Geochronology,geochemistry and geodynamics implications of Middle Triassic garnet-bearing muscovite monzogranite in central Jilin Province
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摘要
Zircon LA-ICP-MS U-Pb geochronology and geochemical analyses are undertaken for the garnet-bearing muscovite monzogranite in Yitong area,central Jilin Province. The formation age and petrogenesis of the granite are determined,and the regional tectonic background is discussed. Zircons from the granite are euhedral-subhedral in shape,and display fine-scale oscillatory growth zoning,indicating a magmatic origin. LAICP-MS zircon U-Pb dating result indicates that the garnet-bearing muscovite monzogranites formed in the middle Triassic( 243 Ma). The garnet-bearing muscovite monzogranites have high SiO_2( Si O2= 74. 1%--76. 49%),rich aluminum( Al_2O_3= 14. 47%--14. 68%) and alkali( Na_2O + K_2O = 4. 31%--7. 9%),low Fe_2O_3 T and MgO( MgO = 0. 1%--0. 13%,Fe_2O_3 T = 0. 46%--1. 02%). The ratio of CaO/Na_2O is between 0. 17--0. 21. The garnet-bearing muscovite monzogranites in Yitong region are relatively enriched in light rare earth elements( LREEs) and large ion lithophile elements( LILEs),and depleted of heavy rare earth elements( HREEs) and high field strength elements( HFSEs). They are characterized by high Sr and Ba,poor Rb and Y,and negative Eu abnormally( δEu = 0. 48--0. 62),with Rb/Sr < 1. The ε_(Hf)( t) values and T_(DM2) of zircons range from + 6. 10 to + 8. 00 and from 725 Ma to 814 Ma,respectively. The above features indicate that garnet-bearing muscovite monzogranites in Yitong area were derived from partial melting of metasedimentary rock.These granites have high Sr/Y ratios,which suggest they formed in a thickened continental crust. Combined with the coeval granitic rocks in central Jilin Province,we suggested that a significant collisional and thickening event took place during the Middle Triassic.
Zircon LA-ICP-MS U-Pb geochronology and geochemical analyses are undertaken for the garnet-bearing muscovite monzogranite in Yitong area,central Jilin Province. The formation age and petrogenesis of the granite are determined,and the regional tectonic background is discussed. Zircons from the granite are euhedral-subhedral in shape,and display fine-scale oscillatory growth zoning,indicating a magmatic origin. LAICP-MS zircon U-Pb dating result indicates that the garnet-bearing muscovite monzogranites formed in the middle Triassic( 243 Ma). The garnet-bearing muscovite monzogranites have high SiO_2( Si O2= 74. 1%--76. 49%),rich aluminum( Al_2O_3= 14. 47%--14. 68%) and alkali( Na_2O + K_2O = 4. 31%--7. 9%),low Fe_2O_3 T and MgO( MgO = 0. 1%--0. 13%,Fe_2O_3 T = 0. 46%--1. 02%). The ratio of CaO/Na_2O is between 0. 17--0. 21. The garnet-bearing muscovite monzogranites in Yitong region are relatively enriched in light rare earth elements( LREEs) and large ion lithophile elements( LILEs),and depleted of heavy rare earth elements( HREEs) and high field strength elements( HFSEs). They are characterized by high Sr and Ba,poor Rb and Y,and negative Eu abnormally( δEu = 0. 48--0. 62),with Rb/Sr < 1. The ε_(Hf)( t) values and T_(DM2) of zircons range from + 6. 10 to + 8. 00 and from 725 Ma to 814 Ma,respectively. The above features indicate that garnet-bearing muscovite monzogranites in Yitong area were derived from partial melting of metasedimentary rock.These granites have high Sr/Y ratios,which suggest they formed in a thickened continental crust. Combined with the coeval granitic rocks in central Jilin Province,we suggested that a significant collisional and thickening event took place during the Middle Triassic.
