新疆东天山博格达造山带西段基性侵入岩的U-Pb年代学、地球化学及其构造意义
|
摘要
博格达造山带广泛分布着基性侵入岩体,其成因对正确认识该区地球动力学背景具有重要意义。对位于博格达造山带西段的基性侵入岩体分别进行了岩石学、岩石地球化学以及LA-ICP-MS锆石U-Pb年代学的研究,从而探讨其岩石成因及构造意义,以期为解决博格达造山带的地质构造演化提供依据。岩石地球化学分析结果显示,基性侵入岩w(SiO2)介于48.08%~50.88%之间,全碱(ALK)质量分数为3.09%~4.39%(小于5%),富CaO(6.87%~11.41%)、贫Al2O3(12.59%~18.49%),w(MgO)介于3.78%~7.66%之间,Mg#值为31.75~65.73(均值为51.29),铝饱和指数值A/CNK为0.60~0.80,属准铝质中钾钙碱性岩石系列。岩石总稀土元素质量分数较低,且轻重稀土元素之间以及轻重稀土元素内部不存在明显的分馏过程;微量元素中Th、Ta、Nb元素明显亏损,Ti元素亏损不明显以及U元素轻微富集,反映岩石具大陆裂谷岩浆活动特点。有关微量元素、稀土元素的相关图解及其比值,指示该区基性侵入岩岩浆源于亏损的岩石圈地幔,侵位过程中受到了地壳物质的混染,分异演化程度较低,为原始尖晶石相橄榄岩经较高程度的部分熔融的产物,形成于板内裂谷的构造环境。此外,辉长岩LA-ICP-MS锆石U-Pb定年结果表明,其形成年龄为(305.0±1.6)Ma(晚石炭世末期),处于博格达裂谷火山活动期晚期,为博格达西段裂谷作用由全面伸展向局限伸展转换的标志。综合对比区域研究成果,认为晚古生代期间(早石炭世-早二叠世),博格达造山带存在大面积与真正裂谷演化有关的岩浆活动,造山带是在裂谷基础上发展起来的,其形成可能与古亚洲洋沿克拉麦里碰撞带向准-吐-哈地块斜向俯冲作用有关。
The Bogda orogenic belt is widely distributed with basic intrusive rock mass,and its origin is of great significance to correctly understand the geodynamic background of the area.This paper studies systematically petrology,geochemistry and zircon U-Pb geochronology of basic intrusive rocks in the west of Bogda orogenic belt in order to define its petrogenesis and tectonic significance,and then to provide a basis for solving geological tectonic evolution of the belt.Rock geochemical analyses show that its SiO2 ranges from 48.08% to 50.88%,and ALK from 3.09% to 4.39%(less than 5%),rich in CaO(6.87%-11.41%),and depleted in Al2 O3(12.59%-18.49%).It has MgO ranging from 3.78% to 7.66%,and Mg#=31.75-65.73(the average is 51.29),A/CNK=0.60-0.80,indicating that it belongs to metaluminous middle K calc-alkaline rock series.The analysis also shows that the belt has low REE(36.30×10-6-101.41×10-6),between light and heavy rare earth and heavy rare earth internal no obvious fractionation process.Obvious loss of Th,Ta and Nb element,no obvious loss of Ti and slight enrichment in U element,show the characteristics of continental rift magmatism.The relevant diagram and the ratio about the trace elements and rare earth elements,indicate that the basic intrusive rock magma originates from the loss lithospheric mantle,suffering contamination of the crust,with low differentiation evolution degree,as the original phase spinel peridotite higher degree of partial melting,formed in the intraplate rift environment.Moreover,gabbro LA-ICP-MS zircon U-Pb dating results show that the forming age of(305.0±1.6)Ma(Latest Carboniferous),in the late period of the Bogda rift volcano activity,indicates the west of Bogda rift underwent a conversion from the overall extension stage to the confined extension stage.The analysed of regional geological datas claim that there is a large rift evolution related to magmatism and during Late Paleozoic Era(Early Carboniferous-Early Permian),the orogenic belt developed on the basis of rifting.Propably,its formation is related to the oblique subduction of the Paleo-Asian Ocean plate towards the Junggar-Turpan-Kumul plates along the Kalameili subduction belt.
