阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系:来自泥质和镁铁质麻粒岩的证据
|
摘要
阿尔泰造山带是中亚造山带(CAOB)的重要组成部分,在其南缘出露有高温泥质和镁铁质麻粒岩,确定其P-T轨迹对于理解阿尔泰造山带南缘在晚古生代的构造演化历史具有重要意义。通过对该区乌恰沟泥质和镁铁质麻粒岩样品精细的岩相学观察,显示其变质矿物组合分别为石榴石+堇青石+黑云母+斜长石+石英+磁铁矿+钛铁矿±斜方辉石±尖晶石±钾长石,斜方辉石+单斜辉石+角闪石+黑云母+斜长石+钾长石+石英+钛铁矿+磁铁矿。使用传统温压计和平均温压计算方法对其变质峰期及峰期后的P-T条件进行了计算,并利用Thermocalc软件对其中两个泥质麻粒岩进行了P-T视剖面图模拟,确定了其峰期变质条件为770~865℃和3.0~5.1kbar,并得到了两条峰期后近等压冷却(IBC)的P-T演化轨迹。这样近等压冷却的P-T轨迹表明高温变质作用可能发生于一个总体伸展的大地构造背景之下。已有年代学数据支持该区高温变质事件发生于二叠纪(270~280Ma),与塔里木地幔柱活动的时间(~275Ma)高度一致。这说明阿尔泰二叠纪高温变质事件可能与塔里木地幔柱有着密切的成因联系。因此,我们认为二叠纪地幔柱活动引起的幔源岩浆底侵和加热可能提供了阿尔泰南缘高温-超高温变质作用所需的热源。
The Altay orogen is an important part of the Central Asian Orogenic Belt( CAOB),and several high-temperature metapelitic and mafic granulites occur on its southern margin. Constructing their P-T paths is of great significance to understand the Late Paleozoic tectonic evolution history of the southern Chinese Altay. Detailed petrographic observations on the metapelitic and mafic granulites at Wuqiagou area show that their metamorphic assemblages are garnet + cordierite + biotite + plagioclase + quartz + magnetite+ ilmenite ± orthopyroxene ± spinel ± k-feldspar and orthopyroxene + clinopyroxene + biotite + plagioclase + k-feldspar + amphibole +magnetite + ilmenite + quartz,respectively. Peak and post-peak metamorphic P-T conditions are estimated using conventional thermobarometers and average P-T approach. P-T pseudosections are calculated for two metapelitic granulites via the Thermocalc program,yielding peak metamorphic P-T conditions of 770 ~ 865℃ /3. 0 ~ 5. 1kbar and two post-peak near-isobaric cooling( IBC) P-T paths. Such IBC P-T paths suggest that high-temperature metamorphism likely occurred in an overall extensional tectonic setting. The available age results support that the high-temperature metamorphism in the region occurred in the Permian( 270 ~ 280Ma) which is coeval with the time of the Tarim mantle plume activity( ~ 275Ma). This indicates that the Altay Permian high-temperature metamorphism is likely associated tightly with the Permian Tarim mantle plume activity. We consider that the heat source necessary for the Permian high-temperature metamorphism in the southern Altay was most probably provided by underplating and heating of mantlederived mafic magma as a result of the Tarim mantle plume.
The Altay orogen is an important part of the Central Asian Orogenic Belt( CAOB),and several high-temperature metapelitic and mafic granulites occur on its southern margin. Constructing their P-T paths is of great significance to understand the Late Paleozoic tectonic evolution history of the southern Chinese Altay. Detailed petrographic observations on the metapelitic and mafic granulites at Wuqiagou area show that their metamorphic assemblages are garnet + cordierite + biotite + plagioclase + quartz + magnetite+ ilmenite ± orthopyroxene ± spinel ± k-feldspar and orthopyroxene + clinopyroxene + biotite + plagioclase + k-feldspar + amphibole +magnetite + ilmenite + quartz,respectively. Peak and post-peak metamorphic P-T conditions are estimated using conventional thermobarometers and average P-T approach. P-T pseudosections are calculated for two metapelitic granulites via the Thermocalc program,yielding peak metamorphic P-T conditions of 770 ~ 865℃ /3. 0 ~ 5. 1kbar and two post-peak near-isobaric cooling( IBC) P-T paths. Such IBC P-T paths suggest that high-temperature metamorphism likely occurred in an overall extensional tectonic setting. The available age results support that the high-temperature metamorphism in the region occurred in the Permian( 270 ~ 280Ma) which is coeval with the time of the Tarim mantle plume activity( ~ 275Ma). This indicates that the Altay Permian high-temperature metamorphism is likely associated tightly with the Permian Tarim mantle plume activity. We consider that the heat source necessary for the Permian high-temperature metamorphism in the southern Altay was most probably provided by underplating and heating of mantlederived mafic magma as a result of the Tarim mantle plume.
引文
Anderson LJ and Smith RD.1995.The effects of temperature and fOon2the Al-in-hornblende barometer.American Mineralogist,80(5-6):549-559
Bindu RS.1997.Granulite facies spine-cordierite assemblages from theKerala Khondalite Belt,Southern India.Gondwana Research,1(1):121-128
Brey GP and Khler TP.1990.Geothermobarometry in four-phaselherzolites:II.New thermobarometers and practical assessment ofexisting thermobarometers.Journal of Petrology,31(6):1353-1378
Briggs SM,Yin A,Manning CE,Chen ZL,Wang XF and Grove M.2007.Late Paleozoic tectonic evolution history of the Ertix Fault inthe Chinese Altay and its implications for the development of theCentral Asian Orogenic System.Geological Society of AmericaBulletin,119(7-8):944-960
Chen H,Li Z,Yang S,Dong C,Xiao W and Tainosho Y.2006.Mineralogical and geochemical study of a newly discovered maficgranulite,Northwest China:Implications for tectonic evolution of theAltay orogenic belt.Island Arc,15(1):210-222
Chen HL,Yang SF,Li ZL,Yu X,Xiao WJ,Yuan C,Lin XB and LiJL.2006.Zircon SHRIMP U-Pb chronology of the Fuyun basicgranulite and its tectonic significance in the Altaid orogenic belt.Acta Petrologica Sinica,22(5):1351-1358(in Chinese withEnglish abstract)
