东北地区新开岭-科洛杂岩变形规律与成因
|
摘要
新开岭-科洛杂岩位于中国东北地区的嫩江-黑河构造带中,其变形规律与成因一直是制约东北地区乃至邻区构造演化的关键问题之一.据详尽的野外调查,系统分析了岩石宏观糜棱面理、矿物拉伸线理、"A"型褶皱、不对称褶皱、眼球状旋转构造和显微书斜式、眼球状旋转等构造样式.构造解析及运动学分析反映杂岩带两侧整体分别向NW及SE向的伸展滑脱特征;杂岩带内黑云斜长片麻岩及侵入糜棱岩中的闪长玢岩锆石U-Pb(LA-ICP-MS)定年及区域对比研究结果显示,其韧性变形变质作用时代为中侏罗世(167 Ma),变质峰期时限为170～163 Ma,中侏罗世晚期(163 Ma)暴露于地表.新开岭-科洛杂岩具上盘盖层、拆离韧性剪切带及下盘核杂岩3层式结构特征.核内为大面积分布的花岗岩类,地层时代远比核外地层偏新,并无"古老"的变质岩;拆离韧性剪切带变形温度约400～500℃,其变质强度达绿片岩相,后期发生明显退变质作用.新开岭-科洛岩浆核杂岩主要是在岩浆底侵、花岗岩岩体强力侵位引起地壳隆升的伸展构造背景下形成.
Xinkailing-Keluo complex, located in Nenjiang-Heihe tectonic belt, NE China, has fully undergone regional tectonic movement and therefore recorded plentiful evolution information. Its residual deformation signatures and genetic mechanisms could provide key clues about regional tectonic evolution history of not only the adjacent region but also the whole north-east area of China. Based on detailed field survey, this paper conducted systematic studies on different types of structure units, foliation of mylonite rock, stretching lineation of minerals, A-type fold, asymmetrical fold, augen-shaped rotational structure and microscopic book skew structure. The results revealed a significant fact two wings of the complex have the extension of NW and SE respectively, The mineral of zircon have been identified from internal biotite-plagioclase gneiss and intrusive dioritic-porphyrite body in mylonite country rock.Its U-Pb dating of zircon and regional study both indicated these deformation mainly occurred during Middle-Jurasic(167 Ma), and reached metamorphic peak during 170-163 Ma. Then it was uplifted by tectonic movement and exposed to the ground in late Middle-Jurasic. Xinkailing-Keluo complex was composed of three layers architecture,the upper cap rock, middle zone and lower complex.The internal part is mainly composed by granite,which are much younger than its outer part.The metamorphic temperature ranged from 400 to 500 degree, reaching extent of greenschist facies and was followed by retrograde metamorphism. Later, the regional uplift happened due to the granite magma underplating and the Xinkailing-Keluo magmatic core complex formed under regional stretch tectonic background.
Xinkailing-Keluo complex, located in Nenjiang-Heihe tectonic belt, NE China, has fully undergone regional tectonic movement and therefore recorded plentiful evolution information. Its residual deformation signatures and genetic mechanisms could provide key clues about regional tectonic evolution history of not only the adjacent region but also the whole north-east area of China. Based on detailed field survey, this paper conducted systematic studies on different types of structure units, foliation of mylonite rock, stretching lineation of minerals, A-type fold, asymmetrical fold, augen-shaped rotational structure and microscopic book skew structure. The results revealed a significant fact two wings of the complex have the extension of NW and SE respectively, The mineral of zircon have been identified from internal biotite-plagioclase gneiss and intrusive dioritic-porphyrite body in mylonite country rock.Its U-Pb dating of zircon and regional study both indicated these deformation mainly occurred during Middle-Jurasic(167 Ma), and reached metamorphic peak during 170-163 Ma. Then it was uplifted by tectonic movement and exposed to the ground in late Middle-Jurasic. Xinkailing-Keluo complex was composed of three layers architecture,the upper cap rock, middle zone and lower complex.The internal part is mainly composed by granite,which are much younger than its outer part.The metamorphic temperature ranged from 400 to 500 degree, reaching extent of greenschist facies and was followed by retrograde metamorphism. Later, the regional uplift happened due to the granite magma underplating and the Xinkailing-Keluo magmatic core complex formed under regional stretch tectonic background.