The Bogda orogenic belt is widely distributed with basic intrusive rock mass,and its origin is of great significance to correctly understand the geodynamic background of the area.This paper studies systematically petrology,geochemistry and zircon U-Pb geochronology of basic intrusive rocks in the west of Bogda orogenic belt in order to define its petrogenesis and tectonic significance,and then to provide a basis for solving geological tectonic evolution of the belt.Rock geochemical analyses show that its SiO2 ranges from 48.08% to 50.88%,and ALK from 3.09% to 4.39%(less than 5%),rich in CaO(6.87%-11.41%),and depleted in Al2 O3(12.59%-18.49%).It has MgO ranging from 3.78% to 7.66%,and Mg#=31.75-65.73(the average is 51.29),A/CNK=0.60-0.80,indicating that it belongs to metaluminous middle K calc-alkaline rock series.The analysis also shows that the belt has low REE(36.30×10-6-101.41×10-6),between light and heavy rare earth and heavy rare earth internal no obvious fractionation process.Obvious loss of Th,Ta and Nb element,no obvious loss of Ti and slight enrichment in U element,show the characteristics of continental rift magmatism.The relevant diagram and the ratio about the trace elements and rare earth elements,indicate that the basic intrusive rock magma originates from the loss lithospheric mantle,suffering contamination of the crust,with low differentiation evolution degree,as the original phase spinel peridotite higher degree of partial melting,formed in the intraplate rift environment.Moreover,gabbro LA-ICP-MS zircon U-Pb dating results show that the forming age of(305.0±1.6)Ma(Latest Carboniferous),in the late period of the Bogda rift volcano activity,indicates the west of Bogda rift underwent a conversion from the overall extension stage to the confined extension stage.The analysed of regional geological datas claim that there is a large rift evolution related to magmatism and during Late Paleozoic Era(Early Carboniferous-Early Permian),the orogenic belt developed on the basis of rifting.Propably,its formation is related to the oblique subduction of the Paleo-Asian Ocean plate towards the Junggar-Turpan-Kumul plates along the Kalameili subduction belt.
引文
[1]Badarch G,Cunningham W D,Windley B F.A new terrane subdivision for Mongolia:Implications for the Phanerozoic crustal growth of Central Asia[J].Journal of Asian Earth Sciences,2002,21(1):87-110.
[2]Xiao W J,Zhang L C,Qin K Z,et al.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):Implications for the continental growth of central Asia[J].American Journal of Science,2004,304(4):370-395.
[3]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.
[4]马星华,陈斌,王超,等.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和SrNd同位素证据[J].岩石学报,2015,31(1):89-104.
[5]刘亮,何学锋,李江涛,等.新疆东部哈尔里克山沁城天生圈岩体岩石成因及其构造意义[J].地质科技情报,2017,36(2):86-96.
[6]李江涛,何学锋,刘亮,等.新疆东天山哈尔里克奥陶纪的构造属性:来自火山岩LA-ICP-MS锆石U-Pb年代学与地球化学的制约[J].现代地质,2017,31(3):460-473.
[7]Coleman R G.Continental growth of north west China[J].Tectonics,1989,8(1):621-635.
[8]方国庆.博格达晚古生代岛弧的沉积岩石学证据[J].沉积学报,1993,11(3):31-36.
[9]马瑞士,舒良树,孙家齐.东天山构造演化与成矿[M].北京:地质出版社,1997:1-202.
[10]李锦轶.新疆东部新元古代晚期和中生代构造格局及其演变[J].地质论评,2004,50(3):304-322.
[11]张传恒,刘典波,张传林,等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1):294-302.
[12]孙桂华,李锦轶,朱志新,等.新疆东部哈尔里克山南麓石炭纪砂岩碎屑锆石SHRIMP U-Pb定年及其地质意义[J].中国地质,2007,34(5):778-789.