Chen LH and Han BF.2006.Geochronology,geochemistry and Sr-Nd-Pbisotopic composition of mafic intrusive rocks in Wuqiagou area,NorthXinjiang:Constraints for mantle sources and deep processes.ActaPetrologica Sinica,22(5):1201-1214(in Chinese with Englishabstract)
Gerya TV,Perchuk LL,Triboulet C,Audren C and Sez’ko AI.1997.Petrology of the Tumanshet zonal metamorphic complex,easternSayan.Petrology,5(6):503-533
Gong HL,Chen ZL,Hu YQ,Li L,Lai XR,Ma QY,Li YY,Hu B andZhang WG.2007.Geochemical characteristics of acidic dike swarmfrom the eastern segment of the Ertix tectonic belt,Altai orogen andits geological implications.Acta Petrologica Sinica,23(5):889-899(in Chinese with English abstract)
Guo JH,Peng P,Chen Y,Jiao SJ and Windley BF.2012.UHTsapphirine granulite metamorphism at 1.93~1.92Ga caused bygabbronorite intrusions:Implications for tectonic evolution of thenorthern margin of the North China Craton.Precambrian Research,222-223:124-142
Han BF,He GQ and Wang SG.1999.Postcollisional mantle-derivedmagmatism,underplating and implications for basement of theJunggar Basin.Science in China(Series D),42(2):113-119
Han BF,Ji JQ,Song B,Chen LH and Li ZH.2004.SHRIMP zircon UPb ages of Kalatongke No.1 and Huangshandong Cu-Ni bearingmafic-ultramafic complexes,North Xinjiang,and geologicalimplications.Chinese Science Bulletin,49(22):2424-2429
Han BF,Guo ZJ,Zhang ZC,Zhang L,Chen JF and Song B.2010.Age,geochemistry,and tectonic implications of a Late Paleozoicstitching pluton in the North Tian Shan suture zone,western China.Geological Society of America Bulletin,122(3-4):627-640
Harley SL.1989.The origins of granulites:A metamorphic perspective.Geological Magazine,126(3):215-247
Holland TJB and Powell R.1998.An internally consistent thermodynamicdata set for phases of petrological interest.Journal of MetamorphicGeology,16(3):309-343
Holland TJB and Powell R.2003.Activity-composition relations forphases in petrological calculations:An asymmetric multi-componentformulation.Contributions to Mineralogy and Petrology,145(4):492-501
Hollister LS,Grissom GC,Peters EK,Stowell HH and Sisson VB.1987.Confirmation of the empirical correlation of Al in hornblende withpressure of solidification of calc-alkaline plutons.AmericanMineralogist,72(3-4):231-239
Hu AQ,Jahn BM,Zhang GX,Chen YB and Zhang QF.2000.Crustalevolution and Phanerozoic crustal growth in northern Xinjiang:Nd-Srisotopic evidence.Part I:Isotopic characterization of basementrocks.Tectonophysics,328(1-2):15-51
Hu AQ,Zhang GX,Zhang QF,Li TD and Zhang JB.2002.A review onages of precambrian metamorphic rocks from Altai orogeny inXinjiang,NW China.Chinese Journal of Geology,37(2):129-142(in Chinese with English abstract)
Hu AQ,Wei GJ,Deng WF and Chen LL.2006.SHRIMP zircon U-Pbdating and its significance for gneisses from the southwest area toQinghe County in the Altai,China.Acta Petrologica Sinica,22(1):1-10(in Chinese with English abstract)
Jahn BM.2004.The Central Asian Orogenic Belt and growth of thecontinental crust in the Phanerozoic.In:Malpas J,Fletcher CJN,Ali JR and Aitchison JC(eds.).Aspects of the Tectonic Evolutionof China.Geological Society London,Special Publications,226(1):73-100
Jiang YD,Sun M,Zhao GC,Yuan C,Xiao WJ,Xia XP,Long XP andWu FY.2010.The~390Ma high-T metamorphic event in theChinese Altai:A consequence of ridge-subductionAmericanJournal of Science,310(10):1421-1452
Johnson MC and Rutherford MJ.1989.Experimental calibration of thealuminum-in-hornblende geobarometer with application to LongValley caldera(California)volcanic rocks.Geology,17(9):837-841
Laurent-Charvet S,Charvet J,MoniéP and Shu L.2003.Late Paleozoicstrike-slip shear zones in eastern central Asia(NW China):Newstructural and geochronological data.Tectonics,22(2):237-241
Li HJ,He GQ,Wu TR and Wu B.2006.Confirmation of Altai-Mongoliamicrocontinent and its implications.Acta Petrologica Sinica,22(5):1369-1379(in Chinese with English abstract)
Li JH,Xiao WJ,Wang K,Sun G and Gao L.2003.Tectonic andmetallogenic evolution of the Altay Shan,Northern Xinjiang UygurAutonomous Region,northwestern China.In:Goldfarb RJ,MaoJW,Hart C,Wang D,Anderson E,Wang Z(eds.).TectonicEvolution and Metallogeny of the Chinese Altay and Tianshan.Beijing:CERCAMS,31-74
Li TD,Qi ZM,Wu BQ,Xiao SL,Zhao CL,Poliyangsiji BH et al.1996.New improvement of comparative study of geology andmineralization of Altay between China and Kazakhstan.In:ChineseGeological Society(ed.).Thesis Volume of the Symposium of the8thFive-year Plan of Geoscience for Contribution to 30thIGC.Beijing:Metallurgical Industrial Publishing House,256-259(inChinese)
Li ZL,Chen HL,Yang SF,Dong CW and Xiao WJ.2004.Petrology,geochemistry and geodynamics of basic granulite from the Altay area,North Xinjiang,China.Journal of Zhejiang University Science,5(8):979-984
Li ZL,Chen HL,Yang SF,Xiao WJ and Tainosho Y.2004.Discoveryof the basic granulite from the Altai area:Evidence from mineralogy.Acta Petrologica Sinica,20(6):1445-1455(in Chinese withEnglish abstract)
