogenic Processes of Mongolia-Okhotsk Orogen.Journal of Shandong University of Science and Technology(Natural Science),24(3):50-52,64(in Chinese with English abstract).
Nowell,G.M.,Kempton,P.D.,Noble,S.R.,et al.,1998.High Precision Hf Isotope Measurements of MORB and OIB by Thermal Ionisation Mass Spectrometry:Insights into the Depleted Mantle.Chemical Geology,149(3-4):211-233.https://doi.org/10.1016/s0009-2541(98)00036-9
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
Qiu,J.S.,Xiao,E.,Hu,J.,et al.,2008.Petrogenesis of Highly Fractionated I-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology,Geochemistry and Nd-Hf Isotopes.Acta Petrologica Sinica,24(11):2468-2484(in Chinese with English abstract).
Shao,J.A.,1991.Crust Evolution in the Middle Part of the Northern Margin of Sino-Korean Plate.Peking University Press,Beijing(in Chinese).
Shao,J.A.,Zhang,L.Q.,Mu,B.L.,et al.2007.Upwelling of Da Hinggan Mountains and Its Geodynamic Background.Geological Publishing House,Beijing,1-6(in Chinese).
She,H.Q.,Li,J.W.,Xiang,A.P.,et al.,2012.U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution.Acta Petrologica Sinica,28(2):571-594(in Chinese with English abstract).
Shi,G.H.,Miao,L.C.,Zhang,F.Q.,et al.2004.Timing and Tectonic Significance of A Type Granite from Xilin Hot,Inner Mongolia.Chinese Science Bulletin,49(4):384-389(in Chinese).
Song,B.,Zhang,Y.H.,Wan,Y.S.,et al.,2002.Mount Making and Procedure of the SHRIMP Dating.Geological Review,48(S1):26-30(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
Tong,Y.,Hong,D.W.,Wang,T.,et al.,2010.Spatial and Temporal Distribution of Granitoids in the Middle Segment of the Sino-Mongolian Border and Its Tectonic and Metallogenic Implications.Acta Geoscientica Sinica,31(3):395-412(in Chinese with English abstract).
Watson,E.B.,Harrison,T.M.,1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters,64(2):295-304.https://doi.org/10.1016/0012-821x(83)90211-x
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Winther,K.T.,1996.An Experimentally Based Model for the Origin of Tonalitic and Trondhjemitic Melts.Chemical Geology,127(1-3):43-59.https://doi.10.1016/0009-2541(95)00087-9
Wu,F.Y.,Jahn,B.M.,Wilde,S.A.,et al.2003.Highly Fractionated I-Type Granites in NE China(I):Geochronology and Petrogenesis.Lithos,66(3-4):241-273.https://doi.org/10.1016/S0024-4937(02)00222-0
Wu,F.Y.,Li,X.H.,Yang,J.H.,et al.,2007a.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Wu,F.Y.,Li,X.H.,Zheng,Y.F.,et al.,2007b.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica,23(2):185-220(in Chinese with English abstract).
Wu,F.Y.,Sun,D.Y.,Ge,W.C.,et al.,2011.Geochronology of the Phanerozoic Granitoids in Northeastern China.Journal of Asian Earth Sciences,41(1):1-30.https://doi.org/10.1016/j.jseaes.2010.11.014
Wu,F.Y.,Sun,D.Y.,Li,H.M.,et al.,2002.A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis.Chemical Geology,187(1-2):143-173.https://doi.org/10.1016/s0009-2541(02)00018-9
Wu,F.Y.,Sun,D.Y.,Lin,Q.,1999.Petrogenesis of the Phanerozoic Granites and Crustal Growth in Northeast China.Acta Petrologica Sinica,15(2):181-189(in Chinese with English abstract).
Wu,F.Y.,Yang,Y.H.,Xie,L.W.,et al.,2006.Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology.Chemical Geology,234(1-2):105-126.https://doi.org/10.1016/j.chemgeo.2006.05.003
Wu,G.,Chen,Y.J.,Zhao,Z.H.,et al.,2009.Geochemistry,Zircon SHRIMP U-Pb Age and Petrogenesis of the East Luoguhe Granites at the Northern End of the Great Hinggan Range.Acta Petrologica Sinica,25(2):233-247(in Chinese with English abstract).