Zircon LA-ICP-MS U-Pb geochronology and geochemical analyses are undertaken for the garnet-bearing muscovite monzogranite in Yitong area,central Jilin Province. The formation age and petrogenesis of the granite are determined,and the regional tectonic background is discussed. Zircons from the granite are euhedral-subhedral in shape,and display fine-scale oscillatory growth zoning,indicating a magmatic origin. LAICP-MS zircon U-Pb dating result indicates that the garnet-bearing muscovite monzogranites formed in the middle Triassic( 243 Ma). The garnet-bearing muscovite monzogranites have high SiO_2( Si O2= 74. 1%--76. 49%),rich aluminum( Al_2O_3= 14. 47%--14. 68%) and alkali( Na_2O + K_2O = 4. 31%--7. 9%),low Fe_2O_3 T and MgO( MgO = 0. 1%--0. 13%,Fe_2O_3 T = 0. 46%--1. 02%). The ratio of CaO/Na_2O is between 0. 17--0. 21. The garnet-bearing muscovite monzogranites in Yitong region are relatively enriched in light rare earth elements( LREEs) and large ion lithophile elements( LILEs),and depleted of heavy rare earth elements( HREEs) and high field strength elements( HFSEs). They are characterized by high Sr and Ba,poor Rb and Y,and negative Eu abnormally( δEu = 0. 48--0. 62),with Rb/Sr < 1. The ε_(Hf)( t) values and T_(DM2) of zircons range from + 6. 10 to + 8. 00 and from 725 Ma to 814 Ma,respectively. The above features indicate that garnet-bearing muscovite monzogranites in Yitong area were derived from partial melting of metasedimentary rock.These granites have high Sr/Y ratios,which suggest they formed in a thickened continental crust. Combined with the coeval granitic rocks in central Jilin Province,we suggested that a significant collisional and thickening event took place during the Middle Triassic.
引文
Barba L,Zhang J Y.1997.The genesis of two major peraluminous granites.Journal of Gems and Gemmology,14(2):11-14.(in Chinese)
Boynton W V.1984.Chapter 3-Cosmochemistry of the rare earth elements:Meteorite Studies Developments in Geochemistry,2(2):63-114.
Brown M B.2010.Melting of the continental crust during orogenesis:the thermal,rheological,and compositional consequences of melt transport from lower to upper continental crust.Canadian Journal of Earth Sciences,47(5):655-694.
Brown M.2013.Granite:from genesis to emplacement.Bulletin of the Geological Society of America,125(7/8):1079-1113.
Bureau of Geology and Mineral Resources in Jilin Province.1988.Regional geological chronicles of Jilin Province.Beijing:Geological Publishing House,313-338.(in Chinese)
Cao H H,Xu W L,Pei F P,et al.2013.Zircon U-Pb geochronology and petrogenesis of the Late Paleozoic-Early Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block.Lithos,170/171(6):191-207.
Deng J F.1987.Rock phase balance and rock genesis.Wuhan:Wuhan College of Geology Publishing House,62-64.(in Chinese)
Deng J F,Zhao H L,Lai S C,et al.1994.Generation of muscovite/two-mica granite and intracontinental subduction.Earth Science,19(2):139-147.(in Chinese with English abstract)
Douce A E P,Johnston A D.1991.Phase equilibria and melt productivity in the pelitic system:implications for the origin of peraluminous granitoids and aluminous granulites.Contributions to Mineralogy&Petrology,107(2):202-218.
Gao L E,Zeng L S,Asimow P D.2017.Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources:the Himalayan leucogranites.Geology,45(1):G38336.1.
Guo S S,Li S G.2007.Petrological and geochemical constraints on the origin of leucogranites.Earth Science Frontiers,14(6):290-298.(in Chinese with English abstract)
Harris N B W,Inger S.1992.Trace element modelling of pelite-derived granites:Contributions to Mineralogy and Petrology.Contributions to Mineralogy&Petrology,110(1):46-56.