Li ZL,Li YQ,Chen HL,Santosh M,Xiao WJ and Wang HH.2010.SHRIMP U-Pb zircon chronology of ultrahigh-temperature spinelorthopyroxene-garnet granulite from south Altay orogenic belt,northwestern China.Island Arc,19(3):506-516
Li ZL,Yang XQ,Li YQ,Santosh M,Chen HL and Xiao WJ.2014.Late Paleozoic tectono-metamorphic evolution of the Altai segment ofthe Central Asian Orogenic Belt:Constraints from metamorphic P-Tpseudosection and zircon U-Pb dating of ultra-high-temperaturegranulite.Lithos,204:83-96
Long XP,Sun M,Yuan C,Xiao WJ,Lin SF,Wu FY,Xia XP and CaiKD.2007.Detrital zircon age and Hf isotopic studies formetasedimentary rocks from the Chinese Altai:Implications for theearly Paleozoic tectonic evolution of the Central Asian Orogenic Belt.Tectonics,26(5):TC5015,doi:10.1029/2007TC002128
Long XP,Yuan C,Sun M,Xiao WJ,Lin SF,Wang YJ and Cai KD.2008.Geochemiscal characteristics and sedimentary environments ofDevonina low metamorphic clastic sedimentary rocks in the southernmargin of the Chinese Altai,North Xinjiang.Acta PetrologicaSinica,24(4):718-732(in Chinese with English abstract)
Newton R and Perkins D.1982.Thermodynamic calibration ofgeobarometers based on the assemblages garnet-plagioclaseorthopyroxene(clinopyroxene)-quartz.American Mineralogist,67(3-4):203-222
Pattison DRM,Chacko T,Farquhar J and McF arlane CRM.2003.Temperatures of granulite-facies metamorphism:Constraints fromexperimental phase equilibria and thermobarometry corrected forretrograde exchange.Journal of Petrology,44(5):867-900
Perchuk LL and Lavrentpeva IV.1983.Experimental investigation ofexchange equilibria in the system cordierite-garnet-biotite.In:Saxena SK(ed.).Kinetics and Equilibrium in Mineral Reactions.New York,Berlin,Heidelberg:Springer-Verlag,199-239
Perkins D III and Chipera SJ.1985.Garnet-orthopyroxene-plagioclasequartz barometry:Refinement and application to the English Riversubprovince and the Minnesota River valley.Contributions toMineralogy and Petrology,89(1):69-80
Pirajno F,Mao JW,Zhang ZC,Zhang ZH and Chai FM.2008.Theassociation of mafic-ultramafic intrusions and A-type magmatism inthe Tian Shan and Altay orogens,NW China:Implications forgeodynamic evolution and potential for the discovery of new oredeposits.Journal of Asian Earth Sciences,32(2-4):165-183
Powell R and Holland T.1994.Optimal geothermometry andgeobarometry.American Mineralogist,79(1-2):120-133
Powell R,Holland TJB and Worley B.1998.Calculating phase diagraminvolving solid solutions via no-linear equations,with examples usingTHERMOCALC.Journal of Metamorphic Geology,16(4):577-586
Powell R and Holland T.1999.Relating formulations of thethermodynamics of mineral solid solutions:Activity modeling ofpyroxenes,amphiboles,and micas.American Mineralogist,84(1-2):1-14
爦engr AMC,Natal’in BA and Burtman VS.1993.Evolution of theAltaid tectonic collage and Palaeozoic crustal growth in Eurasia.Nature,364(6435):299-307
Shen XM,Zhang HX and Ma L.2013.LA-ICP-MS zircon U-Pb datingfor Jieerkuduke acidic dykes in the southern Altay range.XinjiangGeology,31(3):157-161(in Chinese with English abstract)
Sun M,Long XP,Cai KD,Jiang YD,Wang BY,Yuan C,Zhao GC,Xiao WJ and Wu FY.2009.Early Palaeozoic ridge subduction inthe Chinese Altai:Insight from the abrupt change in zircon Hfisotopic compositions.Science in China(Series D),39(7):935-948(in Chinese)
Tang GJ,Wang Q,Wyman DA,Li ZX,Zhao ZH and Yang YH.2012.Late Carboniferous highεNd(t)-εHf(t)granitoids,enclaves anddikes in western Junggar,NW China:Ridge-subduction-relatedmagmatism and crustal growth.Lithos,140(5):86-102
Tong LX,Chen YB,Xu YG and Liu WP.2011.Occurrence of bearingOpx+Sil high-temperature pelitic granulite and its geologicalsignificance.Xi’an:Abstract of 2011’s National Symposium onPetrology and Geodynamics,214(in Chinese)
Tong LX,Chen YB,Xu YG,Zhou X and Liu Z.2013.Zircon U-Pbages of the ultrahigh-temperature metapelitic granulite from the Altaiorogen,NW China,and geological implications.Acta PetrologicaSinica,29(10):3435-3445(in Chinese with English abstract)
Tong L,Chen Y and Chen L.2014a.Confirmation of ultrahightemperature metapelitic granulite in the Altay orogen and itsgeological significance.Chinese Science Bulletin,59(27):3441-3448
Tong L,Xu YG,Cawood PA,Zhou X,Chen YB and Liu Z.2014b.Anticlockwise P-T evolution at~280Ma recorded from Opx-Silbearing metapelitic granulite in the Chinese Altai orogen,possiblelink with the Tarim mantle plumeJournal of Asian Earth Sciences,94:1-11
Tong Y,Wang T,Hong DW and Han BF.2006.Pb isotopic compositionof granitoids from the Altay orogen(China):Evidence for Mantlederived origin and continental growth.Acta Geologica Sinica,80(4):517-528(in Chinese with English abstract)
Wang T,Hong DW,Tong Y,Han BF and Shi YR.2005.Zircon U-PbSHRIMP age and origin of post-orogenic Lamazhao granitic plutonfrom Altai orogen:Its implications for vertical continental growth.Acta Petrologica Sinica,21(3):640-650(in Chinese withEnglish abstract)
Wang T,Hong DW,Jahn BM,Tong Y,Wang YB,Han BF and WangXX.2006.Timing,petrogenesis,and setting of Paleozoicsynorogenic intrusions from the Altai Mountains,Northwest China:Implications for the tectonic evolution of an accretionary orogen.Journal of Geology,114(6):735-751
