大兴安岭克一河地区满克头鄂博组火山岩形成时代、地球化学特征及地质意义
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摘要
大兴安岭北段克一河地区满克头鄂博组岩石主体岩性为流纹质、英安质火山岩,火山岩TAS图解中显示其为流纹岩。LA-ICP-MS锆石U-Pb定年结果显示,其形成于(139±2)Ma。火山岩多为高钾钙碱性系列,具有高SiO_2和全碱含量。稀土元素总量较低(ΣREE=137.34×10~(-6)~191.18×10~(-6)),轻重稀土元素分馏明显((La/Yb)_N=12.57~22.25),具中等负Eu异常(δEu=0.40~0.72)。富集大离子亲石元素Rb、Th、U和轻稀土元素,亏损高场强元素Nb、Ta、P、Ti。岩石Sr平均值为115×10~(-6),Yb的平均值为1.70×10~(-6),Y/Yb平均值为9.46,(Ho/Yb)_N平均值为1.04,且具负的Eu异常,暗示岩浆可能来源于加厚麻粒岩下地壳部分熔融,结合区域特征,推测该火山岩可能形成于蒙古—鄂霍茨克洋闭合碰撞造山所导致的地壳加厚环境。
Petrographically,the volcanic rocks in Manketouebo Formation from keyihe area northern Da Hinggan Mountains are mainly composed of rhyolitic and dacitic volcanic rocks. The TAS diagram displays that they are rhyolite. LA-ICP-MS zircon U-Pb dating results show that they formed at 139 ± 2Ma. The volcanic rocks,which are rich in SiO_2 and alkalis,belong to high K Calc alkaline series. They are low in total rare earth elements(ΣREE = 137. 34 × 10~(-6)~ 191. 18 × 10~(-6)),whilst highly fractionated LREE from HREE((La/Yb)_N= 12. 57 ~22. 25),with moderately negative Eu anomalies(δEu = 0. 40 ~ 0. 72). They are characterized by the enrichment of large ion lithophile elements( such as Rb,Th and U) and LREE,and deplection of high field strength elements( such as Nb,Ta,P,and Ti). The average value of Sr is 115 × 10~(-6),Yb is 1. 70 × 10~(-6),Y/Yb is 9. 46,(Ho/Yb)_N is 1. 04,with negative Eu indicating that the magmas of these volcanic rocks are derived from partial melting of the granulite fracies of thickened lower crust. Integrating regional geology,it is suggested that the formation of the volcanic rocks were related to the crustal thickening during the closure of Mongol-Okhotsk Ocean.
Petrographically,the volcanic rocks in Manketouebo Formation from keyihe area northern Da Hinggan Mountains are mainly composed of rhyolitic and dacitic volcanic rocks. The TAS diagram displays that they are rhyolite. LA-ICP-MS zircon U-Pb dating results show that they formed at 139 ± 2Ma. The volcanic rocks,which are rich in SiO_2 and alkalis,belong to high K Calc alkaline series. They are low in total rare earth elements(ΣREE = 137. 34 × 10~(-6)~ 191. 18 × 10~(-6)),whilst highly fractionated LREE from HREE((La/Yb)_N= 12. 57 ~22. 25),with moderately negative Eu anomalies(δEu = 0. 40 ~ 0. 72). They are characterized by the enrichment of large ion lithophile elements( such as Rb,Th and U) and LREE,and deplection of high field strength elements( such as Nb,Ta,P,and Ti). The average value of Sr is 115 × 10~(-6),Yb is 1. 70 × 10~(-6),Y/Yb is 9. 46,(Ho/Yb)_N is 1. 04,with negative Eu indicating that the magmas of these volcanic rocks are derived from partial melting of the granulite fracies of thickened lower crust. Integrating regional geology,it is suggested that the formation of the volcanic rocks were related to the crustal thickening during the closure of Mongol-Okhotsk Ocean.
引文
[1]周其林,王献忠,吉峰,等.大兴安岭中生代火山岩地层对比[J].地质评论,2013,59(6):1077-1084.ZHOU Qi-lin,WANG Xian-zhong,JI Feng,et al.Stratigraphic correlation of the Mesozoic volcanic rocks in Da Hinggan Mountain[J].Geological Review,2013,59(6):1077-1084.
