北阿尔金西段正长花岗岩和闪长岩地球化学、锆石U-Pb定年及Hf同位素特征
|
摘要
北阿尔金西段出露大量中酸性侵入岩,为探讨西段地区花岗质岩石的成因、形成环境以及北阿尔金地区岩浆活动特点,本文选取北阿尔金西段的正长花岗岩体和闪长岩体作为研究对象,进行了岩石学、地球化学、锆石U-Pb年代学及Hf同位素等方面的研究。研究结果表明,正长花岗岩体形成时代为495.7～502.0Ma,铝饱和指数A/CNK为0.86～1.09小于1.1,P_2O_5与SiO_2含量呈负相关,具I型花岗岩特征。轻稀土富集而重稀土亏损,具有明显的负Eu异常,微量元素特征显示富集Rb、Ba、Th、U、K等元素,相对亏损Nb、Ta、P、Ti等元素。岩石地球化学及锆石Hf同位素特征暗示其源区物质成分不均一,源岩主要为0.95～1.4Ga的新生地壳(变中基性岩),并有1.42～1.83Ga的古老地壳物质的参与。闪长岩体的侵位时代为497.1±3Ma,轻稀土富集而重稀土亏损,较弱的负Eu异常,相对富集Rb、Ba、Th、U、K等元素,而亏损Nb、Ta、P、Ti。锆石ε_(Hf)(t)值为-1.61～+2.16,二阶段模式年龄t_(DM2)为1.34～1.56Ga,暗示其源岩可能主要为新生地壳,并有古老地壳物质参与成岩。北阿尔金西段正长花岗岩、闪长岩均形成于早古生代,具弧型花岗岩特点,结合区域构造背景,认为其形成可能与北阿尔金洋壳俯冲有关,产于陆弧环境。
Abundant intermediate-acid intrusions were widely outcropped in the western segment of North Altyn.In order to investigate the petrogenesis and formation environment of the granitoids in the western segment,and the features of magmatic activity,the syenogranite and diorite from the western segment of North Altyn were chosen to study by means of petrology,geochemistry,zircon U-Pb chronology and Hf isotope.The results show that the zircon U-Pb ages for the syenogranite are 495.7～502.0Ma.These rocks show signatures of I-type granite,with aluminum saturation index(A/CNK=0.86～1.09)less than 1.1 and a negative correlation between P_2O_5and SiO_2.The syenogranite samples show steep REE patterns,with LREE enrichment relative to HREE,and pronounced negative Eu.They also show characteristic distribution,with pronounced enrichments in Rb,Ba,Th,U,K and depletions of Nb,Ta,P,Ti.Geochemistry and zircon Hf isotopic characteristics suggest that the composition of the source is heterogeneous.The source rocks of the syenogranite were mainly intermediate-basic metaigneous rocks of the juvenile crust(0.95～1.4Ga),and minor ancient crust(1.42～1.83Ga).The diorite was emplaced in 497.1±3Ma,with LREE enrichment relative to HREE,slightly negative Eu,enrichments in Rb,Ba,Th,U,K and depletions of Nb,Ta,P,Ti.The zirconε_(Hf)(t)values of the diorite rang from-1.61～+2.16.The two-stage model age(t_(DM2))are varied in 1.34～1.56Ga.These characteristics indicate that the source rocks probablely derived from the juvenile crust and a small amount of ancient crust.The syenogranite and diorite were formed in the Early Paleozoic.They have the characteristics of the arc granites.In combination with the regional tectonic setting,these rocks were probablely formed in continental arc setting related to the subduction of oceanic crust.
Abundant intermediate-acid intrusions were widely outcropped in the western segment of North Altyn.In order to investigate the petrogenesis and formation environment of the granitoids in the western segment,and the features of magmatic activity,the syenogranite and diorite from the western segment of North Altyn were chosen to study by means of petrology,geochemistry,zircon U-Pb chronology and Hf isotope.The results show that the zircon U-Pb ages for the syenogranite are 495.7～502.0Ma.These rocks show signatures of I-type granite,with aluminum saturation index(A/CNK=0.86～1.09)less than 1.1 and a negative correlation between P_2O_5and SiO_2.The syenogranite samples show steep REE patterns,with LREE enrichment relative to HREE,and pronounced negative Eu.They also show characteristic distribution,with pronounced enrichments in Rb,Ba,Th,U,K and depletions of Nb,Ta,P,Ti.Geochemistry and zircon Hf isotopic characteristics suggest that the composition of the source is heterogeneous.The source rocks of the syenogranite were mainly intermediate-basic metaigneous rocks of the juvenile crust(0.95～1.4Ga),and minor ancient crust(1.42～1.83Ga).The diorite was emplaced in 497.1±3Ma,with LREE enrichment relative to HREE,slightly negative Eu,enrichments in Rb,Ba,Th,U,K and depletions of Nb,Ta,P,Ti.The zirconε_(Hf)(t)values of the diorite rang from-1.61～+2.16.The two-stage model age(t_(DM2))are varied in 1.34～1.56Ga.These characteristics indicate that the source rocks probablely derived from the juvenile crust and a small amount of ancient crust.The syenogranite and diorite were formed in the Early Paleozoic.They have the characteristics of the arc granites.In combination with the regional tectonic setting,these rocks were probablely formed in continental arc setting related to the subduction of oceanic crust.