Wang T,Jahn BM,Kovach VP,Tong Y,Hong DW and Han BF.2009a.Nd-Sr isotopic mapping of the Chinese Altai and implicationsfor continental growth in the central Asian orogenic Belt.Lithos,110(1-4):359-372
Wang W,Wei CJ,Wang T,Lou YX and Chu H.2009b.Confirmation ofpelitic granulite in the Altai orogen and its geological significance.Chinese Science Bulletin,54(14):2543-2548
Wang W,Wei CJ,Zhang YH,Chu H,Zhao Y and Liu XC.2014.Ageand origin of sillimanite schist from the Chinese Altai metamorphicbelt:Implications for Late Palaeozoic tectonic evolution of the CentralAsian Orogenic Belt.International Geology Review,56(2):224-236
Wei CJ,Powell R and Clarke GL.2004.Calculated phase equilibria forlow-and medium-pressure metapelites in the KFMASH andKMn FMASH systems.Journal of Metamorphic Geology,22(5):495-508
Wei CJ,Clarke G,Tian W and Qiu L.2007.Transition of metamorphicseries from the kyanite-to andalusite-types in the Altai orogen,Xinjiang,China:Evidence from petrography and calculatedKMn FMASH and KFMASH phase relations.Lithos,96(3-4):353-374
Wells PRA.1977.Pyroxene thermometry in the simple and complexsystems.Contributions to Mineralogy and Petrology,62(2):129-139
White RW,Powell R,Holland TJB and Worley BA.2000.The effect ofTiO 2and Fe2O3on metapelitic assemblages at greenschist andamphibolite facies conditions:Mineral equilibria calculations in thesystem K2O-FeO-MgO-Al2O3-SiO 2-H2O-TiO 2-Fe2O3.Journal ofMetamorphic Geology,18(5):497-511
White RW,Powell R and Clarke GL.2002.The interpretation of reactiontextures in Fe-rich metapelitic granulites of the Musgrave Block,central Australia:Constraints from mineral equilibria calculations inthe system K2O-FeO-MgO-Al2O3-SiO 2-H2O-TiO 2-Fe2O3.Journalof Metamorphic Geology,20(1):41-55
White RW,Powell R and Holland TJB.2007.Progress relating tocalculation of partial melting equilibria for metapelites.Journal ofMetamorphic Geology,25(5):511-527
Windley BF,Krner A,Guo JH,Qu GS,Li YY and Zhang C.2002.Neoproterozoic to Paleozoic geology of the Altai orogen,NW China:New zircon age data and tectonic evolution.Journal of Geology,110(6):719-737
Wood BJ and Banno S.1973.Garnet-orthopyoxene and orthopyroxeneclinopyroxene relationship in simple and complex system.Contrib.Mineral.Petrol.42(2):109-124
Wu CM,Pan YS and Wang KY.1999.Refinement of the biotiteorthopyroxene geothermometer with applications.Acta PetrologicaSinica,15(3):463-468(in Chinese with English abstract)
Wu CM,Zhang J and Ren LD.2004.Empirical garnet-biotite-plagiocl ase-quartz(GBPQ)geobarometry in medium-to high-grademetapelites.Journal of Petrology,45(9):1907-1921
Xiao W,Windley BF,Badarch G,Sun S,Li J,Qin K and Wang Z.2004.Palaeozoic accretion and convergent tectonics of the southernAltaids:Implications for the growth of Central Asia.Journal of theGeological Society,161(3):339-342
Xiao WJ,Han CM,Yuan C,Chen HL,Sun M,Lin SF,Li ZL and MaoQG.2006.Unique Carboniferous-Permian tectonic-metallogenicframework of northern Xinjiang(NW China):Constraints for thetectonics of the southern Paleoasian domain.Acta Petrologica Sinica,22(5):1062-1076(in Chinese with English abstract)
Xiao WJ,Han CM,Yuan C,Sun M,Lin SF,Chen HL,Li ZL,Li JLand Sun S.2008.Middle Cambrian to Permian subduction-relatedaccretionary orogenesis of northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia.Journal ofAsian Earth Sciences,32(2-4):102-117
Xu XC,Zheng CQ and Zhao QY.2005.Metamorphic types and crustalevolution of Hercynian orogenic belt in Altai region,Xinjiang.Journal of Jilin University(Earth Science Edition),35(1):7-11(in Chinese with English abstract)
Zhai MG and Liu WJ.2001.The formation of granulite and itscontribution to evolution of the continental crust.Acta PetrologicaSinica,17(1):28-38(in Chinese with English abstract)
Zhang CG,Wei CJ and Qiu L.2004.Evolution of metamorphism and itsgeologic significance in Altaids,Xinjiang.Xinjiang Geology,22(1):16-23(in Chinese with English abstract)
Zhang CL,Li ZX,Li XH,Xu YG,Zhou G and Ye HM.2010.APermian large igneous province in Tarim and Central Aisian orogenicbelt,NW China:Results of a ca.275Ma mantle plumeGeologicalSociety of America Bulletin,122(11-12):2020-2040
Zhang CL,Santosh M,Zou HB,Xu YG,Zhou G,Dong YG,Ding RFand Wang HY.2012.Revisiting the“Irtish tectonic belt”:Implications for the Palaeozoic tectonic evolution of the Altai orogen.Journal of Asian Earth Science,52:117-133
Zheng CQ,Xu XC,Enami M and Kato T.2005.Monazite ages andgeological implications of andalusite-sillimanite type metamorphicbelt in Aletai,Xinjiang.Global Geology,24(3):236-242(inChinese with English abstract)
Zheng CQ,Kato T,Enami M and Xu XC.2007.CHIME monazite agesof metasediments from the Altai orogen in northwestern China:Devonian and Permian ages of metamorphism and their significance.Island Arc,16(4):598-604
Zheng CQ,Xu XC,Kato T and Enami M.2007.Permian CHIME ages ofmonazites for the kyanite-sillimanite type metamorphic belt inChonghuer area,Altai,Xinjiang and their geological implications.Geological Journal of China University,13(3):566-573(inChinese with English abstract)
Zhuang YX.1994.The PTSt evolution of metamorphism and developmentmechanism of the thermal-structural-gneiss domes in the ChineseAltaides.Acta Geologica Sinica,68(1):35-47(in Chinese withEnglish abstract)