[2]Zhang J H,Gao S,Ge W C,et al.Geochronology of the Mesozoic volcanic rocks in the Great Xing'an Range,northeastern China:implications for subductiion-induced delamination[J].Chemical Geology,2010,276:144-165.
[3]Zhang J H,Ge W C,Wu F Y,et al.Mesozoic bimodal volcanic suite in Zhalantun of the Da Hinggan Range and its geological significance:zircon U--Pb age and Hf isotopic constraints[J].Acta Geologic Sinica,2006,80:801-812.
[4]尹志刚,赵海滨,赵寒冬,等.大兴安岭北端塔木兰沟组玄武质岩石的地球化学特征及构造背景[J].地质通报,2005,24(9):848-853.YIN ZHi-gang,ZHAO Hai-bing,ZHAO Han-dong,et al.Geochemical characteristics and geotectonic background of basaltic rocks in Tamulangou Formation from the northern Da Hinggan Moutain[J].Geological Bulletin of China,2005,24(9):848-853.
[5]张玉涛,张连昌,周新华,等.大兴安岭北段牙克石地区玄武质火山岩的元素、同位素地球化学特征及其地质意义[J].地质通报,2008,27(1):112-120.ZHANG Yu-tao,ZHANG Lian-chang,ZHOU Xin-hua,et al.Geochemical of basaltic rocks from Yakeshi,northern Da Hinggan Moutain and its tectonic implications[J].Geological Bulletin of China,2008,27(1):112-120.
[6]周新华,英基丰,张连昌,等.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U--Pb年龄及多元同位素制约[J].地球科学(中国地质大学学报),2009,34(1):1-10.ZHOU Xin-hua,YING Ji-feng,ZHANG Lian-chang,et al.The petrogenesis of Late Mesozoic volcanic rock and the contributions from ancient micro-continents:constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hf isotopic systematics[J].Earth Science(Journal of China University of Geosciences),2009,34(1):1-10.
[7]孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U--Pb年代学、地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226.MENG En,XU Wen-liang,YANG De-bin,et al.Zircon U-Pb chronology,geochemistry of Mesozoic volcanic rocks from the Lingquan basin in Manzhouli area,and its tectonic implications[J].Acta Petrologica Sinica,2011,27(4):1209-1226.
[8]苟军,孙德有,赵忠华,等.满洲里南部白音高老组流纹岩锆石U--Pb定年及岩石成因[J].岩石学报,2010,26(1):333-344.GOU Jun,SUN De-you,ZHAO Zhong-hua,et al.Zircon LA-ICPMS U-Pb dating and petrogenesis of rhyolites in Baiyingaolao Formation from the southern Manzhouli,Inner Mongolia[J].Acta Petrologica Sinica,2010,26(1):333-344.
[9]孙德有,苟军,任云生,等.满洲里南部玛尼吐组火山岩锆石U--Pb年龄与地球化学研究[J].岩石学报,2011,27(10):3084-3094.SUN De-you,GOU Jun,REN Yun-sheng,et al.Zircon U--Pb dating and study on geochemistry of volcanic rocks in Manitu Formation from southern Manchuria,Inner Mongolia[J].Acta Petrologica Sinica,2011,27(10):3084-3094.
[10]林强,葛文春,曹林,等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学,2003,32(3):208-222.LIN Qiang,GE Wen-chun,CAO Lin,et al.Geochemistry of Mesozoic volcanic rocks in Da Hinggan Ling:the bimodal volcanic rocks[J].Geochimica,2003,32(3):208-222.
[11]葛文春,林强,孙德有,等.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据[J].岩石学报,1999,32(3):396-406.GE Wen-chun,LIN Qiang,SUN De-you,et al.Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling:evidence of the mantel-crust interaction[J].Acta Petrologica Sinica,1999,32(3):396-406.