Xu,M.J.,Xu,W.L.,Wang,F.,et al.,2013.Geochronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range,NE China and Its Tectonic Implications.Acta Petrologica Sinica,29(2):354-368(in Chinese with English abstract).
Xu,W.L.,Wang,F.,Pei,F.P.,et al.,2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NEChina:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica,29(2):339-353(in Chinese with English abstract).
Zhang,J.H.,2009.Geochronology and Geochemistry of the Mesozoic Volcanic Rocks in the Great Xing'an Range,Northeastern China(Dissertation).China University of Geosciences,Wuhan(in Chinese with English abstract).
Zhang,K.F.,Deng,B.,Zhang,F.Q.,et al.,2016.Determination of Early Stage of Early Cretaceous Compressive Event in Hailar Basin,NE China,and Its Tectonic Significance.Earth Science,41(7):1141-1155(in Chinese with English abstract).
Zhang,K.X.,Pan,G.T.,He,W.H.,et al.,2015.New Division of Tectonic-Strata Superregion in China.Earth Science,40(2):206-233(in Chinese with English abstract).
Zhang,Q.,2012.Could Granitic Magmas Experience Fractionation and Evolution?Acta Petrologica et Mineralogica,31(2):252-260(in Chinese with English abstract).
Zhang,Q.,2013.Is the Mesozoic Magmatism in Eastern China Related to the Westward Subduction of the Pacific Plate?Acta Petrologica et Mineralogica,32(1):113-128(in Chinese with English abstract).
Zhang,Q.,Wang,Y.,Li,C.D.,et al.,2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica,22(9):2249-2269(in Chinese with English abstract).
Zhang,X.Z.,Yang,B.J.,Wu,F.Y.,et al.,2006.The Lithosphere Structure in the Hingmong-Jihei(HingganMongolia-Jilin-Heilongjiang)Region,Northeastern China.Geology in China,33(4):816-823(in Chinese with English abstract).
Zhang,Z.M.,Kang,D.Y.,Ding,H.X.,et al.,2018.Partial Melting of Himalayan Orogen and Formation Mechanism of Leucogranites.Earth Science,43(1):82-98(in Chinese with English abstract).
Zhao,S.,Xu,W.L.,Tang,J.,et al.,2016.Neoproterozoic Magmatic Events 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).
Zhao,X.C.,Zhou,W.X.,Fu,D.,et al.,2018.Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot,Inner Mongolia,China.Journal of Earth Science,29(2):280-294.https://doi.org/10.1007/s12583-017-0942-2
Zheng,Y.D.,Davis,G.A.,Wang,C.,et al.,2000.Major Mesozoic Tectonic Events in the Yanshan Belt and the Plate Tectonic Setting.Acta Geologica Sinica,74(4):289-302(in Chinese with English abstract).
Zonenshain,L.P.,Muznin,M.I.,Natapov,L.M.,1990.Mongol-Okhotsk Fold Belt.In:Page,B.M.,ed.,Geology of the USSR:A Plate Tectonic Synthesis.Geophysical Union Gedynamic Series,21:97-120.
Zorin,Y.A.,1999.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt,Trans-Baikal Region(Russia)and Mongolia.Tectonophysics,306(1):33-56.https://doi.org/10.1016/s0040-1951(99)00042-6
陈崇阳,高有峰,吴海波,等,2016.海拉尔盆地火山岩的锆石U-Pb年龄及其地质意义.地球科学,41(8):1259-1274.
邓晋福,罗照华,苏尚国,等,2004.岩石成因、构造环境与成矿作用.北京:地质出版社.
邓晋福,赵海玲,莫宣学,等,1996.中国大陆根柱构造大陆动力学的钥匙.北京:地质出版社.
董树文,李廷栋,钟大赉,等,2009.侏罗纪/白垩纪之交东亚板块汇聚的研究进展和展望.中国科学基金,23(5):281-286.
洪大卫,王式洸,谢锡林,等,2000.兴蒙造山带正ε(Nd,t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456.
侯可军,李延河,谢桂青,2007.锆石Hf同位素的LA-MC-ICP-MS分析方法.质谱学报,28(增刊):26-28.
李锦轶,张进,杨天南,等,2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版),39(4):584-605.
李竞妍,郭锋,李超文,等,2014.东北地区晚古生代-中生代I型和A型花岗岩Nd同位素变化趋势及其构造意义.岩石学报,30(7):1995-2008.