引文
Altherr R,Holl A,Hegner E,Langer C and Kreuzer H.2000.Highpotassium,calc-alkaline I-type plutonism in the European Variscides:Northern Vosges(France)and northern Schwarzwald(Germany).Lithos,50(1-3):51-73
Bea F,Pereira MD and Stroh A.1994.Mineral/leucosome trace-element partitioning in a peraluminous migmatite(a laser ablation-ICP-MSstudy).Chemical Geology,117(1-4):291-312
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets.Earth and Planetary Science Letters,273(1-2):48-57
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Che ZC,Liu L,Liu HF and Luo JH.1995.Discovery and occurrence of high-pressure metapelitic rocks from Altun Mountain areas,Xinjiang Autonomous Region.Chinese Science Bulletin,40(23):1988-1991
Chen XH,Gehrels G,Wang XF,Yang F and Chen ZL.2003.Granite from North Altyn Tagh,NW China:U-Pb geochronology and tectonic setting.Bulletin of Mineralogy,Petrology and Geochemistry,22(4):294-298(in Chinese with English abstract)
Corfu F,Hanchar JM,Hoskin PWO and Kinny P.2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry,53(1):469-500
Gai YS,Liu L,Kang L,Yang WQ,Liao XY and Wang YW.2015.The origin and geologic significance of plagiogranite in ophiolite belt at North Altyn Tagh.Acta Petrologica Sinica,31(9):2549-2565(in Chinese with English abstract)
Gao XF,Xiao PX,Guo L,Dong ZC and Xi RG.2011.Opening of an Early Paleozoic limited oceanic basin in the northern Altyn area:Constraints from plagiogranites in the Hongliugou-Lapeiquan ophiolitic mélange.Science China(Earth Science),54(12):1871-1879
Gehrels GE,Yin A and Wang XF.2003.Magmatic history of the northeastern Tibetan Plateau.Journal of Geophysical Research:Solid Earth,108(B9):2423
Gorton MP and Schandl ES.2000.From continents to island arcs:Ageochemical index of tectonic setting for arc-related and within-plate felsic to intermediate volcanic rocks.The Canadian Mineralogist,38(5):1065-1073
Han FB,Chen BL,Cui LL,Wang SX,Chen ZL,Jiang RB,Li L and Qi WX.2012.Zircon SHRIMP U-Pb age of intermediate-acid intrusive rocks in Kaladawan area,eastern Altun Mountains,NW China,and its implications.Acta Petrologica Sinica,28(7):2277-2291(in Chinese with English abstract)
Hao J,Wang EQ,Liu XH and Sang HQ.2006.Jinyanshan collisional oroginic belt of the Early Paleozoic in the Altun mountains:Evidence from single zircon U-Pb and40Ar/39Ar isotopic dating for the arc magmatite and ophiolitic mélange.Acta Petrologica Sinica,22(11):2743-2752(in Chinese with English abstract)
Hao RX,Chen BL,Chen ZL,Wang Y,Li SB,Han FB and Zhou YG.2013.Geochemical characteristics of basalts from Kaladawan in East Altun Mountains of Xinjiang and their implications.Acta Geoscientica Sinica,34(3):307-317(in Chinese with English abstract)
Kang L,Liu L,Cao YT,Wang C,Yang WQ and Zhu XH.2011.Geochemistry,zircon LA-ICP-MS U-Pb ages and Hf isotopes of Hongliugou moyite from north Altyn Tagh tectonic belt.Geological Bulletin of China,30(7):1066-1076(in Chinese with English abstract)
Kaygusuz A,Siebel W,爦en C and Satir M.2008.Petrochemistry and petrology of I-type granitoids in an arc setting:The composite Torul pluton,Eastern Pontides,NE Turkey.International Journal of Earth Sciences,97(4):739-764
Koschek G.1993.Origin and significance of the SEMcathodoluminescence from zircon.Journal of Microscopy,171(3):223-232