[13]吴庆福.准噶尔盆地构造演化及含油气远景[J].新疆地质,1986,4(3):1-19.
[14]Sawkins F J.Metal deposits in relation to plate tectonics[M].Second Edition.Berlin:Springer-Verlag,1990:1-461.
[15]何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社,1994:37-214.
[16]Han Baofu,He Guoqi,Wang Shiguang.Postcollisional mantlederived magmatism,under plating and implications for basement of the Junggar Basin[J].Sience in China:Series D,1999,42(2):113-119.
[17]顾连兴,胡受奚,于春水,等.博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动[J].岩石学报,2001,17(2):187-198.
[18]顾连兴,胡受奚,于春水,等.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,2001,17(4):585-597.
[19]王银喜,顾连兴,张遵忠,等.博格达裂谷双峰式火山岩地质年代学与Nd-Sr-Pb同位素地球化学特征[J].岩石学报,2006,22(5):1215-1224.
[20]张小连,吴昌志,黄建华,等.东天山黄山岩体的侵位时代及其地质意义[J].地质科技情报,2012,31(1):26-30.
[21]汪晓伟,徐学义,马中平,等.博格达造山带东段芨芨台子地区晚石炭世双峰式火山岩地球化学特征及其地质意义[J].中国地质,2015,42(3):553-569.
[22]汪晓伟,徐学义,马中平,等.博格达造山带东段萨尔乔克地区早石炭世双峰式火山岩地球化学特征及其地质意义[J].地质科技情报,2015,34(3):58-70.
[23]崔方磊,汪晓伟,徐学义,等.东天山七角井-巴里坤地区辉绿岩脉年代学及岩石成因[J].西北地质,2015,48(2):43-56.
[24]舒良树,朱文斌,王博,等.新疆博格达南缘后碰撞期陆内裂谷和水下滑塌构造[J].岩石学报,2005,21(1):25-36.
[25]陕西省地矿局区域地质矿产研究院.新疆东天山吉木萨尔林场一带1∶5万四幅区域地质矿产调查[R].西安:陕西省地矿局区域地质矿产研究院,2017.
[26]Anderson T.Correction of Pb in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192:59-79.
[27]Ludwig K R.User's manual for Isoplot 3.00:A geochronological Toolkit for Microsoft Excel[M].California:Berkeley Geochronology Center,Special Publication,2003.
[28]Yuan H L,Wu F Y,Gao S,et al.Determination of U-Pb age and rare earth element concentrations of zircons from Cenozoic intrusions in northeastern China by laser ablation ICP-MS[J].Chinese Science Bulletin,2003,48(22):2411-2421.
[29]Qi L,Hu J,Gregoire D C.Determination of trace elements in granites by inductively coupled plasma mass spectrometry[J].Talanta,2000,51(3):507-513.
[30]吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604.
[31]李江涛,梁斌,何文劲,等.藏北羌塘盆地基底的地质构造演化:来自侏罗纪雁石坪群砂岩碎屑锆石U-Pb同位素年代学证据[J].中国地质,2016,43(4):1216-1226.
[32]Middlemost E A K.Naming materials in the magma/igneous rock system[J].Earth-Sci.Rev.,1994,37:215-224.
[33]Ewart A.The mineralogy and petrology of Tertiary:Recent orogenic volcanic rock with special reference to the andesitic-basaltic compositional range[C]∥Thorpe R S.Andesites.Chichester:Wiley,1982:25-87.
[34]Boynton WV.Geochemistry of the rare earth elements:Meteorite studies[C]∥Henderson P.Rare Earth element geochemistry.Amsterdam:Elsevier,1984:63-114.
[35]Sun S S,Mc Donough W F.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[C]∥Saunders A D,Norry M J.Magmatism in the ocean basins.[S.l.]:Geological Society London Special Publications,1989,42(1):313-345.
[36]Davies G R,Macdonald R.Crustal influences in the petrogenesis of the Naivasha basalt-comendite complex:Combined trace element and Sr-Nd-Pb isotope constraints[J].Journal of Petrology,1987,28(6):1009-1031.