引文
Bureau of Geology and Mineral Resources of Heilongjiang Province,1993.Regional Geology of Heilongjiang Province.Geological Publishing House,Beijing(in Chinese).
Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region,1996.Stratigraphy(Lithostratic)of NeiMongol Autonomous Region.China University of Geosciences Press,Wuhan(in Chinese).
Davis,G.A.,Lister,G.S.,1988.Detachment Faulting in Continental Extension:Perspectives from the Southwestern U.S.Cordillera.Special Paper of the Geological Society of America,218:133-159.https://doi.org/10.1130/spe218-p133
Davis,G.A.,Xu,B.,Zheng,Y.D.,et al.,2004.Indosinian Extension in the Solonker Suture Zone:The Sonid Metamorphic Core Complex,Inner Mongolia,China.Earth Science Frontiers,11(9):135-143.
Gou,J.,Sun,D.Y.,Li,R.,et al.,2013.Geochronology,Geochemistry and Petrogenesis of the Early Mesozoic Granites in the Sunwu-Jiayin Area,Heilongjiang Province.Journal of Jilin University(Earth Science Edition),43(1):119-133(in Chinese with English abstract).
Li,C.L.,Qu,H.,Zhao,Z.H.,et al.,2013.Zircon U-Pb Ages,Geochemical Characteristics and Tectonic Implications of Early Carboniferous Granites in Huolongmen Area,Heilongjiang Province.Geology in China,40(3):859-868(in Chinese with English abstract).
Li,C.Y.,1982.Explanation to Tectonic Map of Asia(at 1∶8 000 000 Scale).Geological Publishing House,Beijing,13-28(in Chinese).
Li,J.Y.,He,Z.J.,Mo,S.G.,et al.,2004.The Age of Conglomerates in the Lower Part of the Xiufeng Formation in the Northern Da Hinggan Mountains,NE China,and Their Tectonic Implications.Geological Bulletin of China,23(2):120-129(in Chinese with English abstract).
Li,L.,Sun,F.Y.,Li,B.L.,et al.,2017.Geochronology of Ershi’erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance.Earth Science,42(1):35-52(in Chinese with English abstract).https://doi.org/10.1016/10.3799/dqkx.2017.003
Li,Y.,Ding,L.L.,Xu,W.L.,et al.,2015.Geochronology and Geochemistry of Muscovite Granite in Sunwu Area,NE China:Implications for the Timing of Closure of the Mongol-Okhotsk Ocean.Acta Petrologica Sinica,31(1):56-66(in Chinese with English abstract).
Li,Y.,Xu,W.L.,Wang,F.,et al.,2014.Geochronology and Geochemistry of Late Paleozoic Volcanic Rocks on the Western Margin of the Songnen-Zhangguangcai Range Massif,NE China:Implications for the Amalgamation History of the Xing’an and Songnen-Zhangguangcai Range Massifs.Lithos,205:394-410.https://doi.org/10.1016/j.lithos.2014.07.008
Liang,C.Y.,Liu,Y.J.,Li,W.,et al.,2011.Characteristics of Extensional Structure of Keluo Complex in Nenjiang Area,Heilongjiang,China.Geological Bulletin of China,30(Z1):291-299(in Chinese with English abstract).
Ludwig,K.R.,2001.Users Manual for Isoplot/Ex_ver.2.49.Berkeley Geochronology Center,Berkeley.
Mancktelow,N.S.,Pennacchioni,G.,2004.The Influence of Grain Boundary Fluids on the Microstructure of Quartz-Feldspar Mylonites.Journal of Structural Geology,26(1):47-69.https://doi.org/10.1016/s0191-8141(03)00081-6
Maruyama,S.,Send,T.,1986.Orogeny and Relative Plate Motions:Example of the Japanese Islands.Tectonophysics,127(3/4):305-329.https://doi.org/10.1016/0040-1951(86)90067-3
Miao,L.C.,Fan,W.M.,Zhang,F.Q.,et al.,2003.Zircon SHRIMP Geochronology of the Xinkailing-Kele Complex in the Northwestern Lesser Xing’an Range,and Its Geological Implications.Chinese Science Bulletin,48(22):2315-2323(in Chinese).
Passchier,C.W.,Trouw,R.A.J.,2005.Microtectonics.Springer-Verlag,Berlin,40-43.