Zou TR,Cao HZ and Wu BQ.1988.Orogenic and anorogenic granitoidsof the Altay Mountains,Xinjiang and their discrimination criteria.Acta Geologica Sinica,62(3):228-243(in Chinese with Englishabstract)
陈汉林,杨树锋,厉子龙,余兴,肖文交,袁超,林秀斌,李继亮.2006.阿尔泰造山带富蕴基性麻粒岩锆石SHRIMP U-Pb年代学及其构造意义.岩石学报,22(5):1351-1358
陈立辉,韩宝福.2006.新疆北部乌恰沟地区镁铁质侵入岩的年代学地球化学和同位素组成:对地幔源区特征和深部过程的约束.岩石学报,22(5):1201-1214
宫红良,陈正乐,胡远清,李丽,赖新荣,马庆佑,李玉英,胡博,张文贵.2007.阿尔泰额尔齐斯带东段酸性岩墙群地球化学特征及其地质意义.岩石学报,23(5):889-899
胡霭琴,张国新,张前锋,李天德,张积斌.2002.阿尔泰造山带变质岩系时代问题的讨论.地质科学,37(2):129-142
胡霭琴,韦刚健,邓文峰,陈林丽.2006.阿尔泰地区青河县西南片麻岩中锆石SHRIMP U-Pb定年及其地质意义.岩石学报,22(1):1-10
李会军,何国琦,吴泰然,吴波.2006.阿尔泰-蒙古微大陆的确定及其意义.岩石学报,22(5):1369-1379
李天德,祁志明,吴柏青,肖世禄,赵昌龙,别斯帕耶夫XA,波利杨斯基HB,季亚契科夫BA,甘任科ГД,叶夫图申科НП,叶夫图申科ОП.1996.中国和哈萨克斯坦阿尔泰地质及成矿研究的新进展.见:中国地质学会编.献给三十届国际地质大会“八五”地质科技重要成果学术交流会议论文选集.北京:冶金工业出版社,256-259
厉子龙,陈汉林,杨树锋,肖文交,Tainosho Y.2004.阿尔泰基性麻粒岩的发现:来自矿物学的证据.岩石学报,20(6):1445-1455
龙晓平,袁超,孙敏,肖文交,林寿发,王毓靖,蔡克大.2008.北疆阿尔泰南缘泥盆系浅变质碎屑沉积岩地球化学特征及其形成环境.岩石学报,24(4):718-732
沈晓明,张海祥,马林.2013.阿尔泰南缘杰尔库都克酸性岩脉LAICP-MS锆石U-Pb测年.新疆地质,31(3):157-161
孙敏,龙晓平,蔡克大,蒋映德,王步云,袁超,赵国春,肖文交,吴福元.2009.阿尔泰早古生代末期洋中脊俯冲:锆石Hf同位素组成突变的启示.中国科学(D辑),39(7):935-948
仝来喜,陈义兵,徐义刚,刘文平.2011.阿尔泰造山带含Opx+Sil高温变泥质麻粒岩的产出及其地质意义.西安:2011年全国岩石学与地球动力学研讨会论文摘要(上册),214
仝来喜,陈义兵,徐义刚,周信,刘兆.2013.阿尔泰超高温变泥质麻粒岩的锆石U-Pb年龄及其地质意义.岩石学报,29(10):3435-3445
童英,王涛,洪大卫,韩宝福.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征:幔源成因佐证及陆壳生长意义.地质学报,80(4):517-528
王涛,洪大伟,童英,韩宝福,石玉若.2005.中国阿尔泰造山带后造山喇嘛昭花岗岩体锆石SHRIMP年龄-成因及陆壳垂向生长意义.岩石学报,21(3):640-650
吴春明,潘裕生,王凯怡.1999.黑云母-斜方辉石温度计的重新标度及其应用.岩石学报,15(3):463-468
肖文交,韩春明,袁超,陈汉林,孙敏,林寿发,厉子龙,毛启贵,张继恩,孙枢,李继亮.2006.新疆北部石炭纪-二叠纪独特的构造成矿作用:对古亚洲洋构造域南部大地构造演化的制约.岩石学报,22(5):1062-1076
徐学纯,郑常青,赵庆英.2005.阿尔泰海西造山带区域变质作用类型与地壳演化.吉林大学学报(地球科学版),35(1):7-11
翟明国,刘文军.2001.麻粒岩的形成及其对大陆地壳演化的贡献.岩石学报,17(1):28-38
张翠光,魏春景,邱林.2004.新疆阿尔泰造山带变质作用演化及其地质意义.新疆地质,22(1):16-23
郑常青,徐学纯,Enami M,Kato T.2005.新疆阿尔泰红柱石-夕线石型变质带的独居石年龄及其地质意义.世界地质,24(3):236-242
郑常青,徐学纯,Kato T,Enami M.2007.新疆阿尔泰冲乎尔地区蓝晶石-夕线石型变质带独居石CHIME二叠纪年龄及其地质意义.高校地质学报,13(3):566-573
庄育勋.1994.中国阿尔泰造山带变质作用PTSt演化和热-构造-片麻岩穹窿形成机制.地质学报,68(1):35-47
邹天人,曹惠志,吴柏青.1988.新疆阿尔泰造山花岗岩和非造山花岗岩及其判别标志.地质学报,62(3):228-243
Bindu RS.1997.Granulite facies spine-cordierite assemblages from theKerala Khondalite Belt,Southern India.Gondwana Research,1(1):121-128
Brey GP and Khler TP.1990.Geothermobarometry in four-phaselherzolites:II.New thermobarometers and practical assessment ofexisting thermobarometers.Journal of Petrology,31(6):1353-1378
Briggs SM,Yin A,Manning CE,Chen ZL,Wang XF and Grove M.2007.Late Paleozoic tectonic evolution history of the Ertix Fault inthe Chinese Altay and its implications for the development of theCentral Asian Orogenic System.Geological Society of AmericaBulletin,119(7-8):944-960
Chen H,Li Z,Yang S,Dong C,Xiao W and Tainosho Y.2006.Mineralogical and geochemical study of a newly discovered maficgranulite,Northwest China:Implications for tectonic evolution of theAltay orogenic belt.Island Arc,15(1):210-222
Chen HL,Yang SF,Li ZL,Yu X,Xiao WJ,Yuan C,Lin XB and LiJL.2006.Zircon SHRIMP U-Pb chronology of the Fuyun basicgranulite and its tectonic significance in the Altaid orogenic belt.Acta Petrologica Sinica,22(5):1351-1358(in Chinese withEnglish abstract)
Chen LH and Han BF.2006.Geochronology,geochemistry and Sr-Nd-Pbisotopic composition of mafic intrusive rocks in Wuqiagou area,NorthXinjiang:Constraints for mantle sources and deep processes.ActaPetrologica Sinica,22(5):1201-1214(in Chinese with Englishabstract)
Gerya TV,Perchuk LL,Triboulet C,Audren C and Sez’ko AI.1997.Petrology of the Tumanshet zonal metamorphic complex,easternSayan.Petrology,5(6):503-533
Gong HL,Chen ZL,Hu YQ,Li L,Lai XR,Ma QY,Li YY,Hu B andZhang WG.2007.Geochemical characteristics of acidic dike swarmfrom the eastern segment of the Ertix tectonic belt,Altai orogen andits geological implications.Acta Petrologica Sinica,23(5):889-899(in Chinese with English abstract)
Guo JH,Peng P,Chen Y,Jiao SJ and Windley BF.2012.UHTsapphirine granulite metamorphism at 1.93~1.92Ga caused bygabbronorite intrusions:Implications for tectonic evolution of thenorthern margin of the North China Craton.Precambrian Research,222-223:124-142
Han BF,He GQ and Wang SG.1999.Postcollisional mantle-derivedmagmatism,underplating and implications for basement of theJunggar Basin.Science in China(Series D),42(2):113-119
Han BF,Ji JQ,Song B,Chen LH and Li ZH.2004.SHRIMP zircon UPb ages of Kalatongke No.1 and Huangshandong Cu-Ni bearingmafic-ultramafic complexes,North Xinjiang,and geologicalimplications.Chinese Science Bulletin,49(22):2424-2429
Han BF,Guo ZJ,Zhang ZC,Zhang L,Chen JF and Song B.2010.Age,geochemistry,and tectonic implications of a Late Paleozoicstitching pluton in the North Tian Shan suture zone,western China.Geological Society of America Bulletin,122(3-4):627-640
Harley SL.1989.The origins of granulites:A metamorphic perspective.Geological Magazine,126(3):215-247
Holland TJB and Powell R.1998.An internally consistent thermodynamicdata set for phases of petrological interest.Journal of MetamorphicGeology,16(3):309-343
Holland TJB and Powell R.2003.Activity-composition relations forphases in petrological calculations:An asymmetric multi-componentformulation.Contributions to Mineralogy and Petrology,145(4):492-501