[37]Eby G N.Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implications[J].The Journal of Geology,1992,20(7):641-644.
[38]王银喜,顾连兴,张遵忠,等.博格达裂谷闭合和区域隆起的同位素年代学证据及地质意义[J].地球学报,2005,26(增刊):102-104.
[39]王金荣,李泰德,田黎萍,等.新疆博格达造山带晚古生代构造-岩浆演化过程:火山岩组合及地球化学证据[J].岩石学报,2010,26(4):1103-1115.
[40]屈翠侠,杨兴科,易鹏飞,等.巴里坤塔格晚古生代侵入岩岩石地球化学与Sr-Nd-Pb同位素特征[J].西北地质,2015(2):17-30.
[41]雷万杉,许鹏,郭俊锋,等.博格达山东段苏吉山辉长岩LAICP-MS锆石U-Pb年龄、地质地球化学特征及构造意义[J].地质论评,2016,62(2):317-330.
[42]王盘喜,杨霄,卞孝东.冀中坳陷火成岩岩石学及地球化学特征[J].地质科技情报,2012,31(4):4-13.
[43]Zindler A,Hart S R.Chemical geodynamics[J].Ann.Rev.Earth Planet.Sci.,1986,14(1):493-571.
[44]邓晋福,罗照华,苏尚国,等.岩石成因、构造环境与成矿作用[M].北京:地质出版社,2004:3-149.
[45]Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Carton in China:Evidence,timing and mechanism[J].Phy.Chem.Earth,2001,26(9/10):747-757.
[46]Wilson M.Igneous petrogenesis[M].London:Unwin Hyman,1989:1-464.
[47]Condie K C.Plate tectonics and crustal evolution[M].London:Oxford Pergamon Press,1989:476.
[48]Condie K C.Geochemistry and tectonic setting of Early Proterozoic supercrustal rocks in the Southern United States[J].Journal of Geology,1986,94(6):845-864.
[49]Deniel C.Geochemical and isotopic(Sr,Nd,Pb)evidence for plume-lithosphere interactions in the genesis of Grande Comore magmas(Indian Ocean)[J].Chemical Geology,1998,144(3/4):281-303.
[50]Miller C,Schuster R,Klotzli U,et al.Post-collisional potassic and ultrapotassic magmatism in SW Tibet:Geochemical and SrNd-Pb-O isotopic constraints for mantle source characteristics and petrogenesis[J].Journal of Petrology,1999,40(9):1399-1424.
[51]Weaver B L.The origin of ocean island baslt end-member composition:Trace element an isotopic constraints[J].Earth Planet.Sci.Lett.,1991,104(2/3):381-397.
[52]Kieffer B,Arndt N,Lapierre H.Fllod and shield basalts from Ethiopia:Magmas from the African superswell[J].Petrol.,2004,45(4):793-834.
[53]Frey F A,Prinz M.Ultramafic inclusions from San Carlos,Arizona:Petrologic and geochemical data bearing on their petrogenesis[J].Earth Planet.Sci.Lett.,1978,38(1):129-176.
[54]汪晓伟,徐学义,马中平,等.博格达造山带东段早石炭世火山岩地球化学特征及构造属性[J].地质与勘探,2015,51(1):108-122.
[55]李平,刘伟,朱志新,等.博格达西段三个山石英闪长岩体地球化学特征、年代学及地质意义[J].新疆地质,2013,31(3),162-166.
[56]靳刘圆,刘伟,朱志新,等.博格达三个山地区基性岩墙U-Pb年龄、地球化学特征及地质意义[J].新疆地质,2014,32(3),316-321.
[57]田黎萍,王金荣,汤中立,等.新疆博格达山东段早石炭世火山岩地球化学特征及其构造意义[J].兰州大学学报:自然科学版,2010,46(4):30-41.
[58]舒良树,夏飞.新疆北部古生代大陆增生构造[J].新疆地质,2001,19(1):59-63.