Li SB.2013.The Early Paleozoic tectonic evolution of Kaladawan area,northern Altyn Taugh.Master Degree Thesis.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Liu L.1999.High pressure metamorphic rocks and ophiolite in Altun,and its tectonic significance.Ph.D.Dissertation.Beijing:Institute of Geology and Geophysics,Chinese Academy of Geological Sciences(in Chinese)
Liu L,Chen DL,Wang C and Zhang CL.2009.New progress on geochronology of high-pressure/ultrahigh-pressure metamorphic rocks from the South Altyn Tagh,the North Qaidam and the North Qinling orogenic,NW China and their geological significance.Journal of Northwest University(Natural Science Edition),39(3):472-479(in Chinese with English abstract)
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.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
Ludwig KR.2003.User’s Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel.Berkeley CA:Berkeley Geochronology Center
Maniar PD and Piccoli PM.1989.Tectonic discrimination of granitoids.Geological Society of America Bulletin,101(5):635-643
Meng LT,Chen BL,Wang Y,Sun Y,Wu Y,Zhang WG and He JT.2016.Timing of Early Paleozoic tectonic regime transition in North Altun:Evidence from granite.Geotectonica et Metallogenia,40(2):295-307(in Chinese with English abstract)
Meng LT,Chen BL,Zhao NN,Wu Y,Zhang WG,He JT,Wang B and Han MM.2017.The distribution,geochronology and geochemistry of Early Paleozoic granitoid plutons in the North Altun orogenic belt,NW China:Implications for the petrogenesis and tectonic evolution.Lithos,268-271:399-417
Niu YL,Zhao ZD,Zhu DC and Mo XX.2013.Continental collision zones are primary sites for net continental crust growth:A testable hypothesis.Earth-Science Reviews,127:96-110
Pati1o Douce AE and Johnston AD.1991.Phase equilibria and melt productivity in the pelitic system:Implications for the origin of peraluminous granitoids and aluminous granulites.Contributions to Mineralogy and Petrology,107(2):202-218
Qi XX,Li HB,Wu CL,Yang JS,Zhang JX,Meng FC,Shi RD and Chen SY.2005a.SHRIMP U-Pb zircon dating for Qiashikansayi granodiorite,the northern Altyn Tagh Mountains and its geological implications.Chinese Science Bulletin,50(5):440-445
Qi XX,Wu CL and Li HB.2005b.SHRIMP U-Pb age of zircons from Kazisayi granite in the northern Alty Tagh Mountains and its significations.Acta Petrologica Sinica,21(3):859-866(in Chinese with English abstract)
Rickwood PC.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Scherer E,Münker C and Mezger K.2001.Calibration of the lutetiumhafnium clock.Science,293(5530):683-687
Sisson TW.1994.Hornblende-melt trace-element partitioning measured by ion microprobe.Chemical Geology,117(1-4):331-344
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Sylvester PJ.1998.Post-collisional strongly peraluminous granites.Lithos,45(1-4):29-44
Taylor SR and Mc Clennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publication,1-132
Wang XL.2017.Some new research progresses and main scientific problems of granitic rocks.Acta Petrologica Sinica,33(5):1445-1458(in Chinese with English abstract)