李培忠,于津生,1993.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义.地球化学,22(4):389-398.
林强,葛文春,吴福元,等,2004.大兴安岭中生代花岗岩类的地球化学.岩石学报,20(3):403-412.
刘昌实,陈小明,陈培荣,等,2003.A型岩套的分类、判别标志和成因.高校地质学报,9(4):573-591.
刘翠,邓晋福,许立权,等,2011.大兴安岭-小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架.地学前缘,18(3):166-178.
罗照华,黄忠敏,柯珊,2007.花岗质岩石的基本问题.地质论评,53(S1):180-226.
马昌前,1989.结晶分异作用的岩浆动力学条件.地球科学,14(3):245-252.
马永非,刘永江,温泉波,等,2017.大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景.地球科学,42(12):2146-2173.
莫申国,韩美莲,李锦轶,2005.蒙古-鄂霍茨克造山带的组成及造山过程.山东科技大学学报(自然科学版),24(3):50-52,64.
邱检生,肖娥,胡建,等,2008.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报,24(11):2468-2484.
邵济安,1991.中朝板块北缘中段地壳演化.北京:北京大学出版社.
邵济安,张履桥,牟保磊,等,2007.大兴安岭的隆起与地球动力学背景.北京:地质出版社,1-6.
佘宏全,李进文,向安平,等,2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报,28(2):571-594.
施光海,苗来成,张福勤,等,2004.内蒙古锡林浩特A型花岗岩的时代及区域构造意义.科学通报,49(4):384-389.
宋彪,张玉海,万渝生,等,2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(S1):26-30.
童英,洪大卫,王涛,等,2010.中蒙边境中段花岗岩时空分布特征及构造和找矿意义.地球学报,31(3):395-412.
吴福元,李献华,杨进辉,等,2007a.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238.
吴福元,李献华,郑永飞,等,2007b.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220.
吴福元,孙德有,林强,1999.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,15(2):181-189.
武广,陈衍景,赵振华,等,2009.大兴安岭北端洛古河东花岗岩的地球化学、SHRIMP锆石U-Pb年龄和岩石成因.岩石学报,25(2):233-247.
徐美君,许文良,王枫,等,2013.小兴安岭中部早侏罗世花岗质岩石的年代学与地球化学及其构造意义.岩石学报,29(2):354-368.
许文良,王枫,裴福萍,等,2013.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.岩石学报,29(2):339-353.
张吉衡,2009.大兴安岭中生代火山岩年代学及其地球化学研究(博士学位论文).武汉:中国地质大学.
张科峰,邓彬,章凤奇,等,2016.海拉尔盆地早白垩世早期挤压变形事件的厘定及其构造意义.地球科学,41(7):1141-1155.
张克信,潘桂棠,何卫红,等,2015.中国构造-地层大区划分新方案.地球科学,40(2):206-233.
张旗,2012.花岗质岩浆能够结晶分离和演化吗?岩石矿物学杂志,31(2):252-260.
张旗,2013.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?岩石矿物学杂志,32(1):113-128.
张旗,王焰,李承东,等,2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报,22(9):2249-2269.
张兴洲,杨宝俊,吴福元,等,2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
张泽明,康东艳,丁慧霞,等,2018.喜马拉雅造山带的部分熔融与淡色花岗岩成因机制.地球科学,43(1):82-98.
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.
郑亚东,Davis,G.A.,王琮,等,2000.燕山带中生代主要构造事件与板块构造背景问题.地质学报,74(4):289-302.
Chappell,B.W.,White,A.J.R.,1974.Two Contrasting Granite Types.Pacic Geology,8:173-174.
Chappell,B.W.,White,A.J.R.,2001.Two Contrasting Granite Types:25Years Later.Australian Journal of Earth Sciences,48(4):489-499.https://doi.org/10.1046/j.1440-0952.2001.00882.x
Chen,A.X.,Zhou,D.,Zhang,Q.K.,et al.,2018.Age,Geochemistry,and Tectonic Implications of Dulaerqiao Granite,Inner Mongolia.Journal of Earth Science,29(1):78-92.https://doi.org/10.1007/s12583-017-0817-6
Chen,C.Y.,Gao,Y.F.,Wu,H.B.,et al.,2016.Zircon U-Pb Chronology of Volcanic Rocks in the Hailaer Basin,NEChina and Its Geological Implications.Earth Science,41(8):1259-1274(in Chinese with English abstract).