[59]顾连兴,于春水,李宏宇,等.博格达上大河沿岩体铷-锶同位素年龄及其地质意义[J].矿物岩石地球化学通报,2000,19(1):19-21.
[60]第鹏飞,李泰德,王金荣,等.新疆博格达造山带东段二叠纪流纹岩地球化学特征及地质意义[J].兰州大学学报:自然科学版,2010,46(3):8-13.
[61]Pearce J A.Trace element characteristics of lavas from destructive plate boundaries[C]∥Thorps R S.Andesites.New York:John Wiley and Sons,1982:525-548.
[62]Pearce J A,Cann J R.Tectonic setting of basic volcanic rocks determined using trace element analyses[J].Earth Planet.Sci.Lett.,1973,19(2):290-300.
[63]李锦轶.新疆东准噶尔卡拉麦里地区古生代板块构造研究[D].北京:中国地质科学院,1988.
[64]何国琦,李茂松,贾进斗,等.论新疆东准噶尔蛇绿岩的时代及其意义[J].北京大学学报:自然科学版,2001,37(6):852-858.
[65]杨高学,李永军,吴宏恩,等.东准噶尔卡拉麦里地区黄羊山花岗岩和包体LA-ICP-MS锆石U-Pb测年及地质意义[J].岩石学报,2009,25(12):3197-3207.
[2]Xiao W J,Zhang L C,Qin K Z,et al.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):Implications for the continental growth of central Asia[J].American Journal of Science,2004,304(4):370-395.
[3]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.
[4]马星华,陈斌,王超,等.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和SrNd同位素证据[J].岩石学报,2015,31(1):89-104.
[5]刘亮,何学锋,李江涛,等.新疆东部哈尔里克山沁城天生圈岩体岩石成因及其构造意义[J].地质科技情报,2017,36(2):86-96.
[6]李江涛,何学锋,刘亮,等.新疆东天山哈尔里克奥陶纪的构造属性:来自火山岩LA-ICP-MS锆石U-Pb年代学与地球化学的制约[J].现代地质,2017,31(3):460-473.
[7]Coleman R G.Continental growth of north west China[J].Tectonics,1989,8(1):621-635.
[8]方国庆.博格达晚古生代岛弧的沉积岩石学证据[J].沉积学报,1993,11(3):31-36.
[9]马瑞士,舒良树,孙家齐.东天山构造演化与成矿[M].北京:地质出版社,1997:1-202.
[10]李锦轶.新疆东部新元古代晚期和中生代构造格局及其演变[J].地质论评,2004,50(3):304-322.
[11]张传恒,刘典波,张传林,等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1):294-302.
[12]孙桂华,李锦轶,朱志新,等.新疆东部哈尔里克山南麓石炭纪砂岩碎屑锆石SHRIMP U-Pb定年及其地质意义[J].中国地质,2007,34(5):778-789.
[13]吴庆福.准噶尔盆地构造演化及含油气远景[J].新疆地质,1986,4(3):1-19.
[14]Sawkins F J.Metal deposits in relation to plate tectonics[M].Second Edition.Berlin:Springer-Verlag,1990:1-461.
[15]何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社,1994:37-214.
[16]Han Baofu,He Guoqi,Wang Shiguang.Postcollisional mantlederived magmatism,under plating and implications for basement of the Junggar Basin[J].Sience in China:Series D,1999,42(2):113-119.
[17]顾连兴,胡受奚,于春水,等.博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动[J].岩石学报,2001,17(2):187-198.
[18]顾连兴,胡受奚,于春水,等.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,2001,17(4):585-597.
[19]王银喜,顾连兴,张遵忠,等.博格达裂谷双峰式火山岩地质年代学与Nd-Sr-Pb同位素地球化学特征[J].岩石学报,2006,22(5):1215-1224.
[20]张小连,吴昌志,黄建华,等.东天山黄山岩体的侵位时代及其地质意义[J].地质科技情报,2012,31(1):26-30.
[21]汪晓伟,徐学义,马中平,等.博格达造山带东段芨芨台子地区晚石炭世双峰式火山岩地球化学特征及其地质意义[J].中国地质,2015,42(3):553-569.