Hollister LS,Grissom GC,Peters EK,Stowell HH and Sisson VB.1987.Confirmation of the empirical correlation of Al in hornblende withpressure of solidification of calc-alkaline plutons.AmericanMineralogist,72(3-4):231-239
Hu AQ,Jahn BM,Zhang GX,Chen YB and Zhang QF.2000.Crustalevolution and Phanerozoic crustal growth in northern Xinjiang:Nd-Srisotopic evidence.Part I:Isotopic characterization of basementrocks.Tectonophysics,328(1-2):15-51
Hu AQ,Zhang GX,Zhang QF,Li TD and Zhang JB.2002.A review onages of precambrian metamorphic rocks from Altai orogeny inXinjiang,NW China.Chinese Journal of Geology,37(2):129-142(in Chinese with English abstract)
Hu AQ,Wei GJ,Deng WF and Chen LL.2006.SHRIMP zircon U-Pbdating and its significance for gneisses from the southwest area toQinghe County in the Altai,China.Acta Petrologica Sinica,22(1):1-10(in Chinese with English abstract)
Jahn BM.2004.The Central Asian Orogenic Belt and growth of thecontinental crust in the Phanerozoic.In:Malpas J,Fletcher CJN,Ali JR and Aitchison JC(eds.).Aspects of the Tectonic Evolutionof China.Geological Society London,Special Publications,226(1):73-100
Jiang YD,Sun M,Zhao GC,Yuan C,Xiao WJ,Xia XP,Long XP andWu FY.2010.The~390Ma high-T metamorphic event in theChinese Altai:A consequence of ridge-subductionAmericanJournal of Science,310(10):1421-1452
Johnson MC and Rutherford MJ.1989.Experimental calibration of thealuminum-in-hornblende geobarometer with application to LongValley caldera(California)volcanic rocks.Geology,17(9):837-841
Laurent-Charvet S,Charvet J,MoniéP and Shu L.2003.Late Paleozoicstrike-slip shear zones in eastern central Asia(NW China):Newstructural and geochronological data.Tectonics,22(2):237-241
Li HJ,He GQ,Wu TR and Wu B.2006.Confirmation of Altai-Mongoliamicrocontinent and its implications.Acta Petrologica Sinica,22(5):1369-1379(in Chinese with English abstract)
Li JH,Xiao WJ,Wang K,Sun G and Gao L.2003.Tectonic andmetallogenic evolution of the Altay Shan,Northern Xinjiang UygurAutonomous Region,northwestern China.In:Goldfarb RJ,MaoJW,Hart C,Wang D,Anderson E,Wang Z(eds.).TectonicEvolution and Metallogeny of the Chinese Altay and Tianshan.Beijing:CERCAMS,31-74
Li TD,Qi ZM,Wu BQ,Xiao SL,Zhao CL,Poliyangsiji BH et al.1996.New improvement of comparative study of geology andmineralization of Altay between China and Kazakhstan.In:ChineseGeological Society(ed.).Thesis Volume of the Symposium of the8thFive-year Plan of Geoscience for Contribution to 30thIGC.Beijing:Metallurgical Industrial Publishing House,256-259(inChinese)
Li ZL,Chen HL,Yang SF,Dong CW and Xiao WJ.2004.Petrology,geochemistry and geodynamics of basic granulite from the Altay area,North Xinjiang,China.Journal of Zhejiang University Science,5(8):979-984
Li ZL,Chen HL,Yang SF,Xiao WJ and Tainosho Y.2004.Discoveryof the basic granulite from the Altai area:Evidence from mineralogy.Acta Petrologica Sinica,20(6):1445-1455(in Chinese withEnglish abstract)
Li ZL,Li YQ,Chen HL,Santosh M,Xiao WJ and Wang HH.2010.SHRIMP U-Pb zircon chronology of ultrahigh-temperature spinelorthopyroxene-garnet granulite from south Altay orogenic belt,northwestern China.Island Arc,19(3):506-516
Li ZL,Yang XQ,Li YQ,Santosh M,Chen HL and Xiao WJ.2014.Late Paleozoic tectono-metamorphic evolution of the Altai segment ofthe Central Asian Orogenic Belt:Constraints from metamorphic P-Tpseudosection and zircon U-Pb dating of ultra-high-temperaturegranulite.Lithos,204:83-96
Long XP,Sun M,Yuan C,Xiao WJ,Lin SF,Wu FY,Xia XP and CaiKD.2007.Detrital zircon age and Hf isotopic studies formetasedimentary rocks from the Chinese Altai:Implications for theearly Paleozoic tectonic evolution of the Central Asian Orogenic Belt.Tectonics,26(5):TC5015,doi:10.1029/2007TC002128
Long XP,Yuan C,Sun M,Xiao WJ,Lin SF,Wang YJ and Cai KD.2008.Geochemiscal characteristics and sedimentary environments ofDevonina low metamorphic clastic sedimentary rocks in the southernmargin of the Chinese Altai,North Xinjiang.Acta PetrologicaSinica,24(4):718-732(in Chinese with English abstract)
Newton R and Perkins D.1982.Thermodynamic calibration ofgeobarometers based on the assemblages garnet-plagioclaseorthopyroxene(clinopyroxene)-quartz.American Mineralogist,67(3-4):203-222
Pattison DRM,Chacko T,Farquhar J and McF arlane CRM.2003.Temperatures of granulite-facies metamorphism:Constraints fromexperimental phase equilibria and thermobarometry corrected forretrograde exchange.Journal of Petrology,44(5):867-900
Perchuk LL and Lavrentpeva IV.1983.Experimental investigation ofexchange equilibria in the system cordierite-garnet-biotite.In:Saxena SK(ed.).Kinetics and Equilibrium in Mineral Reactions.New York,Berlin,Heidelberg:Springer-Verlag,199-239
Perkins D III and Chipera SJ.1985.Garnet-orthopyroxene-plagioclasequartz barometry:Refinement and application to the English Riversubprovince and the Minnesota River valley.Contributions toMineralogy and Petrology,89(1):69-80
Pirajno F,Mao JW,Zhang ZC,Zhang ZH and Chai FM.2008.Theassociation of mafic-ultramafic intrusions and A-type magmatism inthe Tian Shan and Altay orogens,NW China:Implications forgeodynamic evolution and potential for the discovery of new oredeposits.Journal of Asian Earth Sciences,32(2-4):165-183