Collins,W.J.,Beams,S.D.,White,A.J.R.,et al.,1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200.https://doi.org/10.1007/bf00374895
Davis,G.A.,Zheng,Y.D.,Wang,C.,et al.,2001.Mesozoic Tectonic Evolution of the Yanshan Fold and Thrust Belt,with Emphasis on Hebei and Liaoning Provinces,Northern China.Memoir of the Geological Society of America,194(194):171-197.https://doi.org/10.1130/0-8137-1194-0.171
Deng,J.F.,Luo,Z.H.,Su,S.G.,et al.,2004.Rock Origin,Tectonic Environment and Mineralization.Geological Publishing House,Bejing(in Chinese).
Deng,J.F.,Zhao,H.L.,Mo,X.X.,et al.,1996.Continent RootsPlume Tectonic of China-Key to the Continental Dynamics.Geological Publishing House,Beijng(in Chinese).
Dickinson,W.R.,1971.Plate Tectonics in Geologic History.Science,174(4005):107-113.https://doi.org/10.1126/science.174.4005.107
Didier,J.,Lameyre,J.,1969.Les Granites du Massif Central Fran9ais:Etude Comparée des Leucogranites et Granodiorites.Contributions to Mineralogy and Petrology,24(3):219-238.https://doi.org/10.1007/bf00376049
Dong,S.W.,Li,T.D.,Zhong,D.L.,et al.,2009.Recent Progress and Perspective of the Research on J-K East Asian Multi-Direction Convergent Tectonics.Bulletin of National Natural Science Foundation of China,23(5):281-286(in Chinese with English abstract).
Eby,G.N.,1990.The A-Type Granitoids:A Review of Their Occurrence and Chemical Characteristics and Speculations on Their Petrogenesis.Lithos,26(1-2):115-134.https://doi.org/10.1016/0024-4937(90)90043-z
Hong,D.W.,Wang,S.G.,Xie,X.L.,et al.,2000.Genesis of Positiveε(Nd,t)Granitoids in the Da HingganMts.-Mongolia Orogenic Belt and Growth Continental Crust.Earth Science Frontiers,7(2):441-456(in Chinese with English abstract).
Hou,K.J.,Li,Y.H.,Xie,G.Q.,2007.LA-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon.Journal ofChinese MassSpectrometry Society,28(Suppl.):26-28(in Chinese with English abstract).
King,P.L.,White,A.J.R.,Chappell,B.W.,et al.,1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt,Southeastern Australia.Journal of Petrology,38(3):371-391.https://doi.org/10.1093/petroj/38.3.371
Li,J.Y.,Guo,F.,Li,C.W.,et al.,2014.Neodymium Isotopic Variations of Late Paleozoic to Mesozoic I-and A-Type Granitoids in NE China:Implications for Tectonic Evolution.Acta Petrologica Sinica,30(7):1995-2008(in Chinese with English abstract).
Li,J.Y.,Zhang,J.,Yang,T.N.,et al.,2009.Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas.Journal of Jilin University(Earth Science Edition),39(4):584-605(in Chinese with English abstract).
Li,P.Z.,Yu,J.S.,1993.Nianzishan Miarolitic Alkaline Granite Stock,Heilongjiang-Its Ages and Geological Implications.Geochimica,22(4):389-398(in Chinese with English abstract).
Lin,Q.,Ge,W.C.,Wu,F.Y.,et al.,2004.Geochemistry of Mesozoic Granites in Da Hinggan Ling Ranges.Acta Petrologica Sinica,20(3):403-412(in Chinese with English abstract).
Liu,C.,Deng,J.F.,Xu,L.Q.,et al.,2011.A Preliminary Frame of Magma-Tectonic-Mo Metallogenic Events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains Areas.Earth Science Frontiers,18(3):166-178(in Chinese with English abstract).
Liu,C.S.,Chen,X.M.,Chen,P.R.,et al.,2003.Subdivision,Discrimination Criteria and Genisis for A Type Rock Suites.Geological Journal of China Universities,9(4):573-591(in Chinese with English abstract).
