内蒙古狼山地区早志留世石英闪长岩体的厘定及其地质意义
|
摘要
内蒙古狼山山脉西侧分布有零星的早古生代岩浆岩,早志留世侵入体主要出露于哈日音熬瑞-迈罕陶勒盖一带.该岩体岩性为石英闪长岩,LA-ICP-MS锆石U-Pb年龄显示,其~(206)Pb/~(238)U加权平均年龄为440±1Ma.岩石富集大离子亲石元素Rb、K、Pb,不同程度地亏损高场强元素Nb、Ta、P、Ti;轻稀土富集,重稀土亏损,具有弱的负Eu异常,显示了岩浆弧的地球化学特征ε.Hf(t)值为-12.1～-8.8及TDM2在1 973～2 182Ma之间,反映了源区以古元古代古老地壳为主,闪长质包体中的斜长石斑晶及矿物成因判别图解显示了岩体在形成过程中受到了岩浆混合作用.构造判别图解及Hf同位素特征表明该岩体可能形成于大陆边缘弧的构造背景.对比达茂旗、白乃庙地区新近发表的有关数据,早志留世石英闪长岩的岩石地球化学特征与之十分相似,由此可见,华北地块北缘早古生代俯冲带从白乃庙地区可以延伸到狼山地区.
The Early Paleozoic magmatites are sporadically distributed along the western side of the Langshan Mountains,Inner Mongolia.The Early Silurian rocks are mainly exposed in the zone of Hariyinaorui-Maihantaolegai.LA-ICP-MS zircon U-Pb dating shows that the ~(206)Pb/~(238)U weighted average age of quartz diorite is 440±1 Ma.The rocks show similar chondrite-normalized REE patterns,and display relatively high concentration of light rare earth elements(LREEs)but low contents of heavy rare earth elements(HREEs)with minor negative Eu anomalies.The overall chemical similarities of these rocks on the primitive mantle-normalized variation diagrams display affinity to arc signature;considering both tectonic discriminated diagrams and the Hf isotopic signature,it is proposed that the Langshan area was under the tectonic setting of continental margin arc during Early Silurian.It is concluded that the subduction zone of Early Paleozoic had been extended from the area of Damaoqi to Langshan,since these rocks show similar geochemical characteristics with the recently published data of Early Silurian quartz diorite in the area of Damaoqi and Bainaimiao.
The Early Paleozoic magmatites are sporadically distributed along the western side of the Langshan Mountains,Inner Mongolia.The Early Silurian rocks are mainly exposed in the zone of Hariyinaorui-Maihantaolegai.LA-ICP-MS zircon U-Pb dating shows that the ~(206)Pb/~(238)U weighted average age of quartz diorite is 440±1 Ma.The rocks show similar chondrite-normalized REE patterns,and display relatively high concentration of light rare earth elements(LREEs)but low contents of heavy rare earth elements(HREEs)with minor negative Eu anomalies.The overall chemical similarities of these rocks on the primitive mantle-normalized variation diagrams display affinity to arc signature;considering both tectonic discriminated diagrams and the Hf isotopic signature,it is proposed that the Langshan area was under the tectonic setting of continental margin arc during Early Silurian.It is concluded that the subduction zone of Early Paleozoic had been extended from the area of Damaoqi to Langshan,since these rocks show similar geochemical characteristics with the recently published data of Early Silurian quartz diorite in the area of Damaoqi and Bainaimiao.