[12]邵济安,臧绍先,牟保磊,等.造山带的伸展构造与软流圈隆起:以兴蒙造山带为例[J].科学通报,1994,39(6):533-537.SHAO Ji-an,ZANG Shao-xian,MOU Bao-lei,et al.Extensional structures within the orogenic belt and asthenosphere uplift-taking Xing--Meng orogenic belt as an example[J].Chinese Science Bulletin,1994,39(6):533-537.
[13]Fan W M,Guo F,Wang Y J,et al.Late Mesozoic calcalkaline volcanic of post-orogenic extension in the northern Da Hinggan Moutains,northeatern China[J].Journal of Volcanology and Geothermal Research,2003,121:115-135.
[14]Meng Q R.What drove Late Mesozoic extension of the northern China-Mongolia tract[J].Tectonophysics,2003,369:155-174.
[15]张玉涛,张连昌,英基丰,等.大兴安岭北段塔河地区早白垩世火山岩地球化学及源区特征[J].岩石学报,2007,23(11):2811-2822.ZHANG Yu-tao,ZHANG Lian-chang,YING Ji-feng,et al.Geochemistry and source characteristics of early Cretaceous volcanic rocks in Tahe,north Da Hinggan Mountain[J].Acta Petrologica Sinica,2007,23(11):2811-2822.
[16]蒋国源,权恒.大兴安岭根河、海拉尔盆地中生代火山岩[J].中国地质科学院沈阳地质矿产研究所所刊,1988,17:23-100.JIANG Guo-yuan,QUAN Heng.Mesozoic volcanic rocks in the Genhe and Hailaer Basin Da Hinggan Mountain[J].Journal of Shenyang Institute of Geology and mineral resources,Chinese Academy of Geological Sciences,1988,17:23-100.
[17]内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1993:244-249.Geology and Mineral Bureau of Inner Mongolia.Regional geology of Inner Mongolia[M].Beijing:Geological Publishing House,1993:244-249.
[18]内蒙古自治区地质矿产局.内蒙古自治区岩石地层[M].武汉:中国地质大学出版社,1996:256-264.Geology and Mineral Bureau of Inner Mongolia.Lithostratigraphy of Inner Mongolia[M].Wuhan:China University of Geosciences Press,1996:256-264.
[19]Andersen T.Correction of common lead in U--Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1):59-79.
[20]李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA--ICP--MS)测定锆石U--Pb同位素年龄的研究[J].矿物学报,2009(增刊1):600-601.LI Huai-kun,GENG Jian-feng,HAO Shuang,et al.Study on the determination of zircon U-Pb isotopic age by laser ablation multi receiver plasma mass spectrometer(LA--ICP--MS)[J].Acta Mineralogica Sinica,2009(Suppl.1):600-601.
[21]William I S,Buick A,Cartwright.An extended episode of early Mesoproterozoic metamophic fluid flow in the Reynold Region,central Australia[J].Journal of Metamorphic Geology,1996,14:29-47.
[22]Belousova E A,Griffin W L,O'Reilly,et al.Igneous zircon:trace element composition as an indicator of source rock type[J].Contributions to Mineraloy and Petrology,2002,143:602-622.
[23]Le Maitre R W,Bakteman P,Dudek A,et al.A classification of igneous rocks and glossary of terms:recommendations of the international union of geological sciences subcommission on the systematics of igneous rocks[M].Oxford:Blackwell Scientific Publications,1989:1-193.
[24]Boynton W V.Cosmochemistry of the rare earth elements:meteorite studies[M].New York:Elsevier Science Publishing Company Inc.1984:63-114.
[25]Sun S S,Mc Donough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and Process[J].Geological Society Special publications,1989,42:313-345.
[26]张超,杨伟红,和钟铧,等.大兴安岭中南段塔尔气地区满克头鄂博组流纹岩年代学和地球化学研究[J].世界地质,2014,33(2):255-265.ZHANG Chao,YANG Wei-hong,HE Zhong-hua,et al.Chronology and geochemistry of rhyolites in Manketou'ebo Formation from Ta'erqi area,southerncentral Greater Xing'an Range[J].Global Geology,2014,33(2):255-265.