[22]汪晓伟,徐学义,马中平,等.博格达造山带东段萨尔乔克地区早石炭世双峰式火山岩地球化学特征及其地质意义[J].地质科技情报,2015,34(3):58-70.
[23]崔方磊,汪晓伟,徐学义,等.东天山七角井-巴里坤地区辉绿岩脉年代学及岩石成因[J].西北地质,2015,48(2):43-56.
[24]舒良树,朱文斌,王博,等.新疆博格达南缘后碰撞期陆内裂谷和水下滑塌构造[J].岩石学报,2005,21(1):25-36.
[25]陕西省地矿局区域地质矿产研究院.新疆东天山吉木萨尔林场一带1∶5万四幅区域地质矿产调查[R].西安:陕西省地矿局区域地质矿产研究院,2017.
[26]Anderson T.Correction of Pb in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192:59-79.
[27]Ludwig K R.User's manual for Isoplot 3.00:A geochronological Toolkit for Microsoft Excel[M].California:Berkeley Geochronology Center,Special Publication,2003.
[28]Yuan H L,Wu F Y,Gao S,et al.Determination of U-Pb age and rare earth element concentrations of zircons from Cenozoic intrusions in northeastern China by laser ablation ICP-MS[J].Chinese Science Bulletin,2003,48(22):2411-2421.
[29]Qi L,Hu J,Gregoire D C.Determination of trace elements in granites by inductively coupled plasma mass spectrometry[J].Talanta,2000,51(3):507-513.
[30]吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604.
[31]李江涛,梁斌,何文劲,等.藏北羌塘盆地基底的地质构造演化:来自侏罗纪雁石坪群砂岩碎屑锆石U-Pb同位素年代学证据[J].中国地质,2016,43(4):1216-1226.
[32]Middlemost E A K.Naming materials in the magma/igneous rock system[J].Earth-Sci.Rev.,1994,37:215-224.
[33]Ewart A.The mineralogy and petrology of Tertiary:Recent orogenic volcanic rock with special reference to the andesitic-basaltic compositional range[C]∥Thorpe R S.Andesites.Chichester:Wiley,1982:25-87.
[34]Boynton WV.Geochemistry of the rare earth elements:Meteorite studies[C]∥Henderson P.Rare Earth element geochemistry.Amsterdam:Elsevier,1984:63-114.
[35]Sun S S,Mc Donough W F.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[C]∥Saunders A D,Norry M J.Magmatism in the ocean basins.[S.l.]:Geological Society London Special Publications,1989,42(1):313-345.
[36]Davies G R,Macdonald R.Crustal influences in the petrogenesis of the Naivasha basalt-comendite complex:Combined trace element and Sr-Nd-Pb isotope constraints[J].Journal of Petrology,1987,28(6):1009-1031.
[37]Eby G N.Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implications[J].The Journal of Geology,1992,20(7):641-644.
[38]王银喜,顾连兴,张遵忠,等.博格达裂谷闭合和区域隆起的同位素年代学证据及地质意义[J].地球学报,2005,26(增刊):102-104.
[39]王金荣,李泰德,田黎萍,等.新疆博格达造山带晚古生代构造-岩浆演化过程:火山岩组合及地球化学证据[J].岩石学报,2010,26(4):1103-1115.
[40]屈翠侠,杨兴科,易鹏飞,等.巴里坤塔格晚古生代侵入岩岩石地球化学与Sr-Nd-Pb同位素特征[J].西北地质,2015(2):17-30.
[41]雷万杉,许鹏,郭俊锋,等.博格达山东段苏吉山辉长岩LAICP-MS锆石U-Pb年龄、地质地球化学特征及构造意义[J].地质论评,2016,62(2):317-330.
[42]王盘喜,杨霄,卞孝东.冀中坳陷火成岩岩石学及地球化学特征[J].地质科技情报,2012,31(4):4-13.
[43]Zindler A,Hart S R.Chemical geodynamics[J].Ann.Rev.Earth Planet.Sci.,1986,14(1):493-571.
[44]邓晋福,罗照华,苏尚国,等.岩石成因、构造环境与成矿作用[M].北京:地质出版社,2004:3-149.
[45]Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Carton in China:Evidence,timing and mechanism[J].Phy.Chem.Earth,2001,26(9/10):747-757.
[46]Wilson M.Igneous petrogenesis[M].London:Unwin Hyman,1989:1-464.
[47]Condie K C.Plate tectonics and crustal evolution[M].London:Oxford Pergamon Press,1989:476.
[48]Condie K C.Geochemistry and tectonic setting of Early Proterozoic supercrustal rocks in the Southern United States[J].Journal of Geology,1986,94(6):845-864.
[49]Deniel C.Geochemical and isotopic(Sr,Nd,Pb)evidence for plume-lithosphere interactions in the genesis of Grande Comore magmas(Indian Ocean)[J].Chemical Geology,1998,144(3/4):281-303.
[50]Miller C,Schuster R,Klotzli U,et al.Post-collisional potassic and ultrapotassic magmatism in SW Tibet:Geochemical and SrNd-Pb-O isotopic constraints for mantle source characteristics and petrogenesis[J].Journal of Petrology,1999,40(9):1399-1424.
[51]Weaver B L.The origin of ocean island baslt end-member composition:Trace element an isotopic constraints[J].Earth Planet.Sci.Lett.,1991,104(2/3):381-397.
[52]Kieffer B,Arndt N,Lapierre H.Fllod and shield basalts from Ethiopia:Magmas from the African superswell[J].Petrol.,2004,45(4):793-834.
[53]Frey F A,Prinz M.Ultramafic inclusions from San Carlos,Arizona:Petrologic and geochemical data bearing on their petrogenesis[J].Earth Planet.Sci.Lett.,1978,38(1):129-176.
[54]汪晓伟,徐学义,马中平,等.博格达造山带东段早石炭世火山岩地球化学特征及构造属性[J].地质与勘探,2015,51(1):108-122.
[55]李平,刘伟,朱志新,等.博格达西段三个山石英闪长岩体地球化学特征、年代学及地质意义[J].新疆地质,2013,31(3),162-166.
[56]靳刘圆,刘伟,朱志新,等.博格达三个山地区基性岩墙U-Pb年龄、地球化学特征及地质意义[J].新疆地质,2014,32(3),316-321.
[57]田黎萍,王金荣,汤中立,等.新疆博格达山东段早石炭世火山岩地球化学特征及其构造意义[J].兰州大学学报:自然科学版,2010,46(4):30-41.
[58]舒良树,夏飞.新疆北部古生代大陆增生构造[J].新疆地质,2001,19(1):59-63.
[59]顾连兴,于春水,李宏宇,等.博格达上大河沿岩体铷-锶同位素年龄及其地质意义[J].矿物岩石地球化学通报,2000,19(1):19-21.
[60]第鹏飞,李泰德,王金荣,等.新疆博格达造山带东段二叠纪流纹岩地球化学特征及地质意义[J].兰州大学学报:自然科学版,2010,46(3):8-13.
[61]Pearce J A.Trace element characteristics of lavas from destructive plate boundaries[C]∥Thorps R S.Andesites.New York:John Wiley and Sons,1982:525-548.
[62]Pearce J A,Cann J R.Tectonic setting of basic volcanic rocks determined using trace element analyses[J].Earth Planet.Sci.Lett.,1973,19(2):290-300.
[63]李锦轶.新疆东准噶尔卡拉麦里地区古生代板块构造研究[D].北京:中国地质科学院,1988.
[64]何国琦,李茂松,贾进斗,等.论新疆东准噶尔蛇绿岩的时代及其意义[J].北京大学学报:自然科学版,2001,37(6):852-858.
[65]杨高学,李永军,吴宏恩,等.东准噶尔卡拉麦里地区黄羊山花岗岩和包体LA-ICP-MS锆石U-Pb测年及地质意义[J].岩石学报,2009,25(12):3197-3207.