Wu CL,Yang JS,Yao SZ,Zeng LS,Chen SY,Li HB,Qi XX,Wooden JL and Mazdab FK.2005.Characteristics of the granitoid complex and its zircon SHRIMP dating at the south margin of the Bashikaogong Basin,North Altun,NW China.Acta Petrologica Sinica,21(3):846-858(in Chinese with English abstract)
Wu CL,Yao SZ,Zeng LS,Yang JS,Wooden JL,Chen SY and Mazdab FK.2006.Bashikaogong-Shimierbulake granitic complex,North Altun,NW China:Geochemistry and zircon SHRIMP ages.Science in China(Series D),49(12):1233-1251
Wu CL,Yang JS,Robinson PT,Wooden JL,Mazdab FK,Gao YH,Wu SP and Chen QL.2009.Geochemistry,age and tectonic significance of granitic rocks in north Altun,northwest China.Lithos,113(3-4):423-436
Wu CL,Lei M,Wu D,Zhang X,Chen HJ and Li TX.2016.Zircon U-Pb dating of Paleozoic granites from south Altun and response of the magmatic activity to the tectonic evolution of the Altun Orogenic Belt.Acta Geologica Sinica,90(9):2276-2315(in Chinese with English abstract)
Wu FY,Jahn BM,Wilde SA,Lo CH,Yui TF,Lin Q,Ge WC and Sun DY.2003.Highly fractionated I-type granites in NE China(Ⅰ):Geochronology and petrogenesis.Lithos,66(3-4):241-273
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Wu J,Lan CL,Li JL and Yu LJ.2002.Geochemical evidence of MORBand OIB combination in Hongliugou ophiolite melanges,Altun fault belt.Acta Petrologica et Mineralogica,21(1):24-30(in Chinese with English abstract)
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xu ZQ,Yang JS,Zhang JX,Jiang M,Li HB and Cui JW.1999.Acomparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing.Acta Geologica Sinica,73(3):193-205(in Chinese with English abstract)
Yang JS,Shi RD,Wu CL,Su DC,Chen SY,Wang XB and Wooden J.2008.Petrology and SHRIMP age of the Hongliugou ophiolite at Milan,North Altun,at the northern margin of the Tibetan Plateau.Acta Petrologica Sinica,24(7):1567-1584(in Chinese with English abstract)
Yang WQ,Liu L,Ding HB,Xiao PX,Cao YT and Kang L.2012.Geochemistry,geochronology and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagn and its geological significance.Acta Petrologica Sinica,28(12):4139-4150(in Chinese with English abstract)
Yang ZJ.Early palaeozoic tectonic evolution in Hongliugou,Altyn,Xinjiang.Ph.D.Dissertation.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Yu SY,Zhang JX,Li SZ,Sun DY,Peng YB and Zhao XL.2018.Continuity of the North Qilian and North Altun orogenic belts of NWChina:Evidence from newly discovered Palaeozoic low-Mg and highMg adakitic rocks.Geological Magazine,155(8):1684-1704
Zhang JX,Meng FC,Yu SY,Chen W and Chen SY.2007.39Ar-40Ar geochronology of high-pressure/low-temperature blueschist and eclogite in the North Altyn Tagh and their tectonic implications.Geology in China,34(4):558-564(in Chinese with English abstract)
Zhang ZW,Huang G,Li HM and Zhang WF.2012.LA-ICP-MS zircon U-Pb geochronology and geochemistry of gabbro and diorite from Qilesayi pluton in Lapeiquan area of northern Altun Mountains and their tectonic implications.Acta Petrologica et Mineralogica,31(1):13-27(in Chinese with English abstract)
车自成,刘良,刘洪福,罗金海.1995.阿尔金山地区高压变质泥质岩石的发现及其产出环境.科学通报,40(14):1298-1300
陈宣华,Gehrels G,王小凤,杨风,陈正乐.2003.阿尔金山北缘花岗岩的形成时代及其构造环境探讨.矿物岩石地球化学通报,22(4):294-298
盖永升,刘良,康磊,杨文强,廖小莹,王亚伟.2015.北阿尔金蛇绿混杂岩带中斜长花岗岩的成因及其地质意义.岩石学报,31(9):2549-2565
高晓峰,校培喜,过磊,董增产,奚仁刚.2012.北阿尔金地区早古生代有限洋盆开启时限:来自斜长花岗岩的证据.中国科学(地球科学),42(3):359-368
韩凤彬,陈柏林,崔玲玲,王世新,陈正乐,蒋荣宝,李丽,祁万修.2012.阿尔金山喀腊大湾地区中酸性侵入岩SHRIMP年龄及其意义.岩石学报,28(7):2277-2291