Huang C M,Zhao Z D,Zhu D C,et al.2013.Geochemistry,zircon U-Pb chronology and Hf isotope of Luozha leucogranite,southern Tibet:Implication for petrogenesis.Acta Petrologica Sinica,29(11):3689-3702.(in Chinese with English abstract)
Jahn B M,Wu F Y,Chen B.2000.Massive granitoid generation in Central Asia:Nd isotope evidence and implication for continental growth in the Phanerozoic.Episodes,23(2):82-92.
Koschek G.1993.Origin and significance of the SEM cathodoluminescence from zircon.Journal of Microscopy,171(3):223-232.
Li J Y.1998.Some new ideas on tectonic of NE China and its neighboring areas.Geological Review,44(4):339-347.(in Chinese with English abstract)
Li J Y.2004.Structure characteristics of crustal“mosaicking and superimposition”of the continent of China and its evolution.Geological Bulletin of China,23(Z2):986-1004.(in Chinese with English abstract)
Li J Y.2006.Permian geodynamic setting of Northeast China and adjacent regions:closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences,26(3):207-224.
Li L,Zhang C L,Zhou Y,et al.2012.Early Mesozoic crustand mantle-derived magmatic mixing in the Qinling Orogeny:evidence from geochemistry of mafic microgranular enclaves in the Dongjiangkou pluton.Geological Journal of China Universities,18(2):291-306.(in Chinese with English abstract)
Li S L,Ouyang Z Y.1998.Tectonic framework and evolution of Xing'anling--Mongolian orogenic belt(XMOB)and it's adjacent region.Marine Geology&Quaternary Geology,18(3):45-54.(in Chinese with English abstract)
Liu H T,Zhai M G,Liu J M,et al.2002.The Mesozoic granitoids in the northern marginal region of North China Craton:evolution from post-collisional to anorogenic settings.Acta Petrologica Sinica,18(4):433-448.(in Chinese with English abstract)
Liu J F.2009.Late Paleozoic magmatism and its constraints on regional tectonic evolution in Linxi-Dongwuqi area,Inner Mongolia:doctor's degree thesis.Changchun:Jilin University.(in Chinese with English abstract)
Liu Y S,Hu Z C,Gao S,et al.2008.In situ,analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1/2):34-43.
Liu Y S,Gao S,Hu Z C,et al.2010a.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.
Liu Y S,Hu Z C,Zong K Q,et al.2010b.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Science Bulletin,55(15):1535-1546.
Ludwig K R.2003.Users manual for Isoplot 3.0:a geochronological toolkit for Microsoft Excel.Berkeley:Berkeley Geochronology Centre,Special Publication.1-74.
Peng X D,Zhang M S,Li X M.1999.The evolution of Paleozoic tectonic paleogeography in Jilin and Heilongjiang orogenic belt.World Geology,18(3):24-28.(in Chinese with English abstract)
Peng Y J,Zhao C B.2001.The evolution of the paleo Jihei orogenic belt and accretion of the continental crust.Jilin Geology,20(2):1-9.(in Chinese with English abstract)
Ren J S.1991.The basic characteristics of the tectonic evolution of the continental lithosphere in China.Geological Bulletin of China,(4):289-293.(in Chinese with English abstract)
Ren J S,Wang Z X,Chen B W,et al.1999.The tectonics of China from a global view,a guide to the tectonic map of China and adjacent regions.Beijing:Geological Publishing House,4-32.(in Chinese)
Shao J A.1995.Northeast China terrain and Northeast Asian Continent evolution.Beijing:Seismological Press,29-36.(in Chinese)
Skjerlie K P,Johnston A D.2015.Vapour-absent melting from10 to 20 kbar of crustal rocks that contain multiple hydrous phases:Implications for anatexis in the deep to very deep continental crust and active continental margins.Journal of Petrology,37(3):661-691.
Sylvester P J.1998.Post-collisional strongly peraluminous granites.Lithos,45(1/4):29-44.