Loiselle,M.C.,Wones,D.R.,1979,Characteristics and Origin of Anorogenic Granites.Geol.Soc.Am.Abstr.with Progr.,11,468.
Luo,Z.H.,Huang,Z.M.,Ke,S.,2007.An Overview of Granitoid.Geological Review,53(S1):180-226(in Chinese with English abstract).
Ma,C.Q.,1989.Magma-Dynamical Conditions on Crystallization Differentiation.Earth Science,14(3):245-252(in Chinese with English abstract).
Ma,Y.F.,Liu,Y.J.,Wen,Q.B.,et al.,2017.Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm.at Central Part of Great Xing'an Range.Earth Science,42(12):2146-2173(in Chinese with English abstract).
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Mo,S.G.,Han,M.L.,Li,J.Y.,2005.Compositions and Orogenic Processes of Mongolia-Okhotsk Orogen.Journal of Shandong University of Science and Technology(Natural Science),24(3):50-52,64(in Chinese with English abstract).
Nowell,G.M.,Kempton,P.D.,Noble,S.R.,et al.,1998.High Precision Hf Isotope Measurements of MORB and OIB by Thermal Ionisation Mass Spectrometry:Insights into the Depleted Mantle.Chemical Geology,149(3-4):211-233.https://doi.org/10.1016/s0009-2541(98)00036-9
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
Qiu,J.S.,Xiao,E.,Hu,J.,et al.,2008.Petrogenesis of Highly Fractionated I-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology,Geochemistry and Nd-Hf Isotopes.Acta Petrologica Sinica,24(11):2468-2484(in Chinese with English abstract).
Shao,J.A.,1991.Crust Evolution in the Middle Part of the Northern Margin of Sino-Korean Plate.Peking University Press,Beijing(in Chinese).
Shao,J.A.,Zhang,L.Q.,Mu,B.L.,et al.2007.Upwelling of Da Hinggan Mountains and Its Geodynamic Background.Geological Publishing House,Beijing,1-6(in Chinese).
She,H.Q.,Li,J.W.,Xiang,A.P.,et al.,2012.U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution.Acta Petrologica Sinica,28(2):571-594(in Chinese with English abstract).
Shi,G.H.,Miao,L.C.,Zhang,F.Q.,et al.2004.Timing and Tectonic Significance of A Type Granite from Xilin Hot,Inner Mongolia.Chinese Science Bulletin,49(4):384-389(in Chinese).
Song,B.,Zhang,Y.H.,Wan,Y.S.,et al.,2002.Mount Making and Procedure of the SHRIMP Dating.Geological Review,48(S1):26-30(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
Tong,Y.,Hong,D.W.,Wang,T.,et al.,2010.Spatial and Temporal Distribution of Granitoids in the Middle Segment of the Sino-Mongolian Border and Its Tectonic and Metallogenic Implications.Acta Geoscientica Sinica,31(3):395-412(in Chinese with English abstract).
Watson,E.B.,Harrison,T.M.,1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters,64(2):295-304.https://doi.org/10.1016/0012-821x(83)90211-x
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Winther,K.T.,1996.An Experimentally Based Model for the Origin of Tonalitic and Trondhjemitic Melts.Chemical Geology,127(1-3):43-59.https://doi.10.1016/0009-2541(95)00087-9
Wu,F.Y.,Jahn,B.M.,Wilde,S.A.,et al.2003.Highly Fractionated I-Type Granites in NE China(I):Geochronology and Petrogenesis.Lithos,66(3-4):241-273.https://doi.org/10.1016/S0024-4937(02)00222-0
Wu,F.Y.,Li,X.H.,Yang,J.H.,et al.,2007a.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Wu,F.Y.,Li,X.H.,Zheng,Y.F.,et al.,2007b.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica,23(2):185-220(in Chinese with English abstract).
Wu,F.Y.,Sun,D.Y.,Ge,W.C.,et al.,2011.Geochronology of the Phanerozoic Granitoids in Northeastern China.Journal of Asian Earth Sciences,41(1):1-30.https://doi.org/10.1016/j.jseaes.2010.11.014
Wu,F.Y.,Sun,D.Y.,Li,H.M.,et al.,2002.A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis.Chemical Geology,187(1-2):143-173.https://doi.org/10.1016/s0009-2541(02)00018-9
Wu,F.Y.,Sun,D.Y.,Lin,Q.,1999.Petrogenesis of the Phanerozoic Granites and Crustal Growth in Northeast China.Acta Petrologica Sinica,15(2):181-189(in Chinese with English abstract).