引文
Allen,M.B.,Windley,B.F.,Zhang,C.,1993.Palaeozoic Collisional Tectonics and Magmatism of the Chinese Tien Shan,Central Asia.Tectonophysics,220(1-4):89-115.https://doi.org/10.1016/0040-1951(93)90225-9
Allen,M.B.,Engor,A.M.C.,Natal'in,B.A.,1995.Junggar,Turfan and Alakol Basins as Late Permian to?Early Triassic Extensional Structures in a Sinistral Shear Zone in the Altaid Orogenic Collage,Central Asia.Journal of the Geological Society,152(2):327-338.https://doi.org/10.1144/gsjgs.152.2.0327
Batchelor,R.A.,Bowden,P.,1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology,48(1-4):43-55.https://doi.org/10.1016/0009-2541(85)90034-8
Coleman,R.G.,1989.Continental Growth of Northwest China.Tectonics,8(3):621-635.https://doi.org/10.1029/tc008i003p00621
Defant,M.J.,Drummond,M.S.,1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature,347(6294):662-665.https://doi.org/10.1038/347662a0
Feng,J.Y.,Xiao,W.J.,Windley,B.,et al.,2013.Field Geology,Geochronology and Geochemistry of MaficUltramafic Rocks from Alxa,China:Implications for Late Permian Accretionary Tectonics in the Southern Altaids.Journal of Asian Earth Sciences,78:114-142.https://doi.org/10.1016/j.jseaes.2013.01.020
Gao,J.,Li,M.S.,Xiao,X.C.,et al.,1998.Paleozoic Tectonic Evolution of the Tianshan Orogen,Northwestern China.Tectonophysics,287(1-4):213-231.https://doi.org/10.1016/s0040-1951(98)80070-x
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
Han,B.F.,He,G.Q.,Wang,X.C.,et al.,2011.Late Carboniferous Collision between the Tarim and Kazakhstan-Yili Terranes in the Western Segment of the South Tian Shan Orogen,Central Asia,and Implications for the Northern Xinjiang,Western China.Earth-Science Reviews,109(3-4):74-93.https://doi.org/10.1016/j.earscirev.2011.09.001
Jahn,B.M.,Griffin,W.L.,Windley,B.,2000.Continental Growth in the Phanerozoic:Evidence from Central Asia.Tectonophysics,328(1-2):vii-x.https://doi.org/10.1016/s0040-1951(00)00174-8
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2008.Time Scale of an Early to Mid-Paleozoic Orogenic Cycle of the LongLived Central Asian Orogenic Belt,Inner Mongolia of China:Implications for Continental Growth.Lithos,101(3-4):233-259.https://doi.org/10.1016/j.lithos.2007.07.005
Kuno,H.,1968.“Differentiation of Basaltic Magmas”.In:Hess,H.Arie Poldervaart,A.,eds.,Basalts:The Poldervaart Treatise on Rocks of Basaltic Composition(vol.2).Interscience,New York,623-688.
Li,C.D.,Ran,H.,Zhao,L.G.,et al.,2012.LA-MC-ICPMS U-Pb Geochronology of Zircons from the Wenduermiao Group and Its Tectonic Significance.Acta Petrologica Sinica,28(11):3705-3714(in Chinese with English abstract).
Li,H.K.,Geng,J.Z.,Hao,S.,et al.,2009.Study on the Using LA-MC-ICPMS to Date the U-Pb Isotopic Age of Zircons.Bulletin of Mineralogy,29(S1):600-601(in Chinese with English abstract).
Liu,Y.S.,Gao,S.,Hu,Z.C.,et al.,2010.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating,Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths.Journal of Petrology,51(1-2):537-571.https://doi.org/10.1093/petrology/egp082
Ludwig,K.R.,2003.Users Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,Berkeley,1-39.
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
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
Qian X.Y.,Zhang Z.C.,Chen Y.,et al.,2017.Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area,Inner Mongolia and Their Tectonic Significance.Earth Science,42(9):1472-1494(in Chinese with English abstract).
Sengor,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
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,Z.Z.,Han,B.F.,Feng,L.X.,et al.,2015.Geochronology,Geochemistry and Origins of the Paleozoic-Triassic Plutons in the Langshan Area,Western Inner Mongolia,China.Journal of Asian Earth Sciences,97:337-351.
Wilson,M.,1989.Igneous Petrogenesis.Unwin Hyman,London.
Windley,B.F.,Allen,M.B.,Zhang,C.,et al.,1990.Paleozoic Accretion and Cenozoic Redeformation of the Chinese Tien Shan Range,Central Asia.Geology,18(2):128.
Windley,B.F.,Alexeiev,D.,Xiao,W.J.,et al.,2007.Tectonic Models for Accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164(1):31-47.
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,Y.F.,Zeng,J.N.,Cao,J.J.,et al.,2013.Zircon U-Pb Ages and Hf Isotopes of Hercynian Intrusion in Dongshengmiao,Inner Mongolia.Geological Science and Technology Information,32(6):22-30(in Chinese with English abstract).