Qu,H.,Li,C.L.,Yang,F.S.,et al.,2015.Zircon U-Pb Ages,Geochemical Characteristics and Their Geological Implication of Granitic Complex in Huolongmen Area,Northwestern Xiao Hinggan Mountains.Global Geology,34(1):34-43(in Chinese with English abstract).
Rojas-Agramonte,Y.,Kr?ner,A.,Demoux,A.,et al.,2011.Detrital and Xenocrystic Zircon Ages from Neoproterozoic to Palaeozoic Arc Terranes of Mongolia:Significance for the Origin of Crustal Fragments in the Central Asian Orogenic Belt.Gondwana Research,19(3):751-763.https://doi.org/10.1016/j.gr.2010.10.004
?eng?r,A.M.C.,Natal'in,B.A.,Burtman,V.S.,1993.Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia.Nature,364(6435):299-307.https://doi.org/10.1038/364299a0
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):572-594(in Chinese with English abstract).
Sui,Z.M.,Ge,W.C.,Wu,F.Y.,et al.,2007.Zircon U-Pb Ages,Geochemistry and Its Petrogenesis of Jurassic Granites in Northeastern Part of the Da Hinggan Mts.Acta Petrologica Sinica,23(2):461-480(in Chinese with English abstract).
Sun,D.Y.,Gou,J.,Wang,T.H.,et al.,2013.Geochronological and Geochemical Constraints on the Erguna Massif Basement,NE China-Subduction History of the Mongol-Okhotsk Oceanic Crust.International Geology Review,55(14):1801-1816.https://doi.org/10.1080/00206814.2013.804664
Wang,S.Q.,Xin,H.T.,Hu,X.J.,et al.,2016.Geochronology,Geochemistry and Geological Significance of Early Paleozoic Wulanaobaotu Intrusive Rocks,Inner Mongolia.Earth Science,41(4):555-569(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.046
Wang,Y.,Fu,J.Y.,Yang,F.,et al.,2015.Contraction and Extension in Nenjiang Heihe Tectonic Belt:Evidence from the Late Paleozoic Granitoid Geochemistry.Journal of Jilin University(Earth Science Edition),45(2):374-387(in Chinese with English abstract).
Wang,Y.,Yang,X.P.,Na,F.C.,et al.,2013.Determination and Geological Implication of the Granitic Mylonite in Nenjiang-Heihe Tectonic Belt.Geology and Resources,22(6):452-459(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.,2001.The Nature of Basement beneath the Songliao Basin in NE China:Geochemical and Isotopic Constraints.Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,26(9-10):793-803.https://doi.org/10.1016/s1464-1895(01)00128-4
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
Yan,D.P.,Zhou,M.F.,Song,H.L.,et al.,2003.Origin and Tectonic Significance of a Mesozoic Multi-Layer Over-Thrust System within the Yangtze Block(South China).Tectonophysics,361(3-4):239-254.https://doi.org/10.1016/s0040-1951(02)00646-7
Yang,W.R.,Wang,J.,Liang,X.,2012.The Major Characteristics of Geotectonics of Asia and Regularities of Evolution.Earth Science Frontiers,19(5):1-17(in Chinese with English abstract).
Yuan,H.L.,Gao,S.,Liu,X.M.,et al.,2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research,28(3):353-370.https://doi.org/10.1111/j.1751-908x.2004.tb00755.x
Zhao,H.,Zhang,J.,Wang,Y.N.,et al.,2017.The Deformation Features,Phases and Significance of Keluo Complex in Nenjiang Area,Heilongjiang Province.Geotectonica et Metallogenia,41(4):617-637(in Chinese with English abstract).
Zhao,H.B.,Mo,X.X.,Xu,S.M.,et al.,2007.Composition and Evolution of the Xinkailing Metamorphic Core Complexes in Heilongjiang Province.Chinese Journal of Geology,42(1):176-188(in Chinese with English abstract).
Zhao,Y.D.,Mo,X.X.,Li,S.C.,et al.,2015.Zircon U-Pb LA-ICP-MS Dating,Petrogeochemical Features of Granitic Mylonite in Northwestern Lesser Hinggan Mountains,and Tectonic Significance.Geological Review,61(2):443-456(in Chinese with English abstract).
Zhao,Z.,Chi,X.G.,Pan,S.Y.,et al.,2010.Zircon U-Pb LA-ICP-MS Dating of Carboniferous Volcanics and Its Geological Significance in the Northwestern Lesser Xing’an Range.Acta Petrologica Sinica,26(8):2452-2464(in Chinese with English abstract).