[27]李鹏川,李世超,刘正宏,等.内蒙古林西地区满克头鄂博组火山岩形成时代及构造环境[J].世界地质,2016,35(1):77-88.LI Peng-chuan,LI Shi-chao,LIU Zheng-hong,et al.Formation age and environment of the volcanic rocks from the Manketouebo Formation in Linxi area,Inner Mongolia[J].Global Geology,2016,35(1):77-88.
[28]杨扬,高福红,陈井胜,等.赤峰地区中生代火山岩锆石U--Pb年代学证据[J].吉林大学学报:地球科学版,2012,42(增刊2):257-268.YANG Yang,GAO Fu-hong,CHEN Jing-sheng,et al.Zircon U--Pb ages of Mesozoic volcanic rocks in Chifeng area[J].Journal of Jilin University:Earth Science Edition,2012,42(Suppl.2):257-268.
[29]赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319-328.ZHAO Yue,XU Gang,ZHANG shuan-hong,et al.Yanshanian movement and conversion of tectonic regimes in East Asia[J].Earth Science Fronties,2004,11(3):319-328.
[30]李宇,丁磊磊,许文良,等.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[J].岩石学报,2015,31(1):1-11.LI Yu,DING Lei-lei,XU Wen-liang,et al.Geochronology and geochemistry of muscovite granite in Sunwu area,NE China:implications for the timing of closure of the Mongol-Okhotsk Ocean[J].Acta Petrologica Sinica,2015,31(1):1-11.
[31]Hirose K.Melting experiments on lherzolite KLB1 under hydrous conditions and generation of high-magnesian andesitic melts[J].Geology,1997,25(1):42-44.
[32]葛文春,林强,孙德有,等.大兴安岭中生代两类流纹岩成因的地球化学研究[J].地球科学(中国地质大学学报),2000,25(2):172-178.GE Wen-chun,LIN Qiang,SUN De-you,et al.Geochemical research into origins of two types of Mesozoic rhyolites in Daxing'anling[J].Earth Science(Journal of China University of Geosciences),2000,25(2):172-178.
[33]张旗,王焰,李承东,等.花岗岩的Sr--Yb分类及其地质意义[J].岩石学报,2006,22(9):2249-2269.ZHANG Qi,WANG Yan,LI Cheng-dong,et al.Granite classification on the basis of Sr and Yb contents and its implications[J].Acta Petrologic Sinica,2006,22(9):2249-2269.
[34]张旗.大陆花岗岩的地球动力学意义[J].岩石矿物学杂志,2014,33(4):785-798.ZHANG Qi.Geodynamic implications of continental granites[J].Acta Petrologica et Mineralogica,2014,33(4):785-798.
[35]张旗,冉皞,李承东.A型花岗岩的实质是什么?[J].岩石矿物学杂志,2012,31(4):621-626.ZHANG Qi,RAN Hao,LI Cheng-dong.A-type granite:What is the essence?[J].Acta Petrologica et Mineralogica,2012,31(4):621-626.
[36]李世超,徐仲元,刘正宏,等.大兴安岭中段玛尼吐组火山岩LA--ICP--MS锆石U--Pb年龄及地球化学特征[J].地质通报,2013,23(2/3):399-407.LI Shi-chao,XU Zhong-yuan,LIU Zheng-hong,et al.Zircon U-Pb dating and geochemical study of volcanic rocks in Manitu Formation of central Da Hinggan Mountains[J].Geological Bulletin of China,2013,32(2/3):399-407.
[37]Ying J F,Zhou X H,Zhang L C,et al.Geochronological framework of Mesozoic volcanic rocks in the Great Xing'an Range,NE China,and their geodynamic implications[J].Journal of Asian Earth Sciences,2010,39(6):786-793.
[38]纪政,葛文春,杨浩,等.大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J].世界地质,2016,35(2):283-296.JI Zheng,GE Wen-chun,YANG Hao,et al.Petrogenesis of Early Cretaceous granites in Taerqi area of central Great Xing'an Range and its tectonic setting[J].Global Geology,2016,35(2):283-296.
[39]张旗,金惟俊,李承东,等.再论花岗岩按照SrYb分类:标志[J].岩石学报,2010,26(4):985-1015.ZHANG Qi,JIN Wei-jun,LI Cheng-dong,et al.Revisiting the new classification of granitic rocks based on whole-rock Sr and Yb contents:Index[J].Acta Petrologic Sinica,2010,26(4):985-1015.