Sui Z M,Chen Y J.2011.Zircon saturation temperatures of granites in eastern Great Xing'an Range and its geological signification.30(2):162-172.(in Chinese with English abstract)
Sun D Y,Wu F Y,Zhang Y B,et al.2004.The final closing time of the west Lamulun River-Changchun-Yanji plate suture zone:Evidence from the Dayushan granitic pluton,Jilin Province.Journal of Jilin University(Earth Science Edition),34(2):174-181.(in Chinese with English abstract)
Sun S S,Mcdonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes//Saund A D,Norry M J.(eds.)Magmatism in the ocean basins.London:Geological Society Special Publications,42:313-345.
Wang Y Q,Su Y Z.1996.Regional stratigraphic development and crustal evolution in Northeast China.Jilin Geology,15(34):118-145.(in Chinese)
Wu F Y,Cao L.1999.Some important problems of geology in Northeastern Asia.World Geology,18(2):1-13.(in Chinese with English abstract).
Wu F Y,Sun D Y,Li H,et al.2002.A-type granites in northeastern China:age and geochemical constraints on their petrogenesis.Chemical Geology,187(1/2):143-173.
Wu Y B,Zheng Y F.2004.Study on the mineralogy of zircon and its constraints on the interpretation of U-Pb age.Chinese Science Bulletin,49(16):1589-1604.(in Chinese)
Wu F Y,Yang Y H,Xie L W,et al.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1/2):105-126.
Wu F Y,Zhao G C,Sun D Y,et al.2007.The Hulan Group:its role in the evolution of the Central Asian Orogenic Belt of NE China.Journal of Asian Earth Sciences,30(3):542-556.
Wu F Y,Sun D Y,Ge W C,et al.2011.Geochronology of the Phanerozoic granitoids in northeastern China.Journal of Asian Earth Sciences,41(1):1-30.
Wu F Y,Liu Z C,Liu X C,et al.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift.Acta Petrologica Sinica,31(1):1-36.(in Chinese with English abstract).
Wu F Y,Liu X C,Ji W Q,et al.2017.Highly fractionated granites:recognition and research.China Earth Sciences,(7):1-19.
Xiao Q H.2002.Granite research thinking and methods.Beijing:Geological Publishing House,53-63.(in Chinese)
Xie M Q.2000.Amalgamation and its driving mechanism:tectonic evolution of northeast China and adjacent areas.Beijing:Science Press,1-13.(in Chinese)
Xu P,Wu F,Xie L,et al.2004.Hf isotopic compositions of the standard zircons for U-Pb dating.Chinese Science Bulletin,49(15):1642-1648.
Xu W L,Ji W Q,Pei F P,et al.2009.Triassic volcanism in eastern Heilongjiang and Jilin provinces,NE China:chronology,geochemistry,and tectonic implications.Journal of Asian Earth Sciences,34(3):392-402.
Yang J H,Wu F Y,Shao J A,et al.2006.Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt,North China.Earth&Planetary Science Letters,246(3):336-352.
Zeng L S,Saleeby J B,Asimow P.2005.Nd isotope disequilibrium during crustal anatexis:a record from the Goat Ranch migmatite complex,southern Sierra Nevada batholith,California.Geology,33(1):53-56.
Zeng L S,Saleeby J B,Ducea M.2005.Geochemical characteristics of crustal anatexis during the formation of migmatite at the Southern Sierra Nevada,California.Contributions to Mineralogy&Petrology,150(4):386-402.
Zeng L S,Gao L E.2017.Cenozoic crustal anatexis and the leucogranites in the Himalayan collisional orogenic belt.Acta Petrologica Sinica,33(5):1420-1444.(in Chinese with English abstract)
Zhang X Z,Ma Y X,Chi X G,et al.2012.Discussion on Phanerozoic tectonic evolution in Northeastern China.Journal of Jilin University(Earth Science Edition),42(5):1269-1285.(in Chinese with English abstract)
Zhang Y B,Wu F Y,Wilde S,et al.2004.Zircon U-Pb ages and tectonic implications of‘Early Paleozoic'granitoids at Yanbian,Jilin Province,northeast China.Island Arc,13(4):484-505.