郝杰,王二七,刘小汉,桑海清.2006.阿尔金山脉中金雁山早古生代碰撞造山带:弧岩浆岩的确定与岩体锆石U-Pb和蛇绿混杂岩40Ar/39Ar年代学研究的证据.岩石学报,22(11):2743-2752
郝瑞祥,陈柏林,陈正乐,王永,李松彬,韩凤彬,周永贵.2013.新疆阿尔金山喀腊大湾地区玄武岩的地球化学特征及地质意义.地球学报,34(3):307-317
康磊,刘良,曹玉亭,王超,杨文强,朱小辉.2011.北阿尔金构造带红柳沟钾长花岗岩地球化学特征、LA-ICP-MS锆石U-Pb定年和Hf同位素组成.地质通报,30(7):1066-1076
李松彬.2013.阿尔金北缘喀腊大湾地区早古生代构造演化.硕士学位论文.北京:中国地质科学院
刘良.1999.阿尔金高压变质岩与蛇绿岩及其大地构造意义.博士学位论文.北京:中国科学院地质与地球物理研究所
刘良,陈丹玲,王超,张成立.2009.阿尔金、柴北缘与北秦岭高压-超高压岩石年代学研究进展及其构造地质意义.西北大学学报(自然科学版),39(3):472-479
孟令通,陈柏林,王永,孙岳,吴玉,张文高,何江涛.2016.北阿尔金早古生代构造体制转换的时限:来自花岗岩的证据.大地构造与成矿学,40(2):295-307
戚学祥,李海兵,吴才来,杨经绥,张建新,孟繁聪,史仁灯,陈松永.2005a.北阿尔金恰什坎萨依花岗闪长岩的锆石SHRIMP U-Pb定年及其地质意义.科学通报,50(6):571-576
戚学祥,吴才来,李海兵.2005b.北阿尔金喀孜萨依花岗岩锆石SHRIMP U-Pb定年及其构造意义.岩石学报,21(3):859-866
王孝磊.2017.花岗岩研究的若干新进展与主要科学问题.岩石学报,33(5):1445-1458
吴才来,杨经绥,姚尚志,曾令森,陈松永,李海兵,戚学祥,Wooden JL,Mazdab FK.2005.北阿尔金巴什考供盆地南缘花岗杂岩体特征及锆石SHRIMP定年.岩石学报,21(3):846-858
吴才来,姚尚志,曾令森,杨经绥,Wooden JL,陈松永,Mazdab FK.2007.北阿尔金巴什考供-斯米尔布拉克花岗杂岩特征及锆石SHRIMP U-Pb定年.中国科学(D辑),37(1):10-26
吴才来,雷敏,吴迪,张昕,陈红杰,李天啸.2016.南阿尔金古生代花岗岩U-Pb定年及岩浆活动对造山带构造演化的响应.地质学报,90(9):2276-2315
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
吴峻,兰朝利,李继亮,俞良军.2002.阿尔金红柳沟蛇绿混杂岩中MORB与OIB组合的地球化学证据.岩石矿物学杂志,21(1):24-30
许志琴,杨经绥,张建新,姜枚,李海兵,崔军文.1999.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制.地质学报,73(3):193-205
杨经绥,史仁灯,吴才来,苏德辰,陈松永,王希斌,Wooden J.2008.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年.岩石学报,24(7):1567-1584
杨文强,刘良,丁海波,校培喜,曹玉亭,康磊.2012.南阿尔金迪木那里克花岗岩地球化学、锆石U-Pb年代学与Hf同位素特征及其构造地质意义.岩石学报,28(12):4139-4150
杨子江.2012.新疆阿尔金红柳沟一带早古生代地质构造演化研究.博士学位论文.北京:中国地质科学院
张建新,孟繁聪,于胜尧,陈文,陈松永.2007.北阿尔金HP/LT蓝片岩和榴辉岩的Ar-Ar年代学及其区域构造意义.中国地质,34(4):558-564
张占武,黄岗,李怀敏,张文峰.2012.北阿尔金拉配泉地区齐勒萨依岩体的年代学、地球化学特征及其构造意义.岩石矿物学杂志,31(1):13-27
(1)新疆维吾尔自治区地质局.1982.1∶20万巴什考供幅地质图
Bea F,Pereira MD and Stroh A.1994.Mineral/leucosome trace-element partitioning in a peraluminous migmatite(a laser ablation-ICP-MSstudy).Chemical Geology,117(1-4):291-312
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets.Earth and Planetary Science Letters,273(1-2):48-57
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Che ZC,Liu L,Liu HF and Luo JH.1995.Discovery and occurrence of high-pressure metapelitic rocks from Altun Mountain areas,Xinjiang Autonomous Region.Chinese Science Bulletin,40(23):1988-1991
Chen XH,Gehrels G,Wang XF,Yang F and Chen ZL.2003.Granite from North Altyn Tagh,NW China:U-Pb geochronology and tectonic setting.Bulletin of Mineralogy,Petrology and Geochemistry,22(4):294-298(in Chinese with English abstract)
Corfu F,Hanchar JM,Hoskin PWO and Kinny P.2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry,53(1):469-500
Gai YS,Liu L,Kang L,Yang WQ,Liao XY and Wang YW.2015.The origin and geologic significance of plagiogranite in ophiolite belt at North Altyn Tagh.Acta Petrologica Sinica,31(9):2549-2565(in Chinese with English abstract)
Gao XF,Xiao PX,Guo L,Dong ZC and Xi RG.2011.Opening of an Early Paleozoic limited oceanic basin in the northern Altyn area:Constraints from plagiogranites in the Hongliugou-Lapeiquan ophiolitic mélange.Science China(Earth Science),54(12):1871-1879
Gehrels GE,Yin A and Wang XF.2003.Magmatic history of the northeastern Tibetan Plateau.Journal of Geophysical Research:Solid Earth,108(B9):2423