Xiao,W.J.,Han,C.M.,Yuan,C.,et al.,2008.Middle Cambrian to Permian Subduction-Related Accretionary Orogenesis of Northern Xinjiang,NW China:Implications for the Tectonic Evolution of Central Asia.Journal of Asian Earth Sciences,32(2-4):102-117.https://doi.org/10.1016/j.jseaes.2007.10.008
Xiao,W.J.,Zhang,L.C.,Qin,K.Z.,et al.,2004.Paleozoic Accretionary and Collisional Tectonics of the Eastern Tianshan(China):Implications for the Continental Growth of Central Asia.American Journal of Science,304(4):370-395.https://doi.org/10.2475/ajs.304.4.370
Xie,Y.W.,Zhang,Y.Q.,1990.Peculiarities and Genetic Significance of Hornblende from Granite in the Hengduanshan Region.Acta Mineralogica Sinica,10(1):35-45(in Chinese with English abstract).
Xu,B.,Charvet,J.,Chen,Y.,et al.,2013.Middle Paleozoic Convergent Orogenic Belts in Western Inner Mongolia(China):Framework,Kinematics,Geochronology and Implications for Tectonic Evolution of the Central Asian Orogenic Belt.Gondwana Research,23(4):1342-1364.https://doi.org/10.13039/501100001809
Xu,Z.,Han,B.F.,Ren,R.,et al.,2012.Ultramafic-Mafic Mélange,Island Arc and Post-Collisional Intrusions in the Mayile Mountain,West Junggar,China:Implications for Paleozoic Intra-Oceanic Subduction-Accretion Process.Lithos,132-133:141-161.https://doi.org/10.1016/j.lithos.2011.11.016
Yang,J.H.,Wu,F.Y.,Shao,J.A.,et al.,2006.Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt,North China.Earth and Planetary Science Letters,246(3-4):336-352.https://doi.org/10.1016/j.epsl.2006.04.029
Yang,W.J.,Wang,L.K.,Zhang,S.L.,et al.,1986.Micas of the Two Series of Granites in South China.Acta Mineralogica Sinica,6(4):298-307(in Chinese with English abstract).
Zeng,J.J.,Zheng,Y.Y.,Qi,J.H.,et al.,2008.Foundation and Geological Significance of Adakitic Granite at Guyang of Inner Mongolia.Earth Science,33(6):755-763(in Chinese with English abstract).
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2009a.Contrasting Late Carboniferous and Late Permian-Middle Triassic Intrusive Suites from the Northern Margin of the North China Craton:Geochronology,Petrogenesis,and Tectonic Implications.Geological Society of America Bulletin,121(1-2):181-200.
Zhang,S.H.,Zhao,Y.,Kr9ner,A.,et al.,2009b.Early Permian Plutons from the Northern North China Block:Constraints on Continental Arc Evolution and Convergent Margin Magmatism Related to the Central Asian Orogenic Belt.International Journal of Earth Sciences,98(6):1441-1467.https://doi.org/10.1007/s00531-008-0368-2
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2007.Carboniferous Granitic Plutons from the Northern Margin of the North China Block:Implications for a Late Palaeozoic Active Continental Margin.Journal of the Geological Society,164(2):451-463.https://doi.org/10.1144/0016-76492005-190
Zhang,X.H.,Wilde,S.A.,Zhang,H.F.,et al.,2011a.Early Permian High-K Calc-Alkaline Volcanic Rocks from NW Inner Mongolia,North China:Geochemistry,Origin and Tectonic Implications.Journal of the Geological Society,168(2):525-543.
Zhang,X.H.,Mao,Q.,Zhang,H.F.,et al.,2011b.Mafic and Felsic Magma Interaction during the Construction of High-KCalc-Alkaline Plutons within a Metacratonic Passive Margin:The Early Permian Guyang Batholith from the Northern North China Craton.Lithos,125(1-2):569-591.