Zhou,J.B.,Wang,B.,Zeng,W.S.,et al.,2014.Detrital Zircon U-Pb Dating of the Zhalantun Metamorphic Complex and Its Tectonic Implications,Great Xing’an,NEChina.Acta Petrologica Sinica,30(7):1879-1888(in Chinese with English abstract).
Zeng,T.,Wang,T.,Guo,L.,et al.,2011.Ages,Origin and Geological Implications of Late Mesozoic Granitoids in Xinkailing Region,NE China.Journal of Jilin University(Earth Science Edition),41(6):1881-1900(in Chinese with English abstract).
黑龙江省地质矿产局,1993.黑龙江省区域地质志.北京:地质出版社.
内蒙古自治区地质矿产局,1996.内蒙古自治区岩石地层.武汉:中国地质大学出版社.
苟军,孙德有,李蓉,等,2013.孙吴-嘉荫地区早中生代花岗岩的年代学、地球化学与成因.吉林大学学报(地球科学版),43(1):119-133.
李成禄,曲晖,赵忠海,等,2013.黑龙江霍龙门地区早石炭世花岗岩的锆石U-Pb年龄、地球化学特征及构造意义.中国地质,40(3):859-868.
李春昱,1982.亚洲大地构造1/800万图及说明书.北京:地质出版社,13-28.
李锦轶,和政军,莫申国,等,2004.大兴安岭北部绣峰组下部砾岩的形成时代及其大地构造意义.地质通报,23(2):120-129.
李良,孙丰月,李碧乐,等,2017.漠河盆地二十二站组砂岩形成时代及物源区构造环境判别.地球科学,42(1):35-52.
李宇,丁磊磊,许文良,等,2015.孙吴地区中侏罗世白云母花岗岩的年代学与地球化学:对蒙古-鄂霍茨克洋闭合时间的限定.岩石学报,31(1):56-66.
梁琛岳,刘永江,李伟,等,2011.黑龙江嫩江地区科洛杂岩伸展构造特征.地质通报,30(Z1):291-299.
苗来成,范蔚茗,张福勤,等,2003.小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义.科学通报,48(22):2315-2323.
曲晖,李成禄,杨福深,等,2015.小兴安岭西北部霍龙门地区花岗质杂岩锆石U-Pb年龄、岩石地球化学特征及地质意义.世界地质,34(1):34-43.
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的关系.岩石学报,28(2):572-594.
隋振民,葛文春,吴福元,等,2007.大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因.岩石学报,23(2):461-480.
王树庆,辛后田,胡晓佳,等,2016.内蒙古乌兰敖包图早古生代侵入岩年代学、地球化学特征及地质意义.地球科学,41(4):555-569.
汪岩,付俊彧,杨帆,等,2015.嫩江-黑河构造带收缩与伸展-源自晚古生代花岗岩类的地球化学证据.吉林大学学报(地球科学版),45(2):374-387.
汪岩,杨晓平,那福超,等,2013.嫩江-黑河构造带中花岗质糜棱岩的确定及地质意义.地质与资源,22(6):452-459.
杨巍然,王杰,梁晓,2012.亚洲大地构造基本特征和演化规律.地学前缘,19(5):1-17.
赵衡,张进,王艳楠,等,2017.黑龙江科洛杂岩变形特征、阶段和意义.大地构造与成矿学,41(4):617-637.
赵海滨,莫宣学,徐受民,等,2007.黑龙江新开岭变质核杂岩的组成及其演化.地质科学,42(1):176-188.
赵院冬,莫宣学,李士超,等,2015.小兴安岭西北部花岗质糜棱岩锆石LA-ICP-MS U-Pb年龄、岩石地球化学特征及地质意义.地质论评,61(2):443-456.
赵芝,迟效国,潘世语,等,2010.小兴安岭西北部石炭纪地层火山岩的锆石LA-ICP-MS U-Pb年代学及其地质意义.岩石学报,26(8):2452-2464.
周建波,王斌,曾维顺,等,2014.大兴安岭地区扎兰屯变质杂岩的碎屑锆石U-Pb年龄及其大地构造意义.岩石学报,30(7):1879-1888.
曾涛,王涛,郭磊,等,2011.东北新开岭地区晚中生代花岗岩类时代、成因及地质意义.吉林大学学报(地球科学版),41(6):1881-1900.
Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region,1996.Stratigraphy(Lithostratic)of NeiMongol Autonomous Region.China University of Geosciences Press,Wuhan(in Chinese).
Davis,G.A.,Lister,G.S.,1988.Detachment Faulting in Continental Extension:Perspectives from the Southwestern U.S.Cordillera.Special Paper of the Geological Society of America,218:133-159.https://doi.org/10.1130/spe218-p133
Davis,G.A.,Xu,B.,Zheng,Y.D.,et al.,2004.Indosinian Extension in the Solonker Suture Zone:The Sonid Metamorphic Core Complex,Inner Mongolia,China.Earth Science Frontiers,11(9):135-143.
Gou,J.,Sun,D.Y.,Li,R.,et al.,2013.Geochronology,Geochemistry and Petrogenesis of the Early Mesozoic Granites in the Sunwu-Jiayin Area,Heilongjiang Province.Journal of Jilin University(Earth Science Edition),43(1):119-133(in Chinese with English abstract).
Li,C.L.,Qu,H.,Zhao,Z.H.,et al.,2013.Zircon U-Pb Ages,Geochemical Characteristics and Tectonic Implications of Early Carboniferous Granites in Huolongmen Area,Heilongjiang Province.Geology in China,40(3):859-868(in Chinese with English abstract).
Li,C.Y.,1982.Explanation to Tectonic Map of Asia(at 1∶8 000 000 Scale).Geological Publishing House,Beijing,13-28(in Chinese).
Li,J.Y.,He,Z.J.,Mo,S.G.,et al.,2004.The Age of Conglomerates in the Lower Part of the Xiufeng Formation in the Northern Da Hinggan Mountains,NE China,and Their Tectonic Implications.Geological Bulletin of China,23(2):120-129(in Chinese with English abstract).
Li,L.,Sun,F.Y.,Li,B.L.,et al.,2017.Geochronology of Ershi’erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance.Earth Science,42(1):35-52(in Chinese with English abstract).https://doi.org/10.1016/10.3799/dqkx.2017.003
Li,Y.,Ding,L.L.,Xu,W.L.,et al.,2015.Geochronology and Geochemistry of Muscovite Granite in Sunwu Area,NE China:Implications for the Timing of Closure of the Mongol-Okhotsk Ocean.Acta Petrologica Sinica,31(1):56-66(in Chinese with English abstract).
Li,Y.,Xu,W.L.,Wang,F.,et al.,2014.Geochronology and Geochemistry of Late Paleozoic Volcanic Rocks on the Western Margin of the Songnen-Zhangguangcai Range Massif,NE China:Implications for the Amalgamation History of the Xing’an and Songnen-Zhangguangcai Range Massifs.Lithos,205:394-410.https://doi.org/10.1016/j.lithos.2014.07.008
Liang,C.Y.,Liu,Y.J.,Li,W.,et al.,2011.Characteristics of Extensional Structure of Keluo Complex in Nenjiang Area,Heilongjiang,China.Geological Bulletin of China,30(Z1):291-299(in Chinese with English abstract).
Ludwig,K.R.,2001.Users Manual for Isoplot/Ex_ver.2.49.Berkeley Geochronology Center,Berkeley.
Mancktelow,N.S.,Pennacchioni,G.,2004.The Influence of Grain Boundary Fluids on the Microstructure of Quartz-Feldspar Mylonites.Journal of Structural Geology,26(1):47-69.https://doi.org/10.1016/s0191-8141(03)00081-6
Maruyama,S.,Send,T.,1986.Orogeny and Relative Plate Motions:Example of the Japanese Islands.Tectonophysics,127(3/4):305-329.https://doi.org/10.1016/0040-1951(86)90067-3
Miao,L.C.,Fan,W.M.,Zhang,F.Q.,et al.,2003.Zircon SHRIMP Geochronology of the Xinkailing-Kele Complex in the Northwestern Lesser Xing’an Range,and Its Geological Implications.Chinese Science Bulletin,48(22):2315-2323(in Chinese).
Passchier,C.W.,Trouw,R.A.J.,2005.Microtectonics.Springer-Verlag,Berlin,40-43.
Qu,H.,Li,C.L.,Yang,F.S.,et al.,2015.Zircon U-Pb Ages,Geochemical Characteristics and Their Geological Implication of Granitic Complex in Huolongmen Area,Northwestern Xiao Hinggan Mountains.Global Geology,34(1):34-43(in Chinese with English abstract).