Gorton MP and Schandl ES.2000.From continents to island arcs:Ageochemical index of tectonic setting for arc-related and within-plate felsic to intermediate volcanic rocks.The Canadian Mineralogist,38(5):1065-1073
Han FB,Chen BL,Cui LL,Wang SX,Chen ZL,Jiang RB,Li L and Qi WX.2012.Zircon SHRIMP U-Pb age of intermediate-acid intrusive rocks in Kaladawan area,eastern Altun Mountains,NW China,and its implications.Acta Petrologica Sinica,28(7):2277-2291(in Chinese with English abstract)
Hao J,Wang EQ,Liu XH and Sang HQ.2006.Jinyanshan collisional oroginic belt of the Early Paleozoic in the Altun mountains:Evidence from single zircon U-Pb and40Ar/39Ar isotopic dating for the arc magmatite and ophiolitic mélange.Acta Petrologica Sinica,22(11):2743-2752(in Chinese with English abstract)
Hao RX,Chen BL,Chen ZL,Wang Y,Li SB,Han FB and Zhou YG.2013.Geochemical characteristics of basalts from Kaladawan in East Altun Mountains of Xinjiang and their implications.Acta Geoscientica Sinica,34(3):307-317(in Chinese with English abstract)
Kang L,Liu L,Cao YT,Wang C,Yang WQ and Zhu XH.2011.Geochemistry,zircon LA-ICP-MS U-Pb ages and Hf isotopes of Hongliugou moyite from north Altyn Tagh tectonic belt.Geological Bulletin of China,30(7):1066-1076(in Chinese with English abstract)
Kaygusuz A,Siebel W,爦en C and Satir M.2008.Petrochemistry and petrology of I-type granitoids in an arc setting:The composite Torul pluton,Eastern Pontides,NE Turkey.International Journal of Earth Sciences,97(4):739-764
Koschek G.1993.Origin and significance of the SEMcathodoluminescence from zircon.Journal of Microscopy,171(3):223-232
Li SB.2013.The Early Paleozoic tectonic evolution of Kaladawan area,northern Altyn Taugh.Master Degree Thesis.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Liu L.1999.High pressure metamorphic rocks and ophiolite in Altun,and its tectonic significance.Ph.D.Dissertation.Beijing:Institute of Geology and Geophysics,Chinese Academy of Geological Sciences(in Chinese)
Liu L,Chen DL,Wang C and Zhang CL.2009.New progress on geochronology of high-pressure/ultrahigh-pressure metamorphic rocks from the South Altyn Tagh,the North Qaidam and the North Qinling orogenic,NW China and their geological significance.Journal of Northwest University(Natural Science Edition),39(3):472-479(in Chinese with English abstract)
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.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
Ludwig KR.2003.User’s Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel.Berkeley CA:Berkeley Geochronology Center
Maniar PD and Piccoli PM.1989.Tectonic discrimination of granitoids.Geological Society of America Bulletin,101(5):635-643
Meng LT,Chen BL,Wang Y,Sun Y,Wu Y,Zhang WG and He JT.2016.Timing of Early Paleozoic tectonic regime transition in North Altun:Evidence from granite.Geotectonica et Metallogenia,40(2):295-307(in Chinese with English abstract)
Meng LT,Chen BL,Zhao NN,Wu Y,Zhang WG,He JT,Wang B and Han MM.2017.The distribution,geochronology and geochemistry of Early Paleozoic granitoid plutons in the North Altun orogenic belt,NW China:Implications for the petrogenesis and tectonic evolution.Lithos,268-271:399-417
Niu YL,Zhao ZD,Zhu DC and Mo XX.2013.Continental collision zones are primary sites for net continental crust growth:A testable hypothesis.Earth-Science Reviews,127:96-110