Zhang,W.,Jian,P.,Kr9ner,A.,et al.,2013.Magmatic and Metamorphic Development of an Early to Mid-Paleozoic Continental Margin Arc in the Southernmost Central Asian Orogenic Belt,Inner Mongolia,China.Journal of Asian Earth Sciences,72:63-74.https://doi.org/10.1016/j.jseaes.2012.05.025
Zhang,X.H.,Gao,Y.L.,Wang,Z.J.,et al.,2012.Carboniferous Appinitic Intrusions from the Northern North China Craton:Geochemistry,Petrogenesis and Tectonic Implications.Journal of the Geological Society,169(3):337-351.https://doi.org/10.1144/0016-76492011-062
Zhao,L.M.,Takasu,A.,Liu,Y.J.,et al.,2017.Blueschist from the Toudaoqiao Area,Inner Mongolia,NE China:Evidence for the Suture between the Ergun and the Xing'an Blocks.Journal of Earth Science,28(2):241-248.https://doi.org/10.1007/s12583-017-0721-0
李承东,冉皞,赵利刚,等,2012.温都尔庙群锆石的LA-MC-ICPMS U-Pb年龄及构造意义.岩石学报,28(11):3705-3714.
李怀坤,耿建珍,郝爽,等,2009.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究.矿物学报,29(S1):600-601.
钱筱嫣,张志诚,陈彦,等,2017.内蒙古朱日和地区早古生代岩浆岩年代学、地球化学特征及其构造意义.地球科学,42(9):1472-1494.
吴亚飞,曾键年,曹建劲,等,2013.内蒙古东升庙海西期岩体锆石U-Pb年龄及Hf同位素特征.地质科技情报,32(6):22-30.
谢应雯,张玉泉,1990.横断山区花岗岩类中角闪石的标型特征及其成因意义.矿物学报,10(1):35-45.
杨文金,王联魁,张绍立,等,1986.华南两个不同成因系列花岗岩的云母标型特征.矿物学报,6(4):298-307.
曾俊杰,郑有业,齐建宏,等,2008.内蒙古固阳地区埃达克质花岗岩的发现及其地质意义.地球科学,33(6):755-763.
Allen,M.B.,Engor,A.M.C.,Natal'in,B.A.,1995.Junggar,Turfan and Alakol Basins as Late Permian to?Early Triassic Extensional Structures in a Sinistral Shear Zone in the Altaid Orogenic Collage,Central Asia.Journal of the Geological Society,152(2):327-338.https://doi.org/10.1144/gsjgs.152.2.0327
Batchelor,R.A.,Bowden,P.,1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology,48(1-4):43-55.https://doi.org/10.1016/0009-2541(85)90034-8
Coleman,R.G.,1989.Continental Growth of Northwest China.Tectonics,8(3):621-635.https://doi.org/10.1029/tc008i003p00621
Defant,M.J.,Drummond,M.S.,1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature,347(6294):662-665.https://doi.org/10.1038/347662a0
Feng,J.Y.,Xiao,W.J.,Windley,B.,et al.,2013.Field Geology,Geochronology and Geochemistry of MaficUltramafic Rocks from Alxa,China:Implications for Late Permian Accretionary Tectonics in the Southern Altaids.Journal of Asian Earth Sciences,78:114-142.https://doi.org/10.1016/j.jseaes.2013.01.020
Gao,J.,Li,M.S.,Xiao,X.C.,et al.,1998.Paleozoic Tectonic Evolution of the Tianshan Orogen,Northwestern China.Tectonophysics,287(1-4):213-231.https://doi.org/10.1016/s0040-1951(98)80070-x
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
Han,B.F.,He,G.Q.,Wang,X.C.,et al.,2011.Late Carboniferous Collision between the Tarim and Kazakhstan-Yili Terranes in the Western Segment of the South Tian Shan Orogen,Central Asia,and Implications for the Northern Xinjiang,Western China.Earth-Science Reviews,109(3-4):74-93.https://doi.org/10.1016/j.earscirev.2011.09.001
Jahn,B.M.,Griffin,W.L.,Windley,B.,2000.Continental Growth in the Phanerozoic:Evidence from Central Asia.Tectonophysics,328(1-2):vii-x.https://doi.org/10.1016/s0040-1951(00)00174-8
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2008.Time Scale of an Early to Mid-Paleozoic Orogenic Cycle of the LongLived Central Asian Orogenic Belt,Inner Mongolia of China:Implications for Continental Growth.Lithos,101(3-4):233-259.https://doi.org/10.1016/j.lithos.2007.07.005
Kuno,H.,1968.“Differentiation of Basaltic Magmas”.In:Hess,H.Arie Poldervaart,A.,eds.,Basalts:The Poldervaart Treatise on Rocks of Basaltic Composition(vol.2).Interscience,New York,623-688.