[40]Barbarin B.A review of the relationships between granitoid types,their origins and their geodynamic enviroments[J].Lithos,1999,46(3):605-626.
[41]Pearce J A,Bender J F,De Long S E,et al.Genesis of collision volcanism in Eastern Anatolia,Turkey[J].Journal of Volcanology and Geothermal Research,1990,44(1/2):189-229.
[42]孟凡超,刘嘉麒,崔岩,等.中国东北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 Fan-chao,LIU Jia-qi,CUI Yan,et al.Mesozoic tectonic regimes transition in the Northeast China:constraints from temporal-spatial distribution and associations of volcanic rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[43]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 Wen-liang,WANG Feng,PEI Fu-ping,et al.Mesozoic tectonic regimes and regional ore-forming background in NE China:constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[44]李锦轶,莫申国,和政军,等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘,2004,11(3);157-168.LI Jin-yi,MO Shen-guo,HE Zheng-jun.et al.The timing of crustal sinistral strike-slip movement in the northern Great Khing'an ranges and its constraint on reconstruction of the crustal tectonic evolution of NE China and adjacent areas since the Mesozoic[J].Earth Science Frontiers,2004,11(3):157-168.
[45]莫申国,韩美莲,李锦轶,等.蒙古—鄂霍茨克造山带的组成及造山过程[J].山东科技大学学报:自然科学版,2006,24(3):50-52.MO Shen-guo,HAN Mei-lian,LI Jin-yi,et al.Compositions and orogenic processes of Mongolia--Okhotsk Orogen[J].Journal of Shangdong University of Science and Technology:Nature Science,2006,24(3):50-52.
[46]张允平.东北亚地区晚侏罗—白垩纪构造格架主体特点[J].吉林大学学报:地球科学版,2011,41(5):1267-1284.ZHANG Yun-ping.Main characteristics of Late Jurassic-Cretaceous tectonic framework in Northeast Asia[J].Journal of Jilin University:Earth Science Edition,2011,41(5):1267-1284.
[2]Zhang J H,Gao S,Ge W C,et al.Geochronology of the Mesozoic volcanic rocks in the Great Xing'an Range,northeastern China:implications for subductiion-induced delamination[J].Chemical Geology,2010,276:144-165.
[3]Zhang J H,Ge W C,Wu F Y,et al.Mesozoic bimodal volcanic suite in Zhalantun of the Da Hinggan Range and its geological significance:zircon U--Pb age and Hf isotopic constraints[J].Acta Geologic Sinica,2006,80:801-812.
[4]尹志刚,赵海滨,赵寒冬,等.大兴安岭北端塔木兰沟组玄武质岩石的地球化学特征及构造背景[J].地质通报,2005,24(9):848-853.YIN ZHi-gang,ZHAO Hai-bing,ZHAO Han-dong,et al.Geochemical characteristics and geotectonic background of basaltic rocks in Tamulangou Formation from the northern Da Hinggan Moutain[J].Geological Bulletin of China,2005,24(9):848-853.
[5]张玉涛,张连昌,周新华,等.大兴安岭北段牙克石地区玄武质火山岩的元素、同位素地球化学特征及其地质意义[J].地质通报,2008,27(1):112-120.ZHANG Yu-tao,ZHANG Lian-chang,ZHOU Xin-hua,et al.Geochemical of basaltic rocks from Yakeshi,northern Da Hinggan Moutain and its tectonic implications[J].Geological Bulletin of China,2008,27(1):112-120.
[6]周新华,英基丰,张连昌,等.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U--Pb年龄及多元同位素制约[J].地球科学(中国地质大学学报),2009,34(1):1-10.ZHOU Xin-hua,YING Ji-feng,ZHANG Lian-chang,et al.The petrogenesis of Late Mesozoic volcanic rock and the contributions from ancient micro-continents:constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hf isotopic systematics[J].Earth Science(Journal of China University of Geosciences),2009,34(1):1-10.