Pati1o Douce AE and Johnston AD.1991.Phase equilibria and melt productivity in the pelitic system:Implications for the origin of peraluminous granitoids and aluminous granulites.Contributions to Mineralogy and Petrology,107(2):202-218
Qi XX,Li HB,Wu CL,Yang JS,Zhang JX,Meng FC,Shi RD and Chen SY.2005a.SHRIMP U-Pb zircon dating for Qiashikansayi granodiorite,the northern Altyn Tagh Mountains and its geological implications.Chinese Science Bulletin,50(5):440-445
Qi XX,Wu CL and Li HB.2005b.SHRIMP U-Pb age of zircons from Kazisayi granite in the northern Alty Tagh Mountains and its significations.Acta Petrologica Sinica,21(3):859-866(in Chinese with English abstract)
Rickwood PC.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Scherer E,Münker C and Mezger K.2001.Calibration of the lutetiumhafnium clock.Science,293(5530):683-687
Sisson TW.1994.Hornblende-melt trace-element partitioning measured by ion microprobe.Chemical Geology,117(1-4):331-344
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Sylvester PJ.1998.Post-collisional strongly peraluminous granites.Lithos,45(1-4):29-44
Taylor SR and Mc Clennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publication,1-132
Wang XL.2017.Some new research progresses and main scientific problems of granitic rocks.Acta Petrologica Sinica,33(5):1445-1458(in Chinese with English abstract)
Wu CL,Yang JS,Yao SZ,Zeng LS,Chen SY,Li HB,Qi XX,Wooden JL and Mazdab FK.2005.Characteristics of the granitoid complex and its zircon SHRIMP dating at the south margin of the Bashikaogong Basin,North Altun,NW China.Acta Petrologica Sinica,21(3):846-858(in Chinese with English abstract)
Wu CL,Yao SZ,Zeng LS,Yang JS,Wooden JL,Chen SY and Mazdab FK.2006.Bashikaogong-Shimierbulake granitic complex,North Altun,NW China:Geochemistry and zircon SHRIMP ages.Science in China(Series D),49(12):1233-1251
Wu CL,Yang JS,Robinson PT,Wooden JL,Mazdab FK,Gao YH,Wu SP and Chen QL.2009.Geochemistry,age and tectonic significance of granitic rocks in north Altun,northwest China.Lithos,113(3-4):423-436
Wu CL,Lei M,Wu D,Zhang X,Chen HJ and Li TX.2016.Zircon U-Pb dating of Paleozoic granites from south Altun and response of the magmatic activity to the tectonic evolution of the Altun Orogenic Belt.Acta Geologica Sinica,90(9):2276-2315(in Chinese with English abstract)
Wu FY,Jahn BM,Wilde SA,Lo CH,Yui TF,Lin Q,Ge WC and Sun DY.2003.Highly fractionated I-type granites in NE China(Ⅰ):Geochronology and petrogenesis.Lithos,66(3-4):241-273
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Wu J,Lan CL,Li JL and Yu LJ.2002.Geochemical evidence of MORBand OIB combination in Hongliugou ophiolite melanges,Altun fault belt.Acta Petrologica et Mineralogica,21(1):24-30(in Chinese with English abstract)
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xu ZQ,Yang JS,Zhang JX,Jiang M,Li HB and Cui JW.1999.Acomparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing.Acta Geologica Sinica,73(3):193-205(in Chinese with English abstract)
Yang JS,Shi RD,Wu CL,Su DC,Chen SY,Wang XB and Wooden J.2008.Petrology and SHRIMP age of the Hongliugou ophiolite at Milan,North Altun,at the northern margin of the Tibetan Plateau.Acta Petrologica Sinica,24(7):1567-1584(in Chinese with English abstract)