Li,C.D.,Ran,H.,Zhao,L.G.,et al.,2012.LA-MC-ICPMS U-Pb Geochronology of Zircons from the Wenduermiao Group and Its Tectonic Significance.Acta Petrologica Sinica,28(11):3705-3714(in Chinese with English abstract).
Li,H.K.,Geng,J.Z.,Hao,S.,et al.,2009.Study on the Using LA-MC-ICPMS to Date the U-Pb Isotopic Age of Zircons.Bulletin of Mineralogy,29(S1):600-601(in Chinese with English abstract).
Liu,Y.S.,Gao,S.,Hu,Z.C.,et al.,2010.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating,Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths.Journal of Petrology,51(1-2):537-571.https://doi.org/10.1093/petrology/egp082
Ludwig,K.R.,2003.Users Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,Berkeley,1-39.
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
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
Qian X.Y.,Zhang Z.C.,Chen Y.,et al.,2017.Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area,Inner Mongolia and Their Tectonic Significance.Earth Science,42(9):1472-1494(in Chinese with English abstract).
Sengor,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
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,Z.Z.,Han,B.F.,Feng,L.X.,et al.,2015.Geochronology,Geochemistry and Origins of the Paleozoic-Triassic Plutons in the Langshan Area,Western Inner Mongolia,China.Journal of Asian Earth Sciences,97:337-351.
Wilson,M.,1989.Igneous Petrogenesis.Unwin Hyman,London.
Windley,B.F.,Allen,M.B.,Zhang,C.,et al.,1990.Paleozoic Accretion and Cenozoic Redeformation of the Chinese Tien Shan Range,Central Asia.Geology,18(2):128.
Windley,B.F.,Alexeiev,D.,Xiao,W.J.,et al.,2007.Tectonic Models for Accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164(1):31-47.
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,Y.F.,Zeng,J.N.,Cao,J.J.,et al.,2013.Zircon U-Pb Ages and Hf Isotopes of Hercynian Intrusion in Dongshengmiao,Inner Mongolia.Geological Science and Technology Information,32(6):22-30(in Chinese with English abstract).
Xiao,W.J.,Han,C.M.,Yuan,C.,et al.,2008.Middle Cambrian to Permian Subduction-Related Accretionary Orogenesis of Northern Xinjiang,NW China:Implications for the Tectonic Evolution of Central Asia.Journal of Asian Earth Sciences,32(2-4):102-117.https://doi.org/10.1016/j.jseaes.2007.10.008
Xiao,W.J.,Zhang,L.C.,Qin,K.Z.,et al.,2004.Paleozoic Accretionary and Collisional Tectonics of the Eastern Tianshan(China):Implications for the Continental Growth of Central Asia.American Journal of Science,304(4):370-395.https://doi.org/10.2475/ajs.304.4.370
Xie,Y.W.,Zhang,Y.Q.,1990.Peculiarities and Genetic Significance of Hornblende from Granite in the Hengduanshan Region.Acta Mineralogica Sinica,10(1):35-45(in Chinese with English abstract).
Xu,B.,Charvet,J.,Chen,Y.,et al.,2013.Middle Paleozoic Convergent Orogenic Belts in Western Inner Mongolia(China):Framework,Kinematics,Geochronology and Implications for Tectonic Evolution of the Central Asian Orogenic Belt.Gondwana Research,23(4):1342-1364.https://doi.org/10.13039/501100001809
Xu,Z.,Han,B.F.,Ren,R.,et al.,2012.Ultramafic-Mafic Mélange,Island Arc and Post-Collisional Intrusions in the Mayile Mountain,West Junggar,China:Implications for Paleozoic Intra-Oceanic Subduction-Accretion Process.Lithos,132-133:141-161.https://doi.org/10.1016/j.lithos.2011.11.016
Yang,J.H.,Wu,F.Y.,Shao,J.A.,et al.,2006.Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt,North China.Earth and Planetary Science Letters,246(3-4):336-352.https://doi.org/10.1016/j.epsl.2006.04.029
Yang,W.J.,Wang,L.K.,Zhang,S.L.,et al.,1986.Micas of the Two Series of Granites in South China.Acta Mineralogica Sinica,6(4):298-307(in Chinese with English abstract).