Zhao C J.1996.Tectonic framework and crust evolution of eastern Jilin and Heilongjiang Provinces.Shenyang:Liaoning University Press,1-186.(in Chinese with English abstract)
Zhang Q,Wang Y,Li C D,et al.2006.Granite classification on the basis of Sr and Yb contents and its implications.Acta Petrologica Sinica,22(9):49-69.(in Chinese with English abstract)
Zhang S H,Zhao Y,Liu J M,et al.2010.Geochronology,geochemistry and tectonic setting of the Late PaleozoicEarly Mesozoic magmatism in the northern margin of the North China Block:a preliminary review.Acta Petrologica et Mineralogica,29(6):824-842.(in Chinese with English abstract)
Zhou Z B,Pei F P,Wang Z W,et al.2016.Detrital zircons from late Permian to Triassic sedimentary rocks of Jilin Province,NE China:constraints on the timing of final closure of the Paleo-Asian Ocean.Journal of Asian Earth Sciences,144(15):82-109.
Boynton W V.1984.Chapter 3-Cosmochemistry of the rare earth elements:Meteorite Studies Developments in Geochemistry,2(2):63-114.
Brown M B.2010.Melting of the continental crust during orogenesis:the thermal,rheological,and compositional consequences of melt transport from lower to upper continental crust.Canadian Journal of Earth Sciences,47(5):655-694.
Brown M.2013.Granite:from genesis to emplacement.Bulletin of the Geological Society of America,125(7/8):1079-1113.
Bureau of Geology and Mineral Resources in Jilin Province.1988.Regional geological chronicles of Jilin Province.Beijing:Geological Publishing House,313-338.(in Chinese)
Cao H H,Xu W L,Pei F P,et al.2013.Zircon U-Pb geochronology and petrogenesis of the Late Paleozoic-Early Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block.Lithos,170/171(6):191-207.
Deng J F.1987.Rock phase balance and rock genesis.Wuhan:Wuhan College of Geology Publishing House,62-64.(in Chinese)
Deng J F,Zhao H L,Lai S C,et al.1994.Generation of muscovite/two-mica granite and intracontinental subduction.Earth Science,19(2):139-147.(in Chinese with English abstract)
Douce A E P,Johnston A D.1991.Phase equilibria and melt productivity in the pelitic system:implications for the origin of peraluminous granitoids and aluminous granulites.Contributions to Mineralogy&Petrology,107(2):202-218.
Gao L E,Zeng L S,Asimow P D.2017.Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources:the Himalayan leucogranites.Geology,45(1):G38336.1.
Guo S S,Li S G.2007.Petrological and geochemical constraints on the origin of leucogranites.Earth Science Frontiers,14(6):290-298.(in Chinese with English abstract)
Harris N B W,Inger S.1992.Trace element modelling of pelite-derived granites:Contributions to Mineralogy and Petrology.Contributions to Mineralogy&Petrology,110(1):46-56.
Huang C M,Zhao Z D,Zhu D C,et al.2013.Geochemistry,zircon U-Pb chronology and Hf isotope of Luozha leucogranite,southern Tibet:Implication for petrogenesis.Acta Petrologica Sinica,29(11):3689-3702.(in Chinese with English abstract)
Jahn B M,Wu F Y,Chen B.2000.Massive granitoid generation in Central Asia:Nd isotope evidence and implication for continental growth in the Phanerozoic.Episodes,23(2):82-92.
Koschek G.1993.Origin and significance of the SEM cathodoluminescence from zircon.Journal of Microscopy,171(3):223-232.
Li J Y.1998.Some new ideas on tectonic of NE China and its neighboring areas.Geological Review,44(4):339-347.(in Chinese with English abstract)
Li J Y.2004.Structure characteristics of crustal“mosaicking and superimposition”of the continent of China and its evolution.Geological Bulletin of China,23(Z2):986-1004.(in Chinese with English abstract)
Li J Y.2006.Permian geodynamic setting of Northeast China and adjacent regions:closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences,26(3):207-224.