[7]孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U--Pb年代学、地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226.MENG En,XU Wen-liang,YANG De-bin,et al.Zircon U-Pb chronology,geochemistry of Mesozoic volcanic rocks from the Lingquan basin in Manzhouli area,and its tectonic implications[J].Acta Petrologica Sinica,2011,27(4):1209-1226.
[8]苟军,孙德有,赵忠华,等.满洲里南部白音高老组流纹岩锆石U--Pb定年及岩石成因[J].岩石学报,2010,26(1):333-344.GOU Jun,SUN De-you,ZHAO Zhong-hua,et al.Zircon LA-ICPMS U-Pb dating and petrogenesis of rhyolites in Baiyingaolao Formation from the southern Manzhouli,Inner Mongolia[J].Acta Petrologica Sinica,2010,26(1):333-344.
[9]孙德有,苟军,任云生,等.满洲里南部玛尼吐组火山岩锆石U--Pb年龄与地球化学研究[J].岩石学报,2011,27(10):3084-3094.SUN De-you,GOU Jun,REN Yun-sheng,et al.Zircon U--Pb dating and study on geochemistry of volcanic rocks in Manitu Formation from southern Manchuria,Inner Mongolia[J].Acta Petrologica Sinica,2011,27(10):3084-3094.
[10]林强,葛文春,曹林,等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学,2003,32(3):208-222.LIN Qiang,GE Wen-chun,CAO Lin,et al.Geochemistry of Mesozoic volcanic rocks in Da Hinggan Ling:the bimodal volcanic rocks[J].Geochimica,2003,32(3):208-222.
[11]葛文春,林强,孙德有,等.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据[J].岩石学报,1999,32(3):396-406.GE Wen-chun,LIN Qiang,SUN De-you,et al.Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling:evidence of the mantel-crust interaction[J].Acta Petrologica Sinica,1999,32(3):396-406.
[12]邵济安,臧绍先,牟保磊,等.造山带的伸展构造与软流圈隆起:以兴蒙造山带为例[J].科学通报,1994,39(6):533-537.SHAO Ji-an,ZANG Shao-xian,MOU Bao-lei,et al.Extensional structures within the orogenic belt and asthenosphere uplift-taking Xing--Meng orogenic belt as an example[J].Chinese Science Bulletin,1994,39(6):533-537.
[13]Fan W M,Guo F,Wang Y J,et al.Late Mesozoic calcalkaline volcanic of post-orogenic extension in the northern Da Hinggan Moutains,northeatern China[J].Journal of Volcanology and Geothermal Research,2003,121:115-135.
[14]Meng Q R.What drove Late Mesozoic extension of the northern China-Mongolia tract[J].Tectonophysics,2003,369:155-174.
[15]张玉涛,张连昌,英基丰,等.大兴安岭北段塔河地区早白垩世火山岩地球化学及源区特征[J].岩石学报,2007,23(11):2811-2822.ZHANG Yu-tao,ZHANG Lian-chang,YING Ji-feng,et al.Geochemistry and source characteristics of early Cretaceous volcanic rocks in Tahe,north Da Hinggan Mountain[J].Acta Petrologica Sinica,2007,23(11):2811-2822.
[16]蒋国源,权恒.大兴安岭根河、海拉尔盆地中生代火山岩[J].中国地质科学院沈阳地质矿产研究所所刊,1988,17:23-100.JIANG Guo-yuan,QUAN Heng.Mesozoic volcanic rocks in the Genhe and Hailaer Basin Da Hinggan Mountain[J].Journal of Shenyang Institute of Geology and mineral resources,Chinese Academy of Geological Sciences,1988,17:23-100.
[17]内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1993:244-249.Geology and Mineral Bureau of Inner Mongolia.Regional geology of Inner Mongolia[M].Beijing:Geological Publishing House,1993:244-249.
[18]内蒙古自治区地质矿产局.内蒙古自治区岩石地层[M].武汉:中国地质大学出版社,1996:256-264.Geology and Mineral Bureau of Inner Mongolia.Lithostratigraphy of Inner Mongolia[M].Wuhan:China University of Geosciences Press,1996:256-264.
[19]Andersen T.Correction of common lead in U--Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1):59-79.