Powell R and Holland T.1994.Optimal geothermometry andgeobarometry.American Mineralogist,79(1-2):120-133
Powell R,Holland TJB and Worley B.1998.Calculating phase diagraminvolving solid solutions via no-linear equations,with examples usingTHERMOCALC.Journal of Metamorphic Geology,16(4):577-586
Powell R and Holland T.1999.Relating formulations of thethermodynamics of mineral solid solutions:Activity modeling ofpyroxenes,amphiboles,and micas.American Mineralogist,84(1-2):1-14
爦engr AMC,Natal’in BA and Burtman VS.1993.Evolution of theAltaid tectonic collage and Palaeozoic crustal growth in Eurasia.Nature,364(6435):299-307
Shen XM,Zhang HX and Ma L.2013.LA-ICP-MS zircon U-Pb datingfor Jieerkuduke acidic dykes in the southern Altay range.XinjiangGeology,31(3):157-161(in Chinese with English abstract)
Sun M,Long XP,Cai KD,Jiang YD,Wang BY,Yuan C,Zhao GC,Xiao WJ and Wu FY.2009.Early Palaeozoic ridge subduction inthe Chinese Altai:Insight from the abrupt change in zircon Hfisotopic compositions.Science in China(Series D),39(7):935-948(in Chinese)
Tang GJ,Wang Q,Wyman DA,Li ZX,Zhao ZH and Yang YH.2012.Late Carboniferous highεNd(t)-εHf(t)granitoids,enclaves anddikes in western Junggar,NW China:Ridge-subduction-relatedmagmatism and crustal growth.Lithos,140(5):86-102
Tong LX,Chen YB,Xu YG and Liu WP.2011.Occurrence of bearingOpx+Sil high-temperature pelitic granulite and its geologicalsignificance.Xi’an:Abstract of 2011’s National Symposium onPetrology and Geodynamics,214(in Chinese)
Tong LX,Chen YB,Xu YG,Zhou X and Liu Z.2013.Zircon U-Pbages of the ultrahigh-temperature metapelitic granulite from the Altaiorogen,NW China,and geological implications.Acta PetrologicaSinica,29(10):3435-3445(in Chinese with English abstract)
Tong L,Chen Y and Chen L.2014a.Confirmation of ultrahightemperature metapelitic granulite in the Altay orogen and itsgeological significance.Chinese Science Bulletin,59(27):3441-3448
Tong L,Xu YG,Cawood PA,Zhou X,Chen YB and Liu Z.2014b.Anticlockwise P-T evolution at~280Ma recorded from Opx-Silbearing metapelitic granulite in the Chinese Altai orogen,possiblelink with the Tarim mantle plumeJournal of Asian Earth Sciences,94:1-11
Tong Y,Wang T,Hong DW and Han BF.2006.Pb isotopic compositionof granitoids from the Altay orogen(China):Evidence for Mantlederived origin and continental growth.Acta Geologica Sinica,80(4):517-528(in Chinese with English abstract)
Wang T,Hong DW,Tong Y,Han BF and Shi YR.2005.Zircon U-PbSHRIMP age and origin of post-orogenic Lamazhao granitic plutonfrom Altai orogen:Its implications for vertical continental growth.Acta Petrologica Sinica,21(3):640-650(in Chinese withEnglish abstract)
Wang T,Hong DW,Jahn BM,Tong Y,Wang YB,Han BF and WangXX.2006.Timing,petrogenesis,and setting of Paleozoicsynorogenic intrusions from the Altai Mountains,Northwest China:Implications for the tectonic evolution of an accretionary orogen.Journal of Geology,114(6):735-751
Wang T,Jahn BM,Kovach VP,Tong Y,Hong DW and Han BF.2009a.Nd-Sr isotopic mapping of the Chinese Altai and implicationsfor continental growth in the central Asian orogenic Belt.Lithos,110(1-4):359-372
Wang W,Wei CJ,Wang T,Lou YX and Chu H.2009b.Confirmation ofpelitic granulite in the Altai orogen and its geological significance.Chinese Science Bulletin,54(14):2543-2548
Wang W,Wei CJ,Zhang YH,Chu H,Zhao Y and Liu XC.2014.Ageand origin of sillimanite schist from the Chinese Altai metamorphicbelt:Implications for Late Palaeozoic tectonic evolution of the CentralAsian Orogenic Belt.International Geology Review,56(2):224-236
Wei CJ,Powell R and Clarke GL.2004.Calculated phase equilibria forlow-and medium-pressure metapelites in the KFMASH andKMn FMASH systems.Journal of Metamorphic Geology,22(5):495-508
Wei CJ,Clarke G,Tian W and Qiu L.2007.Transition of metamorphicseries from the kyanite-to andalusite-types in the Altai orogen,Xinjiang,China:Evidence from petrography and calculatedKMn FMASH and KFMASH phase relations.Lithos,96(3-4):353-374
Wells PRA.1977.Pyroxene thermometry in the simple and complexsystems.Contributions to Mineralogy and Petrology,62(2):129-139
White RW,Powell R,Holland TJB and Worley BA.2000.The effect ofTiO 2and Fe2O3on metapelitic assemblages at greenschist andamphibolite facies conditions:Mineral equilibria calculations in thesystem K2O-FeO-MgO-Al2O3-SiO 2-H2O-TiO 2-Fe2O3.Journal ofMetamorphic Geology,18(5):497-511
White RW,Powell R and Clarke GL.2002.The interpretation of reactiontextures in Fe-rich metapelitic granulites of the Musgrave Block,central Australia:Constraints from mineral equilibria calculations inthe system K2O-FeO-MgO-Al2O3-SiO 2-H2O-TiO 2-Fe2O3.Journalof Metamorphic Geology,20(1):41-55
White RW,Powell R and Holland TJB.2007.Progress relating tocalculation of partial melting equilibria for metapelites.Journal ofMetamorphic Geology,25(5):511-527
Windley BF,Krner A,Guo JH,Qu GS,Li YY and Zhang C.2002.Neoproterozoic to Paleozoic geology of the Altai orogen,NW China:New zircon age data and tectonic evolution.Journal of Geology,110(6):719-737