Wu,F.Y.,Yang,Y.H.,Xie,L.W.,et al.,2006.Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology.Chemical Geology,234(1-2):105-126.https://doi.org/10.1016/j.chemgeo.2006.05.003
Wu,G.,Chen,Y.J.,Zhao,Z.H.,et al.,2009.Geochemistry,Zircon SHRIMP U-Pb Age and Petrogenesis of the East Luoguhe Granites at the Northern End of the Great Hinggan Range.Acta Petrologica Sinica,25(2):233-247(in Chinese with English abstract).
Xu,M.J.,Xu,W.L.,Wang,F.,et al.,2013.Geochronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range,NE China and Its Tectonic Implications.Acta Petrologica Sinica,29(2):354-368(in Chinese with English abstract).
Xu,W.L.,Wang,F.,Pei,F.P.,et al.,2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NEChina:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica,29(2):339-353(in Chinese with English abstract).
Zhang,J.H.,2009.Geochronology and Geochemistry of the Mesozoic Volcanic Rocks in the Great Xing'an Range,Northeastern China(Dissertation).China University of Geosciences,Wuhan(in Chinese with English abstract).
Zhang,K.F.,Deng,B.,Zhang,F.Q.,et al.,2016.Determination of Early Stage of Early Cretaceous Compressive Event in Hailar Basin,NE China,and Its Tectonic Significance.Earth Science,41(7):1141-1155(in Chinese with English abstract).
Zhang,K.X.,Pan,G.T.,He,W.H.,et al.,2015.New Division of Tectonic-Strata Superregion in China.Earth Science,40(2):206-233(in Chinese with English abstract).
Zhang,Q.,2012.Could Granitic Magmas Experience Fractionation and Evolution?Acta Petrologica et Mineralogica,31(2):252-260(in Chinese with English abstract).
Zhang,Q.,2013.Is the Mesozoic Magmatism in Eastern China Related to the Westward Subduction of the Pacific Plate?Acta Petrologica et Mineralogica,32(1):113-128(in Chinese with English abstract).
Zhang,Q.,Wang,Y.,Li,C.D.,et al.,2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica,22(9):2249-2269(in Chinese with English abstract).
Zhang,X.Z.,Yang,B.J.,Wu,F.Y.,et al.,2006.The Lithosphere Structure in the Hingmong-Jihei(HingganMongolia-Jilin-Heilongjiang)Region,Northeastern China.Geology in China,33(4):816-823(in Chinese with English abstract).
Zhang,Z.M.,Kang,D.Y.,Ding,H.X.,et al.,2018.Partial Melting of Himalayan Orogen and Formation Mechanism of Leucogranites.Earth Science,43(1):82-98(in Chinese with English abstract).
Zhao,S.,Xu,W.L.,Tang,J.,et al.,2016.Neoproterozoic Magmatic Events 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).
Zhao,X.C.,Zhou,W.X.,Fu,D.,et al.,2018.Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot,Inner Mongolia,China.Journal of Earth Science,29(2):280-294.https://doi.org/10.1007/s12583-017-0942-2
Zheng,Y.D.,Davis,G.A.,Wang,C.,et al.,2000.Major Mesozoic Tectonic Events in the Yanshan Belt and the Plate Tectonic Setting.Acta Geologica Sinica,74(4):289-302(in Chinese with English abstract).
Zonenshain,L.P.,Muznin,M.I.,Natapov,L.M.,1990.Mongol-Okhotsk Fold Belt.In:Page,B.M.,ed.,Geology of the USSR:A Plate Tectonic Synthesis.Geophysical Union Gedynamic Series,21:97-120.
Zorin,Y.A.,1999.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt,Trans-Baikal Region(Russia)and Mongolia.Tectonophysics,306(1):33-56.https://doi.org/10.1016/s0040-1951(99)00042-6
陈崇阳,高有峰,吴海波,等,2016.海拉尔盆地火山岩的锆石U-Pb年龄及其地质意义.地球科学,41(8):1259-1274.
邓晋福,罗照华,苏尚国,等,2004.岩石成因、构造环境与成矿作用.北京:地质出版社.