[20]李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA--ICP--MS)测定锆石U--Pb同位素年龄的研究[J].矿物学报,2009(增刊1):600-601.LI Huai-kun,GENG Jian-feng,HAO Shuang,et al.Study on the determination of zircon U-Pb isotopic age by laser ablation multi receiver plasma mass spectrometer(LA--ICP--MS)[J].Acta Mineralogica Sinica,2009(Suppl.1):600-601.
[21]William I S,Buick A,Cartwright.An extended episode of early Mesoproterozoic metamophic fluid flow in the Reynold Region,central Australia[J].Journal of Metamorphic Geology,1996,14:29-47.
[22]Belousova E A,Griffin W L,O'Reilly,et al.Igneous zircon:trace element composition as an indicator of source rock type[J].Contributions to Mineraloy and Petrology,2002,143:602-622.
[23]Le Maitre R W,Bakteman P,Dudek A,et al.A classification of igneous rocks and glossary of terms:recommendations of the international union of geological sciences subcommission on the systematics of igneous rocks[M].Oxford:Blackwell Scientific Publications,1989:1-193.
[24]Boynton W V.Cosmochemistry of the rare earth elements:meteorite studies[M].New York:Elsevier Science Publishing Company Inc.1984:63-114.
[25]Sun S S,Mc Donough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and Process[J].Geological Society Special publications,1989,42:313-345.
[26]张超,杨伟红,和钟铧,等.大兴安岭中南段塔尔气地区满克头鄂博组流纹岩年代学和地球化学研究[J].世界地质,2014,33(2):255-265.ZHANG Chao,YANG Wei-hong,HE Zhong-hua,et al.Chronology and geochemistry of rhyolites in Manketou'ebo Formation from Ta'erqi area,southerncentral Greater Xing'an Range[J].Global Geology,2014,33(2):255-265.
[27]李鹏川,李世超,刘正宏,等.内蒙古林西地区满克头鄂博组火山岩形成时代及构造环境[J].世界地质,2016,35(1):77-88.LI Peng-chuan,LI Shi-chao,LIU Zheng-hong,et al.Formation age and environment of the volcanic rocks from the Manketouebo Formation in Linxi area,Inner Mongolia[J].Global Geology,2016,35(1):77-88.
[28]杨扬,高福红,陈井胜,等.赤峰地区中生代火山岩锆石U--Pb年代学证据[J].吉林大学学报:地球科学版,2012,42(增刊2):257-268.YANG Yang,GAO Fu-hong,CHEN Jing-sheng,et al.Zircon U--Pb ages of Mesozoic volcanic rocks in Chifeng area[J].Journal of Jilin University:Earth Science Edition,2012,42(Suppl.2):257-268.
[29]赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319-328.ZHAO Yue,XU Gang,ZHANG shuan-hong,et al.Yanshanian movement and conversion of tectonic regimes in East Asia[J].Earth Science Fronties,2004,11(3):319-328.
[30]李宇,丁磊磊,许文良,等.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[J].岩石学报,2015,31(1):1-11.LI Yu,DING Lei-lei,XU Wen-liang,et al.Geochronology and geochemistry of muscovite granite in Sunwu area,NE China:implications for the timing of closure of the Mongol-Okhotsk Ocean[J].Acta Petrologica Sinica,2015,31(1):1-11.
[31]Hirose K.Melting experiments on lherzolite KLB1 under hydrous conditions and generation of high-magnesian andesitic melts[J].Geology,1997,25(1):42-44.
[32]葛文春,林强,孙德有,等.大兴安岭中生代两类流纹岩成因的地球化学研究[J].地球科学(中国地质大学学报),2000,25(2):172-178.GE Wen-chun,LIN Qiang,SUN De-you,et al.Geochemical research into origins of two types of Mesozoic rhyolites in Daxing'anling[J].Earth Science(Journal of China University of Geosciences),2000,25(2):172-178.
[33]张旗,王焰,李承东,等.花岗岩的Sr--Yb分类及其地质意义[J].岩石学报,2006,22(9):2249-2269.ZHANG Qi,WANG Yan,LI Cheng-dong,et al.Granite classification on the basis of Sr and Yb contents and its implications[J].Acta Petrologic Sinica,2006,22(9):2249-2269.