Li L,Zhang C L,Zhou Y,et al.2012.Early Mesozoic crustand mantle-derived magmatic mixing in the Qinling Orogeny:evidence from geochemistry of mafic microgranular enclaves in the Dongjiangkou pluton.Geological Journal of China Universities,18(2):291-306.(in Chinese with English abstract)
Li S L,Ouyang Z Y.1998.Tectonic framework and evolution of Xing'anling--Mongolian orogenic belt(XMOB)and it's adjacent region.Marine Geology&Quaternary Geology,18(3):45-54.(in Chinese with English abstract)
Liu H T,Zhai M G,Liu J M,et al.2002.The Mesozoic granitoids in the northern marginal region of North China Craton:evolution from post-collisional to anorogenic settings.Acta Petrologica Sinica,18(4):433-448.(in Chinese with English abstract)
Liu J F.2009.Late Paleozoic magmatism and its constraints on regional tectonic evolution in Linxi-Dongwuqi area,Inner Mongolia:doctor's degree thesis.Changchun:Jilin University.(in Chinese with English abstract)
Liu Y S,Hu Z C,Gao S,et al.2008.In situ,analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1/2):34-43.
Liu Y S,Gao S,Hu Z C,et al.2010a.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.
Liu Y S,Hu Z C,Zong K Q,et al.2010b.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Science Bulletin,55(15):1535-1546.
Ludwig K R.2003.Users manual for Isoplot 3.0:a geochronological toolkit for Microsoft Excel.Berkeley:Berkeley Geochronology Centre,Special Publication.1-74.
Peng X D,Zhang M S,Li X M.1999.The evolution of Paleozoic tectonic paleogeography in Jilin and Heilongjiang orogenic belt.World Geology,18(3):24-28.(in Chinese with English abstract)
Peng Y J,Zhao C B.2001.The evolution of the paleo Jihei orogenic belt and accretion of the continental crust.Jilin Geology,20(2):1-9.(in Chinese with English abstract)
Ren J S.1991.The basic characteristics of the tectonic evolution of the continental lithosphere in China.Geological Bulletin of China,(4):289-293.(in Chinese with English abstract)
Ren J S,Wang Z X,Chen B W,et al.1999.The tectonics of China from a global view,a guide to the tectonic map of China and adjacent regions.Beijing:Geological Publishing House,4-32.(in Chinese)
Shao J A.1995.Northeast China terrain and Northeast Asian Continent evolution.Beijing:Seismological Press,29-36.(in Chinese)
Skjerlie K P,Johnston A D.2015.Vapour-absent melting from10 to 20 kbar of crustal rocks that contain multiple hydrous phases:Implications for anatexis in the deep to very deep continental crust and active continental margins.Journal of Petrology,37(3):661-691.
Sylvester P J.1998.Post-collisional strongly peraluminous granites.Lithos,45(1/4):29-44.
Sui Z M,Chen Y J.2011.Zircon saturation temperatures of granites in eastern Great Xing'an Range and its geological signification.30(2):162-172.(in Chinese with English abstract)
Sun D Y,Wu F Y,Zhang Y B,et al.2004.The final closing time of the west Lamulun River-Changchun-Yanji plate suture zone:Evidence from the Dayushan granitic pluton,Jilin Province.Journal of Jilin University(Earth Science Edition),34(2):174-181.(in Chinese with English abstract)
Sun S S,Mcdonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes//Saund A D,Norry M J.(eds.)Magmatism in the ocean basins.London:Geological Society Special Publications,42:313-345.
Wang Y Q,Su Y Z.1996.Regional stratigraphic development and crustal evolution in Northeast China.Jilin Geology,15(34):118-145.(in Chinese)
Wu F Y,Cao L.1999.Some important problems of geology in Northeastern Asia.World Geology,18(2):1-13.(in Chinese with English abstract).
Wu F Y,Sun D Y,Li H,et al.2002.A-type granites in northeastern China:age and geochemical constraints on their petrogenesis.Chemical Geology,187(1/2):143-173.