Yang WQ,Liu L,Ding HB,Xiao PX,Cao YT and Kang L.2012.Geochemistry,geochronology and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagn and its geological significance.Acta Petrologica Sinica,28(12):4139-4150(in Chinese with English abstract)
Yang ZJ.Early palaeozoic tectonic evolution in Hongliugou,Altyn,Xinjiang.Ph.D.Dissertation.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Yu SY,Zhang JX,Li SZ,Sun DY,Peng YB and Zhao XL.2018.Continuity of the North Qilian and North Altun orogenic belts of NWChina:Evidence from newly discovered Palaeozoic low-Mg and highMg adakitic rocks.Geological Magazine,155(8):1684-1704
Zhang JX,Meng FC,Yu SY,Chen W and Chen SY.2007.39Ar-40Ar geochronology of high-pressure/low-temperature blueschist and eclogite in the North Altyn Tagh and their tectonic implications.Geology in China,34(4):558-564(in Chinese with English abstract)
Zhang ZW,Huang G,Li HM and Zhang WF.2012.LA-ICP-MS zircon U-Pb geochronology and geochemistry of gabbro and diorite from Qilesayi pluton in Lapeiquan area of northern Altun Mountains and their tectonic implications.Acta Petrologica et Mineralogica,31(1):13-27(in Chinese with English abstract)
车自成,刘良,刘洪福,罗金海.1995.阿尔金山地区高压变质泥质岩石的发现及其产出环境.科学通报,40(14):1298-1300
陈宣华,Gehrels G,王小凤,杨风,陈正乐.2003.阿尔金山北缘花岗岩的形成时代及其构造环境探讨.矿物岩石地球化学通报,22(4):294-298
盖永升,刘良,康磊,杨文强,廖小莹,王亚伟.2015.北阿尔金蛇绿混杂岩带中斜长花岗岩的成因及其地质意义.岩石学报,31(9):2549-2565
高晓峰,校培喜,过磊,董增产,奚仁刚.2012.北阿尔金地区早古生代有限洋盆开启时限:来自斜长花岗岩的证据.中国科学(地球科学),42(3):359-368
韩凤彬,陈柏林,崔玲玲,王世新,陈正乐,蒋荣宝,李丽,祁万修.2012.阿尔金山喀腊大湾地区中酸性侵入岩SHRIMP年龄及其意义.岩石学报,28(7):2277-2291
郝杰,王二七,刘小汉,桑海清.2006.阿尔金山脉中金雁山早古生代碰撞造山带:弧岩浆岩的确定与岩体锆石U-Pb和蛇绿混杂岩40Ar/39Ar年代学研究的证据.岩石学报,22(11):2743-2752
郝瑞祥,陈柏林,陈正乐,王永,李松彬,韩凤彬,周永贵.2013.新疆阿尔金山喀腊大湾地区玄武岩的地球化学特征及地质意义.地球学报,34(3):307-317
康磊,刘良,曹玉亭,王超,杨文强,朱小辉.2011.北阿尔金构造带红柳沟钾长花岗岩地球化学特征、LA-ICP-MS锆石U-Pb定年和Hf同位素组成.地质通报,30(7):1066-1076
李松彬.2013.阿尔金北缘喀腊大湾地区早古生代构造演化.硕士学位论文.北京:中国地质科学院
刘良.1999.阿尔金高压变质岩与蛇绿岩及其大地构造意义.博士学位论文.北京:中国科学院地质与地球物理研究所
刘良,陈丹玲,王超,张成立.2009.阿尔金、柴北缘与北秦岭高压-超高压岩石年代学研究进展及其构造地质意义.西北大学学报(自然科学版),39(3):472-479
孟令通,陈柏林,王永,孙岳,吴玉,张文高,何江涛.2016.北阿尔金早古生代构造体制转换的时限:来自花岗岩的证据.大地构造与成矿学,40(2):295-307
戚学祥,李海兵,吴才来,杨经绥,张建新,孟繁聪,史仁灯,陈松永.2005a.北阿尔金恰什坎萨依花岗闪长岩的锆石SHRIMP U-Pb定年及其地质意义.科学通报,50(6):571-576
戚学祥,吴才来,李海兵.2005b.北阿尔金喀孜萨依花岗岩锆石SHRIMP U-Pb定年及其构造意义.岩石学报,21(3):859-866
王孝磊.2017.花岗岩研究的若干新进展与主要科学问题.岩石学报,33(5):1445-1458
吴才来,杨经绥,姚尚志,曾令森,陈松永,李海兵,戚学祥,Wooden JL,Mazdab FK.2005.北阿尔金巴什考供盆地南缘花岗杂岩体特征及锆石SHRIMP定年.岩石学报,21(3):846-858
吴才来,姚尚志,曾令森,杨经绥,Wooden JL,陈松永,Mazdab FK.2007.北阿尔金巴什考供-斯米尔布拉克花岗杂岩特征及锆石SHRIMP U-Pb定年.中国科学(D辑),37(1):10-26
吴才来,雷敏,吴迪,张昕,陈红杰,李天啸.2016.南阿尔金古生代花岗岩U-Pb定年及岩浆活动对造山带构造演化的响应.地质学报,90(9):2276-2315
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
吴峻,兰朝利,李继亮,俞良军.2002.阿尔金红柳沟蛇绿混杂岩中MORB与OIB组合的地球化学证据.岩石矿物学杂志,21(1):24-30
许志琴,杨经绥,张建新,姜枚,李海兵,崔军文.1999.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制.地质学报,73(3):193-205
杨经绥,史仁灯,吴才来,苏德辰,陈松永,王希斌,Wooden J.2008.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年.岩石学报,24(7):1567-1584
杨文强,刘良,丁海波,校培喜,曹玉亭,康磊.2012.南阿尔金迪木那里克花岗岩地球化学、锆石U-Pb年代学与Hf同位素特征及其构造地质意义.岩石学报,28(12):4139-4150
杨子江.2012.新疆阿尔金红柳沟一带早古生代地质构造演化研究.博士学位论文.北京:中国地质科学院
张建新,孟繁聪,于胜尧,陈文,陈松永.2007.北阿尔金HP/LT蓝片岩和榴辉岩的Ar-Ar年代学及其区域构造意义.中国地质,34(4):558-564
张占武,黄岗,李怀敏,张文峰.2012.北阿尔金拉配泉地区齐勒萨依岩体的年代学、地球化学特征及其构造意义.岩石矿物学杂志,31(1):13-27
(1)新疆维吾尔自治区地质局.1982.1∶20万巴什考供幅地质图