Zeng,J.J.,Zheng,Y.Y.,Qi,J.H.,et al.,2008.Foundation and Geological Significance of Adakitic Granite at Guyang of Inner Mongolia.Earth Science,33(6):755-763(in Chinese with English abstract).
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2009a.Contrasting Late Carboniferous and Late Permian-Middle Triassic Intrusive Suites from the Northern Margin of the North China Craton:Geochronology,Petrogenesis,and Tectonic Implications.Geological Society of America Bulletin,121(1-2):181-200.
Zhang,S.H.,Zhao,Y.,Kr9ner,A.,et al.,2009b.Early Permian Plutons from the Northern North China Block:Constraints on Continental Arc Evolution and Convergent Margin Magmatism Related to the Central Asian Orogenic Belt.International Journal of Earth Sciences,98(6):1441-1467.https://doi.org/10.1007/s00531-008-0368-2
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2007.Carboniferous Granitic Plutons from the Northern Margin of the North China Block:Implications for a Late Palaeozoic Active Continental Margin.Journal of the Geological Society,164(2):451-463.https://doi.org/10.1144/0016-76492005-190
Zhang,X.H.,Wilde,S.A.,Zhang,H.F.,et al.,2011a.Early Permian High-K Calc-Alkaline Volcanic Rocks from NW Inner Mongolia,North China:Geochemistry,Origin and Tectonic Implications.Journal of the Geological Society,168(2):525-543.
Zhang,X.H.,Mao,Q.,Zhang,H.F.,et al.,2011b.Mafic and Felsic Magma Interaction during the Construction of High-KCalc-Alkaline Plutons within a Metacratonic Passive Margin:The Early Permian Guyang Batholith from the Northern North China Craton.Lithos,125(1-2):569-591.
Zhang,W.,Jian,P.,Kr9ner,A.,et al.,2013.Magmatic and Metamorphic Development of an Early to Mid-Paleozoic Continental Margin Arc in the Southernmost Central Asian Orogenic Belt,Inner Mongolia,China.Journal of Asian Earth Sciences,72:63-74.https://doi.org/10.1016/j.jseaes.2012.05.025
Zhang,X.H.,Gao,Y.L.,Wang,Z.J.,et al.,2012.Carboniferous Appinitic Intrusions from the Northern North China Craton:Geochemistry,Petrogenesis and Tectonic Implications.Journal of the Geological Society,169(3):337-351.https://doi.org/10.1144/0016-76492011-062
Zhao,L.M.,Takasu,A.,Liu,Y.J.,et al.,2017.Blueschist from the Toudaoqiao Area,Inner Mongolia,NE China:Evidence for the Suture between the Ergun and the Xing'an Blocks.Journal of Earth Science,28(2):241-248.https://doi.org/10.1007/s12583-017-0721-0
李承东,冉皞,赵利刚,等,2012.温都尔庙群锆石的LA-MC-ICPMS U-Pb年龄及构造意义.岩石学报,28(11):3705-3714.
李怀坤,耿建珍,郝爽,等,2009.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究.矿物学报,29(S1):600-601.
钱筱嫣,张志诚,陈彦,等,2017.内蒙古朱日和地区早古生代岩浆岩年代学、地球化学特征及其构造意义.地球科学,42(9):1472-1494.
吴亚飞,曾键年,曹建劲,等,2013.内蒙古东升庙海西期岩体锆石U-Pb年龄及Hf同位素特征.地质科技情报,32(6):22-30.
谢应雯,张玉泉,1990.横断山区花岗岩类中角闪石的标型特征及其成因意义.矿物学报,10(1):35-45.
杨文金,王联魁,张绍立,等,1986.华南两个不同成因系列花岗岩的云母标型特征.矿物学报,6(4):298-307.
曾俊杰,郑有业,齐建宏,等,2008.内蒙古固阳地区埃达克质花岗岩的发现及其地质意义.地球科学,33(6):755-763.