Rojas-Agramonte,Y.,Kr?ner,A.,Demoux,A.,et al.,2011.Detrital and Xenocrystic Zircon Ages from Neoproterozoic to Palaeozoic Arc Terranes of Mongolia:Significance for the Origin of Crustal Fragments in the Central Asian Orogenic Belt.Gondwana Research,19(3):751-763.https://doi.org/10.1016/j.gr.2010.10.004
?eng?r,A.M.C.,Natal'in,B.A.,Burtman,V.S.,1993.Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia.Nature,364(6435):299-307.https://doi.org/10.1038/364299a0
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):572-594(in Chinese with English abstract).
Sui,Z.M.,Ge,W.C.,Wu,F.Y.,et al.,2007.Zircon U-Pb Ages,Geochemistry and Its Petrogenesis of Jurassic Granites in Northeastern Part of the Da Hinggan Mts.Acta Petrologica Sinica,23(2):461-480(in Chinese with English abstract).
Sun,D.Y.,Gou,J.,Wang,T.H.,et al.,2013.Geochronological and Geochemical Constraints on the Erguna Massif Basement,NE China-Subduction History of the Mongol-Okhotsk Oceanic Crust.International Geology Review,55(14):1801-1816.https://doi.org/10.1080/00206814.2013.804664
Wang,S.Q.,Xin,H.T.,Hu,X.J.,et al.,2016.Geochronology,Geochemistry and Geological Significance of Early Paleozoic Wulanaobaotu Intrusive Rocks,Inner Mongolia.Earth Science,41(4):555-569(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.046
Wang,Y.,Fu,J.Y.,Yang,F.,et al.,2015.Contraction and Extension in Nenjiang Heihe Tectonic Belt:Evidence from the Late Paleozoic Granitoid Geochemistry.Journal of Jilin University(Earth Science Edition),45(2):374-387(in Chinese with English abstract).
Wang,Y.,Yang,X.P.,Na,F.C.,et al.,2013.Determination and Geological Implication of the Granitic Mylonite in Nenjiang-Heihe Tectonic Belt.Geology and Resources,22(6):452-459(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.,2001.The Nature of Basement beneath the Songliao Basin in NE China:Geochemical and Isotopic Constraints.Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,26(9-10):793-803.https://doi.org/10.1016/s1464-1895(01)00128-4
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
Yan,D.P.,Zhou,M.F.,Song,H.L.,et al.,2003.Origin and Tectonic Significance of a Mesozoic Multi-Layer Over-Thrust System within the Yangtze Block(South China).Tectonophysics,361(3-4):239-254.https://doi.org/10.1016/s0040-1951(02)00646-7
Yang,W.R.,Wang,J.,Liang,X.,2012.The Major Characteristics of Geotectonics of Asia and Regularities of Evolution.Earth Science Frontiers,19(5):1-17(in Chinese with English abstract).
Yuan,H.L.,Gao,S.,Liu,X.M.,et al.,2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research,28(3):353-370.https://doi.org/10.1111/j.1751-908x.2004.tb00755.x
Zhao,H.,Zhang,J.,Wang,Y.N.,et al.,2017.The Deformation Features,Phases and Significance of Keluo Complex in Nenjiang Area,Heilongjiang Province.Geotectonica et Metallogenia,41(4):617-637(in Chinese with English abstract).
Zhao,H.B.,Mo,X.X.,Xu,S.M.,et al.,2007.Composition and Evolution of the Xinkailing Metamorphic Core Complexes in Heilongjiang Province.Chinese Journal of Geology,42(1):176-188(in Chinese with English abstract).
Zhao,Y.D.,Mo,X.X.,Li,S.C.,et al.,2015.Zircon U-Pb LA-ICP-MS Dating,Petrogeochemical Features of Granitic Mylonite in Northwestern Lesser Hinggan Mountains,and Tectonic Significance.Geological Review,61(2):443-456(in Chinese with English abstract).
Zhao,Z.,Chi,X.G.,Pan,S.Y.,et al.,2010.Zircon U-Pb LA-ICP-MS Dating of Carboniferous Volcanics and Its Geological Significance in the Northwestern Lesser Xing’an Range.Acta Petrologica Sinica,26(8):2452-2464(in Chinese with English abstract).