Wu Y B,Zheng Y F.2004.Study on the mineralogy of zircon and its constraints on the interpretation of U-Pb age.Chinese Science Bulletin,49(16):1589-1604.(in Chinese)
Wu F Y,Yang Y H,Xie L W,et al.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1/2):105-126.
Wu F Y,Zhao G C,Sun D Y,et al.2007.The Hulan Group:its role in the evolution of the Central Asian Orogenic Belt of NE China.Journal of Asian Earth Sciences,30(3):542-556.
Wu F Y,Sun D Y,Ge W C,et al.2011.Geochronology of the Phanerozoic granitoids in northeastern China.Journal of Asian Earth Sciences,41(1):1-30.
Wu F Y,Liu Z C,Liu X C,et al.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift.Acta Petrologica Sinica,31(1):1-36.(in Chinese with English abstract).
Wu F Y,Liu X C,Ji W Q,et al.2017.Highly fractionated granites:recognition and research.China Earth Sciences,(7):1-19.
Xiao Q H.2002.Granite research thinking and methods.Beijing:Geological Publishing House,53-63.(in Chinese)
Xie M Q.2000.Amalgamation and its driving mechanism:tectonic evolution of northeast China and adjacent areas.Beijing:Science Press,1-13.(in Chinese)
Xu P,Wu F,Xie L,et al.2004.Hf isotopic compositions of the standard zircons for U-Pb dating.Chinese Science Bulletin,49(15):1642-1648.
Xu W L,Ji W Q,Pei F P,et al.2009.Triassic volcanism in eastern Heilongjiang and Jilin provinces,NE China:chronology,geochemistry,and tectonic implications.Journal of Asian Earth Sciences,34(3):392-402.
Yang J H,Wu F Y,Shao J A,et al.2006.Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt,North China.Earth&Planetary Science Letters,246(3):336-352.
Zeng L S,Saleeby J B,Asimow P.2005.Nd isotope disequilibrium during crustal anatexis:a record from the Goat Ranch migmatite complex,southern Sierra Nevada batholith,California.Geology,33(1):53-56.
Zeng L S,Saleeby J B,Ducea M.2005.Geochemical characteristics of crustal anatexis during the formation of migmatite at the Southern Sierra Nevada,California.Contributions to Mineralogy&Petrology,150(4):386-402.
Zeng L S,Gao L E.2017.Cenozoic crustal anatexis and the leucogranites in the Himalayan collisional orogenic belt.Acta Petrologica Sinica,33(5):1420-1444.(in Chinese with English abstract)
Zhang X Z,Ma Y X,Chi X G,et al.2012.Discussion on Phanerozoic tectonic evolution in Northeastern China.Journal of Jilin University(Earth Science Edition),42(5):1269-1285.(in Chinese with English abstract)
Zhang Y B,Wu F Y,Wilde S,et al.2004.Zircon U-Pb ages and tectonic implications of‘Early Paleozoic'granitoids at Yanbian,Jilin Province,northeast China.Island Arc,13(4):484-505.
Zhao C J.1996.Tectonic framework and crust evolution of eastern Jilin and Heilongjiang Provinces.Shenyang:Liaoning University Press,1-186.(in Chinese with English abstract)
Zhang Q,Wang Y,Li C D,et al.2006.Granite classification on the basis of Sr and Yb contents and its implications.Acta Petrologica Sinica,22(9):49-69.(in Chinese with English abstract)
Zhang S H,Zhao Y,Liu J M,et al.2010.Geochronology,geochemistry and tectonic setting of the Late PaleozoicEarly Mesozoic magmatism in the northern margin of the North China Block:a preliminary review.Acta Petrologica et Mineralogica,29(6):824-842.(in Chinese with English abstract)
Zhou Z B,Pei F P,Wang Z W,et al.2016.Detrital zircons from late Permian to Triassic sedimentary rocks of Jilin Province,NE China:constraints on the timing of final closure of the Paleo-Asian Ocean.Journal of Asian Earth Sciences,144(15):82-109.