邓晋福,赵海玲,莫宣学,等,1996.中国大陆根柱构造大陆动力学的钥匙.北京:地质出版社.
董树文,李廷栋,钟大赉,等,2009.侏罗纪/白垩纪之交东亚板块汇聚的研究进展和展望.中国科学基金,23(5):281-286.
洪大卫,王式洸,谢锡林,等,2000.兴蒙造山带正ε(Nd,t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456.
侯可军,李延河,谢桂青,2007.锆石Hf同位素的LA-MC-ICP-MS分析方法.质谱学报,28(增刊):26-28.
李锦轶,张进,杨天南,等,2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版),39(4):584-605.
李竞妍,郭锋,李超文,等,2014.东北地区晚古生代-中生代I型和A型花岗岩Nd同位素变化趋势及其构造意义.岩石学报,30(7):1995-2008.
李培忠,于津生,1993.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义.地球化学,22(4):389-398.
林强,葛文春,吴福元,等,2004.大兴安岭中生代花岗岩类的地球化学.岩石学报,20(3):403-412.
刘昌实,陈小明,陈培荣,等,2003.A型岩套的分类、判别标志和成因.高校地质学报,9(4):573-591.
刘翠,邓晋福,许立权,等,2011.大兴安岭-小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架.地学前缘,18(3):166-178.
罗照华,黄忠敏,柯珊,2007.花岗质岩石的基本问题.地质论评,53(S1):180-226.
马昌前,1989.结晶分异作用的岩浆动力学条件.地球科学,14(3):245-252.
马永非,刘永江,温泉波,等,2017.大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景.地球科学,42(12):2146-2173.
莫申国,韩美莲,李锦轶,2005.蒙古-鄂霍茨克造山带的组成及造山过程.山东科技大学学报(自然科学版),24(3):50-52,64.
邱检生,肖娥,胡建,等,2008.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报,24(11):2468-2484.
邵济安,1991.中朝板块北缘中段地壳演化.北京:北京大学出版社.
邵济安,张履桥,牟保磊,等,2007.大兴安岭的隆起与地球动力学背景.北京:地质出版社,1-6.
佘宏全,李进文,向安平,等,2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报,28(2):571-594.
施光海,苗来成,张福勤,等,2004.内蒙古锡林浩特A型花岗岩的时代及区域构造意义.科学通报,49(4):384-389.
宋彪,张玉海,万渝生,等,2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(S1):26-30.
童英,洪大卫,王涛,等,2010.中蒙边境中段花岗岩时空分布特征及构造和找矿意义.地球学报,31(3):395-412.
吴福元,李献华,杨进辉,等,2007a.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238.
吴福元,李献华,郑永飞,等,2007b.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220.
吴福元,孙德有,林强,1999.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,15(2):181-189.
武广,陈衍景,赵振华,等,2009.大兴安岭北端洛古河东花岗岩的地球化学、SHRIMP锆石U-Pb年龄和岩石成因.岩石学报,25(2):233-247.
徐美君,许文良,王枫,等,2013.小兴安岭中部早侏罗世花岗质岩石的年代学与地球化学及其构造意义.岩石学报,29(2):354-368.
许文良,王枫,裴福萍,等,2013.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.岩石学报,29(2):339-353.
张吉衡,2009.大兴安岭中生代火山岩年代学及其地球化学研究(博士学位论文).武汉:中国地质大学.
张科峰,邓彬,章凤奇,等,2016.海拉尔盆地早白垩世早期挤压变形事件的厘定及其构造意义.地球科学,41(7):1141-1155.
张克信,潘桂棠,何卫红,等,2015.中国构造-地层大区划分新方案.地球科学,40(2):206-233.
张旗,2012.花岗质岩浆能够结晶分离和演化吗?岩石矿物学杂志,31(2):252-260.
张旗,2013.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?岩石矿物学杂志,32(1):113-128.
张旗,王焰,李承东,等,2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报,22(9):2249-2269.
张兴洲,杨宝俊,吴福元,等,2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
张泽明,康东艳,丁慧霞,等,2018.喜马拉雅造山带的部分熔融与淡色花岗岩成因机制.地球科学,43(1):82-98.
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.
郑亚东,Davis,G.A.,王琮,等,2000.燕山带中生代主要构造事件与板块构造背景问题.地质学报,74(4):289-302.
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