Zhou,J.B.,Wang,B.,Zeng,W.S.,et al.,2014.Detrital Zircon U-Pb Dating of the Zhalantun Metamorphic Complex and Its Tectonic Implications,Great Xing’an,NEChina.Acta Petrologica Sinica,30(7):1879-1888(in Chinese with English abstract).
Zeng,T.,Wang,T.,Guo,L.,et al.,2011.Ages,Origin and Geological Implications of Late Mesozoic Granitoids in Xinkailing Region,NE China.Journal of Jilin University(Earth Science Edition),41(6):1881-1900(in Chinese with English abstract).
黑龙江省地质矿产局,1993.黑龙江省区域地质志.北京:地质出版社.
内蒙古自治区地质矿产局,1996.内蒙古自治区岩石地层.武汉:中国地质大学出版社.
苟军,孙德有,李蓉,等,2013.孙吴-嘉荫地区早中生代花岗岩的年代学、地球化学与成因.吉林大学学报(地球科学版),43(1):119-133.
李成禄,曲晖,赵忠海,等,2013.黑龙江霍龙门地区早石炭世花岗岩的锆石U-Pb年龄、地球化学特征及构造意义.中国地质,40(3):859-868.
李春昱,1982.亚洲大地构造1/800万图及说明书.北京:地质出版社,13-28.
李锦轶,和政军,莫申国,等,2004.大兴安岭北部绣峰组下部砾岩的形成时代及其大地构造意义.地质通报,23(2):120-129.
李良,孙丰月,李碧乐,等,2017.漠河盆地二十二站组砂岩形成时代及物源区构造环境判别.地球科学,42(1):35-52.
李宇,丁磊磊,许文良,等,2015.孙吴地区中侏罗世白云母花岗岩的年代学与地球化学:对蒙古-鄂霍茨克洋闭合时间的限定.岩石学报,31(1):56-66.
梁琛岳,刘永江,李伟,等,2011.黑龙江嫩江地区科洛杂岩伸展构造特征.地质通报,30(Z1):291-299.
苗来成,范蔚茗,张福勤,等,2003.小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义.科学通报,48(22):2315-2323.
曲晖,李成禄,杨福深,等,2015.小兴安岭西北部霍龙门地区花岗质杂岩锆石U-Pb年龄、岩石地球化学特征及地质意义.世界地质,34(1):34-43.
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的关系.岩石学报,28(2):572-594.
隋振民,葛文春,吴福元,等,2007.大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因.岩石学报,23(2):461-480.
王树庆,辛后田,胡晓佳,等,2016.内蒙古乌兰敖包图早古生代侵入岩年代学、地球化学特征及地质意义.地球科学,41(4):555-569.
汪岩,付俊彧,杨帆,等,2015.嫩江-黑河构造带收缩与伸展-源自晚古生代花岗岩类的地球化学证据.吉林大学学报(地球科学版),45(2):374-387.
汪岩,杨晓平,那福超,等,2013.嫩江-黑河构造带中花岗质糜棱岩的确定及地质意义.地质与资源,22(6):452-459.
杨巍然,王杰,梁晓,2012.亚洲大地构造基本特征和演化规律.地学前缘,19(5):1-17.
赵衡,张进,王艳楠,等,2017.黑龙江科洛杂岩变形特征、阶段和意义.大地构造与成矿学,41(4):617-637.
赵海滨,莫宣学,徐受民,等,2007.黑龙江新开岭变质核杂岩的组成及其演化.地质科学,42(1):176-188.
赵院冬,莫宣学,李士超,等,2015.小兴安岭西北部花岗质糜棱岩锆石LA-ICP-MS U-Pb年龄、岩石地球化学特征及地质意义.地质论评,61(2):443-456.
赵芝,迟效国,潘世语,等,2010.小兴安岭西北部石炭纪地层火山岩的锆石LA-ICP-MS U-Pb年代学及其地质意义.岩石学报,26(8):2452-2464.
周建波,王斌,曾维顺,等,2014.大兴安岭地区扎兰屯变质杂岩的碎屑锆石U-Pb年龄及其大地构造意义.岩石学报,30(7):1879-1888.
曾涛,王涛,郭磊,等,2011.东北新开岭地区晚中生代花岗岩类时代、成因及地质意义.吉林大学学报(地球科学版),41(6):1881-1900.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |