松辽盆地北部营城组火山岩地球化学特征及地质意义
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摘要
松辽盆地北部早白垩世营城组发育一套以流纹岩为主的中酸性火山岩,其具有高硅、铝,富碱和低镁、铁的特征,不同类型火山岩均具有轻稀土富集、重稀土亏损、轻重分异严重的特征。其中:酸性流纹岩表现为富集Pb、U、Th、Ta、Hf和Zr等元素,亏损Sr、Ba、Eu等元素;中性安山岩、粗安岩和基性玄武岩则亏损不明显;中酸性英安岩介于两者之间。地化特征分析表明,营城组岩浆来源于亏损地幔,是地幔底侵导致地壳部分熔融,并受到地幔物质的混染,酸性岩喷出前经历了较强的岩浆分异作用。构造判别图解指示营城组火山岩形成于板内伸展环境,具有与板块俯冲作用有关的、发育于活动陆缘或岛弧的火山岩类似的演化特征。结合中国东部构造环境演化特征,认为松辽盆地北部早白垩世火山活动可能是古太平洋板块北北西方向高速俯冲导致地壳岩石圈减薄、地幔物质上涌的产物。
The widely distributed Early Cretaceous volcanic rocks of Yingcheng Formation in northern Songliao basin are intermediate-felsic rocks,which are mainly rhyolites,characterized by high silicon,aluminum,rich alkali,and low magnesium and iron.The standard curve of rare earth elements reveals the deficiency of heavy rare earth elements,but the enrichment of light rare earth elements,and the rare earth elements are seriously differentiated in different kinds of volcanic rocks.The rhyolites are distinctly enriched in incompatible elements such as Pb,U,Th,Ta,Hf,Zr,and apparently loss of Sr,Ba,Eu,while in neutral andesite,trachyandesite and basic basalt they have no obvious loss,and in the intermediate-acid dacite they are in between.The results show that the magma of Yingcheng Formation originated form depleted mantle.Because the magma was contaminated by crust during evolution under magma plating and crust partial melting,forceful magmatic differentiation occurred before the eruption of acid magma.The volcanoes of Yingcheng Formation may erupt in an extensional background within plate according to the discrimination diagrams,and the volcanic rocks of Yingcheng Formation have the same evolutionary characteristics as those of the volcanic rocks developed in active continental margin or island arc associated with plate subduction.Taking the tectonic environment of Eastern China into consideration,the large-scale volcanic action in the Early Cretaceous may be associated with the lithospheric thinning and mantle upwelling under the subduction of the Pacific plate toward northwest in a high speed.
The widely distributed Early Cretaceous volcanic rocks of Yingcheng Formation in northern Songliao basin are intermediate-felsic rocks,which are mainly rhyolites,characterized by high silicon,aluminum,rich alkali,and low magnesium and iron.The standard curve of rare earth elements reveals the deficiency of heavy rare earth elements,but the enrichment of light rare earth elements,and the rare earth elements are seriously differentiated in different kinds of volcanic rocks.The rhyolites are distinctly enriched in incompatible elements such as Pb,U,Th,Ta,Hf,Zr,and apparently loss of Sr,Ba,Eu,while in neutral andesite,trachyandesite and basic basalt they have no obvious loss,and in the intermediate-acid dacite they are in between.The results show that the magma of Yingcheng Formation originated form depleted mantle.Because the magma was contaminated by crust during evolution under magma plating and crust partial melting,forceful magmatic differentiation occurred before the eruption of acid magma.The volcanoes of Yingcheng Formation may erupt in an extensional background within plate according to the discrimination diagrams,and the volcanic rocks of Yingcheng Formation have the same evolutionary characteristics as those of the volcanic rocks developed in active continental margin or island arc associated with plate subduction.Taking the tectonic environment of Eastern China into consideration,the large-scale volcanic action in the Early Cretaceous may be associated with the lithospheric thinning and mantle upwelling under the subduction of the Pacific plate toward northwest in a high speed.
引文
[1]宋立忠,赵泽辉,焦贵浩,等.松辽盆地早白垩世火山岩地球化学特征及其构造意义[J].岩石学报,2010,26(4):1182-1194.Song Lizhong,Zhao Zehui,Jiao Guihao,et al.Geochemical Characteristics of Early Cretaceous Volcanic Rocks from Songliao Basin,Northeast China,and Its Tectonic Implication[J].Acta Petrologic Sinica,2010,26(4):1182-1194.
[2]闫全人,高山林,王宗起,等.松辽盆地火山岩的同位素年代、地球化学特征及意义[J].地球化学,2002,31(2):169-179.Yan Quanren,Gao Shanlin,Wang Zongqi,et al.Geochronology and Geochemistry of Volcanic Rocks from the Songliao Basin and Their Implication[J].Geochemical,2002,31(2):169-179.
[3]朱勤文,路凤香,谢意红,等.大陆边缘扩张型活动带火山岩组合:松辽盆地周边中生代火山岩研究[J].岩石学报,1997,13(4):551-562.Zhu Qinwen,Lu Fengxiang,Xie Yihong,et al.Volcanic Rocks Assemblages in Active Belt of Spreading Type in Continental Margin:Study on Mesozoic Volcanic Rocks Around Songliao Basin[J].Acta Petrologic Sinica,1997,13(4):551-562.
[4]王清海,许文良.松辽盆地形成与演化的深部作用过程:中生代火山岩探针[J].吉林大学学报(地球科学版),2003,33(1):37-42.Wang Qinghai,Xu Wenliang.The Deep Process of Formation and Evolution of Songliao Basin:Mesozoic Volcanic Rock Probe[J].Journal of Jilin University(Earth Science Edition),2003,33(1):37-42.
[5]葛荣峰,张庆龙,王良书,等.松辽盆地构造演化与中国东部构造体质转换[J].地质论评,2010,56(2):180-195.Ge Rongfeng,Zhang Qinglong,Wang Liangshu,et al.Tectonic Evolution of Songliao Basin and the Prominent Tectonic Regime Transition in Eastern China[J].Geological Review,2010,56(2):180-195.
[6]张元高,陈树民,张尔华,等.徐家围子断陷构造地质特征研究新进展[J].岩石学报,2010,26(1):142-148.Zhang Yuangao,Chen Shumin,Zhang Erhua,et al.The New Progress of Xujiaweizi Fault Depression Characteristics of Structural Geology Research[J].Acta Petrologic Sinica,2010,26(1):142-148.
[7]赵书跃,韩彦东,朱春燕,等.大兴安岭火山喷发带北段中性、中酸性火山岩地球化学特征及其地质意义[J].地质力学学报,2001,10(3):276-287.Zhao Shuyue,Han Yandong,Zhu Chunyan,et al.Geochemical Characteristics and Geological Significance of Intermedicate and Intermediate-Acid Volcanic Rocks in the Northern Sector of the Da Hinggan Volcanic Eruption Zone[J].Journal of Geomechanics,2001,10(3):276-287.
[8]章凤奇,程晓敢,陈汉林,等.松辽盆地东南缘晚中生代火山事件的锆石年代学与地球化学制约[J].岩石学报,2009,25(1):39-54.Zhang Fengqi,Cheng Xiaogan,Chen Hanlin,et al.Zircon Chronological and Geochemical Constraints on the Late Mesozoic Volcanic Events in the Southeastern Margin of the Songliao Basin,NE China[J].Acta Petrologic Sinica,2009,25(1):39-54.
[9]Feeley T C,Dungan M A.Compositional and Dynamic Controls on Mafic-Silicic Magma Interactions at Continental Arc Volcanoes:Evidence from Cordon El Guadal,Tatara-San Pedro Comples,Chile[J].Journal of Petrology,1996,37(6):1547-1577.
[10]章凤奇,庞彦明,杨树锋,等.松辽盆地北部断陷区营城组火山岩锆石SHRIMP年代学、地球化学及其意义[J].地质学报,2007,81(9):1248-1258.Zhang Fengqi,Pang Yanming,Yang Shufeng,et al.Geochronlogy of Zircon SHRIMP,Geochemistry and Its Implication of the Volcanic Rocks from Yingcheng Formation in Depressionarea,North of Songliao Basin[J].Acta Geologica Sinica,2007,81(9):1248-1258.
[11]孟凡超,刘嘉麟,李明,等.松辽盆地徐家围子营城组流纹岩地球化学特征及构造指示意义[J].岩石学报,2010,26(1):227-241.Meng Fanchao,Liu Jiaqi,Li Ming,et al.Geochemistry and Tectonic Implication of Rhyolites Feom Yingcheng Formation in Xujiaweizi,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):227-241.
[12]Wang P J,Chen F K,Chen S M,et al.Geochemical and Nd-Sr-Pb Isotopic Composition of Mesozoic Volcanic Rocks in the Songliao Basin,NE China[J].Geochemical Journal,2006,40(2):149-159.
[13]Rollison M P,Clemens J D.Origin of HighPostassium,Talcalkaline,Ⅰ-Type Granitoids[J].Geology,1993,21(9):825-828.
[14]Boynton W V.Geochemistry of the Rare Earth Elements:Meteorite Studies[C]//Henderson P.Rare Earth Element Geochemistry.New York:Elsevier Science Publications B V,1984:63-114.
[15]Sun S S,MacDonough W F.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publishions,1989,42(1):313-345.
[16]Miller J A,Harris C.Petrogenesis of Swaziland and Northern Nata Rhyolites of the Lebombo Rifted Volcanic Margin,South East Africa[J].Journal of Petrology,2007,48(1):185-218.
[17]高晓峰,郭峰,范蔚茗,等.南兴安岭晚中生代中酸性火山岩的岩石成因[J].岩石学报,2005,21(3):737-748.Gao Xiaofeng,Guo Feng,Fan Weiming,et al.Orgin of Late Mesozoic Intermediate-Felsic Volcanic Rocks from the Northern Da Hinggan Mountain,NEChina[J].Acta Petrologica Sinica,2005,21(3):737-748.
[18]Grove T L,Donnelly J M.The Evolution of Young Silicic Lavas at Medicine Lake Volcano,California:Implications for the Origin of Compositional Gaps in Calc-Alkaline Series Lavas[J].Contributions to Mineralogy and Petrology,1986,92:281-302.
[19]Hochstaedter A G,Gill J B,Morris J.Volcanism in the Sumisu Rift:Ⅱ:Subduction and Non-Subduction Related Componenets[J].Earth Planetary Science Letters,1990,100:195-209.
[20]Bullen T D,Clynne M A.Trace Element and Isotopic Constraints on Magmatic Evolution at Lassen Volcanic Center[J].Journal of Geophysical Research,1990,95:19671-19691.
[21]李伍平,李献华.燕山造山带中段晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3):501-510.Li Wuping,Li Xianhua.Petrogenesis and Its Implication for the Middle-Late Jurassic Intermediate-Acidic Volcanic Rocks in the Middle Section of Yanshan Orogen[J].Acta Petrologica Sinica,2004,20(3):501-510.
[22]Wilson M.Magmatism and Geodynamics of Basin Formation[J].Sedimentary Geology,1993,86(1/2):5-29.
[23]孟凡超,路玉林,刘嘉麒,等.松辽盆地营城组两类酸性火山岩地球化学特征与成因[J].岩石学报,2013,29(8):2731-2745.Meng Fanchao,Lu Yulin,Liu Jiaqi,et al.Geochemical Characteristics and Petrogenesis of Two Types of Acid Volcanic Rocks from Yingcheng Formation in Songliao Basin[J].Acta Petrologica Sinica,2013,29(8):2731-2745.
[24]王腾飞,程日辉,沈艳杰.松辽盆地东南缘营城组流纹岩类型及其在火山岩地层分析中的意义[J].吉林大学学报(地球科学版),2014,44(1):45-55.Wang Tengfei,Cheng Rihui,Shen Yanjie.Classification of Rhyolite from Yingcheng Formation and Its Significance for Volcanic Stratigraphy Analysis in Southeastern Uplift of Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2014,44(1):45-55.
[25]邵济安,张履桥,牟保磊.大兴安岭中生代伸展造山过程中的岩浆作用[J].地学前缘,1999,6(4):339-345.Shao Ji’an,Zhang Lüqiao,Mou Baolei.Magmatism in the Mesozoic Extending Orogenic Process of Da Hinggan Mts[J].Earth Science Frontiers,1999,6(4):339-345.
[26]温升福,刘曼丽,刘玮,等.松辽盆地长岭断陷中基性火山岩的时代与其成因[J].吉林大学学报(地球科学版),2013,43(6):1762-1771.Wen Shengfu,Liu Manli,Liu Wei,et al.Geochronolgy and Petrogenesis of IntermediateBasic Volcanic Rocks from Changling Depression in the Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2013,43(6):1762-1771.
[27]孟凡超,刘嘉麒,崔岩,等.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约[J].岩石学报,2014,30(12):3569-3586.Meng Fanchao,Liu Jiaqi,Cui Yan,et al.Mesozoic Tectonic Regimes Transition in the Northeast China:Constriants from Temporal-Spatial and Association of Volcanic Rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[28]Rittmann A.The Probable Origin of High-Alumina Basalts[J].Bulletin Volcanologique,1970,34(2):414-420.
[29]Pearce J A,Harris N B W,Tindle A G.Trace Element Distribution Diagram for the Tectonic Interpretation of Granitic Rocks[J].Journal of Petrology,1984,25:956-983.
[30]曾维顺,周建波,董策,等.蒙古-鄂霍茨克洋俯冲的记录:额尔古纳地区八大关变质杂岩的证据[J].岩石学报,2014,30(7):1948-1960.Zeng Weishun,Zhou Jianbo,Dong Ce,et al.SubductionRecord of Mongol-Okhotsk Ocean:Constrains from Badaguan Metamorphic Complexes in the Erguna Massif,NE China[J].Acta Petrologic Sinica,2014,30(7):1948-1960.
[31]林强,葛文春,孙德有,等.中国东北地区中生代火山岩的大地构造意义[J].地质科学,1998,33(2):129-139.Lin Qiang,Ge Wenchun,Sun Deyou,et al.Tectonic Significance of Mesozoic Volcanic Rocks in Northeastern China[J].Scientia Geologica Scinica,1998,33(2):129-139.
[32]Xu W L,Ji W Q,Pei F P,et al.Triassic Volcanism in Eastern Heilongjiang and Jilin Proviences,NEChina:Chronology,Geochemistry,and Tectonic Implications[J].Journal of Asian Earth Sciences,2009,34(3):392-402.
[33]许文良,王枫,裴福萍,等.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[J].岩石学报,2013,29(2):339-353.Xu Wenliang,Wang Feng,Pei Fuping,et al.Mesozoic Tectonic Regimes and Regional OreForming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J].Acta Petrologic Sinica,2013,29(2):339-353.
[34]Maruyama S,Isozaki Y,Kimura G,et al.Paleogeographic Maps of the Japanese Islands:Plate Tectonic Synthesis from 750 Ma to the Present[J].Island Arc,1997,6(1):121-142.
[2]闫全人,高山林,王宗起,等.松辽盆地火山岩的同位素年代、地球化学特征及意义[J].地球化学,2002,31(2):169-179.Yan Quanren,Gao Shanlin,Wang Zongqi,et al.Geochronology and Geochemistry of Volcanic Rocks from the Songliao Basin and Their Implication[J].Geochemical,2002,31(2):169-179.
[3]朱勤文,路凤香,谢意红,等.大陆边缘扩张型活动带火山岩组合:松辽盆地周边中生代火山岩研究[J].岩石学报,1997,13(4):551-562.Zhu Qinwen,Lu Fengxiang,Xie Yihong,et al.Volcanic Rocks Assemblages in Active Belt of Spreading Type in Continental Margin:Study on Mesozoic Volcanic Rocks Around Songliao Basin[J].Acta Petrologic Sinica,1997,13(4):551-562.
[4]王清海,许文良.松辽盆地形成与演化的深部作用过程:中生代火山岩探针[J].吉林大学学报(地球科学版),2003,33(1):37-42.Wang Qinghai,Xu Wenliang.The Deep Process of Formation and Evolution of Songliao Basin:Mesozoic Volcanic Rock Probe[J].Journal of Jilin University(Earth Science Edition),2003,33(1):37-42.
[5]葛荣峰,张庆龙,王良书,等.松辽盆地构造演化与中国东部构造体质转换[J].地质论评,2010,56(2):180-195.Ge Rongfeng,Zhang Qinglong,Wang Liangshu,et al.Tectonic Evolution of Songliao Basin and the Prominent Tectonic Regime Transition in Eastern China[J].Geological Review,2010,56(2):180-195.
[6]张元高,陈树民,张尔华,等.徐家围子断陷构造地质特征研究新进展[J].岩石学报,2010,26(1):142-148.Zhang Yuangao,Chen Shumin,Zhang Erhua,et al.The New Progress of Xujiaweizi Fault Depression Characteristics of Structural Geology Research[J].Acta Petrologic Sinica,2010,26(1):142-148.
[7]赵书跃,韩彦东,朱春燕,等.大兴安岭火山喷发带北段中性、中酸性火山岩地球化学特征及其地质意义[J].地质力学学报,2001,10(3):276-287.Zhao Shuyue,Han Yandong,Zhu Chunyan,et al.Geochemical Characteristics and Geological Significance of Intermedicate and Intermediate-Acid Volcanic Rocks in the Northern Sector of the Da Hinggan Volcanic Eruption Zone[J].Journal of Geomechanics,2001,10(3):276-287.
[8]章凤奇,程晓敢,陈汉林,等.松辽盆地东南缘晚中生代火山事件的锆石年代学与地球化学制约[J].岩石学报,2009,25(1):39-54.Zhang Fengqi,Cheng Xiaogan,Chen Hanlin,et al.Zircon Chronological and Geochemical Constraints on the Late Mesozoic Volcanic Events in the Southeastern Margin of the Songliao Basin,NE China[J].Acta Petrologic Sinica,2009,25(1):39-54.
[9]Feeley T C,Dungan M A.Compositional and Dynamic Controls on Mafic-Silicic Magma Interactions at Continental Arc Volcanoes:Evidence from Cordon El Guadal,Tatara-San Pedro Comples,Chile[J].Journal of Petrology,1996,37(6):1547-1577.
[10]章凤奇,庞彦明,杨树锋,等.松辽盆地北部断陷区营城组火山岩锆石SHRIMP年代学、地球化学及其意义[J].地质学报,2007,81(9):1248-1258.Zhang Fengqi,Pang Yanming,Yang Shufeng,et al.Geochronlogy of Zircon SHRIMP,Geochemistry and Its Implication of the Volcanic Rocks from Yingcheng Formation in Depressionarea,North of Songliao Basin[J].Acta Geologica Sinica,2007,81(9):1248-1258.
[11]孟凡超,刘嘉麟,李明,等.松辽盆地徐家围子营城组流纹岩地球化学特征及构造指示意义[J].岩石学报,2010,26(1):227-241.Meng Fanchao,Liu Jiaqi,Li Ming,et al.Geochemistry and Tectonic Implication of Rhyolites Feom Yingcheng Formation in Xujiaweizi,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):227-241.
[12]Wang P J,Chen F K,Chen S M,et al.Geochemical and Nd-Sr-Pb Isotopic Composition of Mesozoic Volcanic Rocks in the Songliao Basin,NE China[J].Geochemical Journal,2006,40(2):149-159.
[13]Rollison M P,Clemens J D.Origin of HighPostassium,Talcalkaline,Ⅰ-Type Granitoids[J].Geology,1993,21(9):825-828.
[14]Boynton W V.Geochemistry of the Rare Earth Elements:Meteorite Studies[C]//Henderson P.Rare Earth Element Geochemistry.New York:Elsevier Science Publications B V,1984:63-114.
[15]Sun S S,MacDonough W F.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publishions,1989,42(1):313-345.
[16]Miller J A,Harris C.Petrogenesis of Swaziland and Northern Nata Rhyolites of the Lebombo Rifted Volcanic Margin,South East Africa[J].Journal of Petrology,2007,48(1):185-218.
[17]高晓峰,郭峰,范蔚茗,等.南兴安岭晚中生代中酸性火山岩的岩石成因[J].岩石学报,2005,21(3):737-748.Gao Xiaofeng,Guo Feng,Fan Weiming,et al.Orgin of Late Mesozoic Intermediate-Felsic Volcanic Rocks from the Northern Da Hinggan Mountain,NEChina[J].Acta Petrologica Sinica,2005,21(3):737-748.
[18]Grove T L,Donnelly J M.The Evolution of Young Silicic Lavas at Medicine Lake Volcano,California:Implications for the Origin of Compositional Gaps in Calc-Alkaline Series Lavas[J].Contributions to Mineralogy and Petrology,1986,92:281-302.
[19]Hochstaedter A G,Gill J B,Morris J.Volcanism in the Sumisu Rift:Ⅱ:Subduction and Non-Subduction Related Componenets[J].Earth Planetary Science Letters,1990,100:195-209.
[20]Bullen T D,Clynne M A.Trace Element and Isotopic Constraints on Magmatic Evolution at Lassen Volcanic Center[J].Journal of Geophysical Research,1990,95:19671-19691.
[21]李伍平,李献华.燕山造山带中段晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3):501-510.Li Wuping,Li Xianhua.Petrogenesis and Its Implication for the Middle-Late Jurassic Intermediate-Acidic Volcanic Rocks in the Middle Section of Yanshan Orogen[J].Acta Petrologica Sinica,2004,20(3):501-510.
[22]Wilson M.Magmatism and Geodynamics of Basin Formation[J].Sedimentary Geology,1993,86(1/2):5-29.
[23]孟凡超,路玉林,刘嘉麒,等.松辽盆地营城组两类酸性火山岩地球化学特征与成因[J].岩石学报,2013,29(8):2731-2745.Meng Fanchao,Lu Yulin,Liu Jiaqi,et al.Geochemical Characteristics and Petrogenesis of Two Types of Acid Volcanic Rocks from Yingcheng Formation in Songliao Basin[J].Acta Petrologica Sinica,2013,29(8):2731-2745.
[24]王腾飞,程日辉,沈艳杰.松辽盆地东南缘营城组流纹岩类型及其在火山岩地层分析中的意义[J].吉林大学学报(地球科学版),2014,44(1):45-55.Wang Tengfei,Cheng Rihui,Shen Yanjie.Classification of Rhyolite from Yingcheng Formation and Its Significance for Volcanic Stratigraphy Analysis in Southeastern Uplift of Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2014,44(1):45-55.
[25]邵济安,张履桥,牟保磊.大兴安岭中生代伸展造山过程中的岩浆作用[J].地学前缘,1999,6(4):339-345.Shao Ji’an,Zhang Lüqiao,Mou Baolei.Magmatism in the Mesozoic Extending Orogenic Process of Da Hinggan Mts[J].Earth Science Frontiers,1999,6(4):339-345.
[26]温升福,刘曼丽,刘玮,等.松辽盆地长岭断陷中基性火山岩的时代与其成因[J].吉林大学学报(地球科学版),2013,43(6):1762-1771.Wen Shengfu,Liu Manli,Liu Wei,et al.Geochronolgy and Petrogenesis of IntermediateBasic Volcanic Rocks from Changling Depression in the Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2013,43(6):1762-1771.
[27]孟凡超,刘嘉麒,崔岩,等.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约[J].岩石学报,2014,30(12):3569-3586.Meng Fanchao,Liu Jiaqi,Cui Yan,et al.Mesozoic Tectonic Regimes Transition in the Northeast China:Constriants from Temporal-Spatial and Association of Volcanic Rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[28]Rittmann A.The Probable Origin of High-Alumina Basalts[J].Bulletin Volcanologique,1970,34(2):414-420.
[29]Pearce J A,Harris N B W,Tindle A G.Trace Element Distribution Diagram for the Tectonic Interpretation of Granitic Rocks[J].Journal of Petrology,1984,25:956-983.
[30]曾维顺,周建波,董策,等.蒙古-鄂霍茨克洋俯冲的记录:额尔古纳地区八大关变质杂岩的证据[J].岩石学报,2014,30(7):1948-1960.Zeng Weishun,Zhou Jianbo,Dong Ce,et al.SubductionRecord of Mongol-Okhotsk Ocean:Constrains from Badaguan Metamorphic Complexes in the Erguna Massif,NE China[J].Acta Petrologic Sinica,2014,30(7):1948-1960.
[31]林强,葛文春,孙德有,等.中国东北地区中生代火山岩的大地构造意义[J].地质科学,1998,33(2):129-139.Lin Qiang,Ge Wenchun,Sun Deyou,et al.Tectonic Significance of Mesozoic Volcanic Rocks in Northeastern China[J].Scientia Geologica Scinica,1998,33(2):129-139.
[32]Xu W L,Ji W Q,Pei F P,et al.Triassic Volcanism in Eastern Heilongjiang and Jilin Proviences,NEChina:Chronology,Geochemistry,and Tectonic Implications[J].Journal of Asian Earth Sciences,2009,34(3):392-402.
[33]许文良,王枫,裴福萍,等.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[J].岩石学报,2013,29(2):339-353.Xu Wenliang,Wang Feng,Pei Fuping,et al.Mesozoic Tectonic Regimes and Regional OreForming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J].Acta Petrologic Sinica,2013,29(2):339-353.
[34]Maruyama S,Isozaki Y,Kimura G,et al.Paleogeographic Maps of the Japanese Islands:Plate Tectonic Synthesis from 750 Ma to the Present[J].Island Arc,1997,6(1):121-142.