[34]张旗.大陆花岗岩的地球动力学意义[J].岩石矿物学杂志,2014,33(4):785-798.ZHANG Qi.Geodynamic implications of continental granites[J].Acta Petrologica et Mineralogica,2014,33(4):785-798.
[35]张旗,冉皞,李承东.A型花岗岩的实质是什么?[J].岩石矿物学杂志,2012,31(4):621-626.ZHANG Qi,RAN Hao,LI Cheng-dong.A-type granite:What is the essence?[J].Acta Petrologica et Mineralogica,2012,31(4):621-626.
[36]李世超,徐仲元,刘正宏,等.大兴安岭中段玛尼吐组火山岩LA--ICP--MS锆石U--Pb年龄及地球化学特征[J].地质通报,2013,23(2/3):399-407.LI Shi-chao,XU Zhong-yuan,LIU Zheng-hong,et al.Zircon U-Pb dating and geochemical study of volcanic rocks in Manitu Formation of central Da Hinggan Mountains[J].Geological Bulletin of China,2013,32(2/3):399-407.
[37]Ying J F,Zhou X H,Zhang L C,et al.Geochronological framework of Mesozoic volcanic rocks in the Great Xing'an Range,NE China,and their geodynamic implications[J].Journal of Asian Earth Sciences,2010,39(6):786-793.
[38]纪政,葛文春,杨浩,等.大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J].世界地质,2016,35(2):283-296.JI Zheng,GE Wen-chun,YANG Hao,et al.Petrogenesis of Early Cretaceous granites in Taerqi area of central Great Xing'an Range and its tectonic setting[J].Global Geology,2016,35(2):283-296.
[39]张旗,金惟俊,李承东,等.再论花岗岩按照SrYb分类:标志[J].岩石学报,2010,26(4):985-1015.ZHANG Qi,JIN Wei-jun,LI Cheng-dong,et al.Revisiting the new classification of granitic rocks based on whole-rock Sr and Yb contents:Index[J].Acta Petrologic Sinica,2010,26(4):985-1015.
[40]Barbarin B.A review of the relationships between granitoid types,their origins and their geodynamic enviroments[J].Lithos,1999,46(3):605-626.
[41]Pearce J A,Bender J F,De Long S E,et al.Genesis of collision volcanism in Eastern Anatolia,Turkey[J].Journal of Volcanology and Geothermal Research,1990,44(1/2):189-229.
[42]孟凡超,刘嘉麒,崔岩,等.中国东北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 Fan-chao,LIU Jia-qi,CUI Yan,et al.Mesozoic tectonic regimes transition in the Northeast China:constraints from temporal-spatial distribution and associations of volcanic rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[43]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 Wen-liang,WANG Feng,PEI Fu-ping,et al.Mesozoic tectonic regimes and regional ore-forming background in NE China:constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[44]李锦轶,莫申国,和政军,等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘,2004,11(3);157-168.LI Jin-yi,MO Shen-guo,HE Zheng-jun.et al.The timing of crustal sinistral strike-slip movement in the northern Great Khing'an ranges and its constraint on reconstruction of the crustal tectonic evolution of NE China and adjacent areas since the Mesozoic[J].Earth Science Frontiers,2004,11(3):157-168.
[45]莫申国,韩美莲,李锦轶,等.蒙古—鄂霍茨克造山带的组成及造山过程[J].山东科技大学学报:自然科学版,2006,24(3):50-52.MO Shen-guo,HAN Mei-lian,LI Jin-yi,et al.Compositions and orogenic processes of Mongolia--Okhotsk Orogen[J].Journal of Shangdong University of Science and Technology:Nature Science,2006,24(3):50-52.
[46]张允平.东北亚地区晚侏罗—白垩纪构造格架主体特点[J].吉林大学学报:地球科学版,2011,41(5):1267-1284.ZHANG Yun-ping.Main characteristics of Late Jurassic-Cretaceous tectonic framework in Northeast Asia[J].Journal of Jilin University:Earth Science Edition,2011,41(5):1267-1284.