Wood BJ and Banno S.1973.Garnet-orthopyoxene and orthopyroxeneclinopyroxene relationship in simple and complex system.Contrib.Mineral.Petrol.42(2):109-124
Wu CM,Pan YS and Wang KY.1999.Refinement of the biotiteorthopyroxene geothermometer with applications.Acta PetrologicaSinica,15(3):463-468(in Chinese with English abstract)
Wu CM,Zhang J and Ren LD.2004.Empirical garnet-biotite-plagiocl ase-quartz(GBPQ)geobarometry in medium-to high-grademetapelites.Journal of Petrology,45(9):1907-1921
Xiao W,Windley BF,Badarch G,Sun S,Li J,Qin K and Wang Z.2004.Palaeozoic accretion and convergent tectonics of the southernAltaids:Implications for the growth of Central Asia.Journal of theGeological Society,161(3):339-342
Xiao WJ,Han CM,Yuan C,Chen HL,Sun M,Lin SF,Li ZL and MaoQG.2006.Unique Carboniferous-Permian tectonic-metallogenicframework of northern Xinjiang(NW China):Constraints for thetectonics of the southern Paleoasian domain.Acta Petrologica Sinica,22(5):1062-1076(in Chinese with English abstract)
Xiao WJ,Han CM,Yuan C,Sun M,Lin SF,Chen HL,Li ZL,Li JLand Sun S.2008.Middle Cambrian to Permian subduction-relatedaccretionary orogenesis of northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia.Journal ofAsian Earth Sciences,32(2-4):102-117
Xu XC,Zheng CQ and Zhao QY.2005.Metamorphic types and crustalevolution of Hercynian orogenic belt in Altai region,Xinjiang.Journal of Jilin University(Earth Science Edition),35(1):7-11(in Chinese with English abstract)
Zhai MG and Liu WJ.2001.The formation of granulite and itscontribution to evolution of the continental crust.Acta PetrologicaSinica,17(1):28-38(in Chinese with English abstract)
Zhang CG,Wei CJ and Qiu L.2004.Evolution of metamorphism and itsgeologic significance in Altaids,Xinjiang.Xinjiang Geology,22(1):16-23(in Chinese with English abstract)
Zhang CL,Li ZX,Li XH,Xu YG,Zhou G and Ye HM.2010.APermian large igneous province in Tarim and Central Aisian orogenicbelt,NW China:Results of a ca.275Ma mantle plumeGeologicalSociety of America Bulletin,122(11-12):2020-2040
Zhang CL,Santosh M,Zou HB,Xu YG,Zhou G,Dong YG,Ding RFand Wang HY.2012.Revisiting the“Irtish tectonic belt”:Implications for the Palaeozoic tectonic evolution of the Altai orogen.Journal of Asian Earth Science,52:117-133
Zheng CQ,Xu XC,Enami M and Kato T.2005.Monazite ages andgeological implications of andalusite-sillimanite type metamorphicbelt in Aletai,Xinjiang.Global Geology,24(3):236-242(inChinese with English abstract)
Zheng CQ,Kato T,Enami M and Xu XC.2007.CHIME monazite agesof metasediments from the Altai orogen in northwestern China:Devonian and Permian ages of metamorphism and their significance.Island Arc,16(4):598-604
Zheng CQ,Xu XC,Kato T and Enami M.2007.Permian CHIME ages ofmonazites for the kyanite-sillimanite type metamorphic belt inChonghuer area,Altai,Xinjiang and their geological implications.Geological Journal of China University,13(3):566-573(inChinese with English abstract)
Zhuang YX.1994.The PTSt evolution of metamorphism and developmentmechanism of the thermal-structural-gneiss domes in the ChineseAltaides.Acta Geologica Sinica,68(1):35-47(in Chinese withEnglish abstract)
Zou TR,Cao HZ and Wu BQ.1988.Orogenic and anorogenic granitoidsof the Altay Mountains,Xinjiang and their discrimination criteria.Acta Geologica Sinica,62(3):228-243(in Chinese with Englishabstract)
陈汉林,杨树锋,厉子龙,余兴,肖文交,袁超,林秀斌,李继亮.2006.阿尔泰造山带富蕴基性麻粒岩锆石SHRIMP U-Pb年代学及其构造意义.岩石学报,22(5):1351-1358
陈立辉,韩宝福.2006.新疆北部乌恰沟地区镁铁质侵入岩的年代学地球化学和同位素组成:对地幔源区特征和深部过程的约束.岩石学报,22(5):1201-1214
宫红良,陈正乐,胡远清,李丽,赖新荣,马庆佑,李玉英,胡博,张文贵.2007.阿尔泰额尔齐斯带东段酸性岩墙群地球化学特征及其地质意义.岩石学报,23(5):889-899
胡霭琴,张国新,张前锋,李天德,张积斌.2002.阿尔泰造山带变质岩系时代问题的讨论.地质科学,37(2):129-142
胡霭琴,韦刚健,邓文峰,陈林丽.2006.阿尔泰地区青河县西南片麻岩中锆石SHRIMP U-Pb定年及其地质意义.岩石学报,22(1):1-10
李会军,何国琦,吴泰然,吴波.2006.阿尔泰-蒙古微大陆的确定及其意义.岩石学报,22(5):1369-1379
李天德,祁志明,吴柏青,肖世禄,赵昌龙,别斯帕耶夫XA,波利杨斯基HB,季亚契科夫BA,甘任科ГД,叶夫图申科НП,叶夫图申科ОП.1996.中国和哈萨克斯坦阿尔泰地质及成矿研究的新进展.见:中国地质学会编.献给三十届国际地质大会“八五”地质科技重要成果学术交流会议论文选集.北京:冶金工业出版社,256-259
厉子龙,陈汉林,杨树锋,肖文交,Tainosho Y.2004.阿尔泰基性麻粒岩的发现:来自矿物学的证据.岩石学报,20(6):1445-1455
龙晓平,袁超,孙敏,肖文交,林寿发,王毓靖,蔡克大.2008.北疆阿尔泰南缘泥盆系浅变质碎屑沉积岩地球化学特征及其形成环境.岩石学报,24(4):718-732
沈晓明,张海祥,马林.2013.阿尔泰南缘杰尔库都克酸性岩脉LAICP-MS锆石U-Pb测年.新疆地质,31(3):157-161
孙敏,龙晓平,蔡克大,蒋映德,王步云,袁超,赵国春,肖文交,吴福元.2009.阿尔泰早古生代末期洋中脊俯冲:锆石Hf同位素组成突变的启示.中国科学(D辑),39(7):935-948
仝来喜,陈义兵,徐义刚,刘文平.2011.阿尔泰造山带含Opx+Sil高温变泥质麻粒岩的产出及其地质意义.西安:2011年全国岩石学与地球动力学研讨会论文摘要(上册),214
仝来喜,陈义兵,徐义刚,周信,刘兆.2013.阿尔泰超高温变泥质麻粒岩的锆石U-Pb年龄及其地质意义.岩石学报,29(10):3435-3445
童英,王涛,洪大卫,韩宝福.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征:幔源成因佐证及陆壳生长意义.地质学报,80(4):517-528
王涛,洪大伟,童英,韩宝福,石玉若.2005.中国阿尔泰造山带后造山喇嘛昭花岗岩体锆石SHRIMP年龄-成因及陆壳垂向生长意义.岩石学报,21(3):640-650
吴春明,潘裕生,王凯怡.1999.黑云母-斜方辉石温度计的重新标度及其应用.岩石学报,15(3):463-468
肖文交,韩春明,袁超,陈汉林,孙敏,林寿发,厉子龙,毛启贵,张继恩,孙枢,李继亮.2006.新疆北部石炭纪-二叠纪独特的构造成矿作用:对古亚洲洋构造域南部大地构造演化的制约.岩石学报,22(5):1062-1076
徐学纯,郑常青,赵庆英.2005.阿尔泰海西造山带区域变质作用类型与地壳演化.吉林大学学报(地球科学版),35(1):7-11
翟明国,刘文军.2001.麻粒岩的形成及其对大陆地壳演化的贡献.岩石学报,17(1):28-38
张翠光,魏春景,邱林.2004.新疆阿尔泰造山带变质作用演化及其地质意义.新疆地质,22(1):16-23
郑常青,徐学纯,Enami M,Kato T.2005.新疆阿尔泰红柱石-夕线石型变质带的独居石年龄及其地质意义.世界地质,24(3):236-242
郑常青,徐学纯,Kato T,Enami M.2007.新疆阿尔泰冲乎尔地区蓝晶石-夕线石型变质带独居石CHIME二叠纪年龄及其地质意义.高校地质学报,13(3):566-573
庄育勋.1994.中国阿尔泰造山带变质作用PTSt演化和热-构造-片麻岩穹窿形成机制.地质学报,68(1):35-47
邹天人,曹惠志,吴柏青.1988.新疆阿尔泰造山花岗岩和非造山花岗岩及其判别标志.地质学报,62(3):228-243