浙西南遂昌-大柘地区石榴角闪二长片麻岩成因及变质演化
|
摘要
浙西南遂昌-大柘地区八都群中分布一套含石榴石、角闪石的二长片麻岩,发育典型石榴石"白眼圈"反应结构,但其成因及变质演化目前尚不明确.运用矿物X射线电子探针微区分析、LA-ICP-MS锆石U-Pb定年并结合全岩主微量元素进行了研究.识别出3个阶段的变质矿物共生组合:进变质阶段(M_1)矿物组合为石榴石变斑晶内部的包裹体矿物石榴石+角闪石+斜长石+石英(Grt_1+Amp_1+Pl_1+Q),变质峰期矿物组合(M_2)为石榴子石变斑晶幔部和基质矿物钾长石+斜长石+黑云母+石英(Grt_2+Kf_2+Pl_2+Bt_2+Q),退变质阶段矿物组合(M_3)为"白眼圈"后成合晶角闪石+斜长石+黑云母+钛铁矿(Amp_3+Pl_3+Bt_3+Ilm).矿物地质温压计和相平衡模拟估算的3阶段P-T条件分别为:进变质阶段为600~700℃/0.60~0.65GPa,变质峰期为800~820℃/0.94~0.96GPa,退变质阶段为550~700℃/0.56~0.71GPa,变质程度达到麻粒岩相,变质作用PTt轨迹显示顺时针型式,具有近等温降压(ITD)特征,暗示其经历了地壳加厚和快速折返过程.岩石地球化学特征显示其原岩为准铝质A型花岗岩,含有少量幔源组分,形成于造山后的陆壳拉张环境;锆石U-Pb定年呈现二阶段年龄特征,成岩年龄为1.83~1.85Ga,表明石榴角闪二长片麻岩的原岩形成于古元古代,变质年龄为220~230Ma,显示了印支期变质作用对古元古代花岗岩的改造,是浙西南地区对印支期古太平洋板块向华南板块俯冲过程的响应,也为浙西南地区印支期造山作用提供了新的证据.
There is a set of garnet amphibolite monzogneiss which developed typical garnet"white eye socket"structure from the Badu Group in Suichang-Dazhe region,southwestern Zhejiang Province.However,its genesis and metamorphic evolution remain unclear.In this study,mineral X-ray microprobe microanalysis,LA-ICP-MS zircon U-Pb dating and whole-rock major and trace element analyses were carried out to address these questions.Three stages of mineral assemblages have been identified:the prograde metamorphic assemblages(M_1)are mineral inclusions garnet+amphibole+plagioclase+quartz(Grt_1 +Amp_1+Pl_1 +Q)preserved in the garnet porphyroblasts,the peak metamorphic assemblages(M_2)are represented by the"garnet-mantles"and the matrix minerals garnet+K-feldspar+plagioclase+biotite+quartz(Grt_2 +Kf_2 +Pl_2 +Bt_2 +Q),whereas the retrograde assemblages(M_3)are composed of amphibole+plagioclase+biotite+ilmenite(Amp_3+Pl_3+Bt_3+Ilm)symplectites rimming the garnet porphyroblasts.Thermobarometric computation and phase equilibrium modeling show that the metamorphic conditions of the garnet amphibolite monzogneiss are 600-700 ℃/0.60-0.65 GPa for the M_1 stage,800-820℃/0.94-0.96 GPa for the metamorphic peak M_2 stage,and 550-700℃/0.56-0.71 GPa for the retrograde M_3 stage,respectively.Metamorphic grade reached granulite facies and metamorphism PTt paths are characterized by clockwise pattern involving the nearly isothermal decompression(ITD)segments,indicating crustal thickening and rapid exhumation process.Petrogeochemistry shows that the protolith of monzogneiss is metaluminous A-type granite with some mantle-derived components which formed in continental crust extensional environment during post orogeny.LA-ICP-MS zircon U-Pb dating indicates two-stage age characteristics,in which the diagenetic age of 1.83-1.85 Ga suggests the protolith of monzogneiss formed in the Paleoproterozoic and the metamorphic age of 220-230 Ma shows the reworking of Indosinian metamorphism to Paleoproterozoic granite.It is the response to the subduction of Indo Pacific plate into South China plate during Indosinian,which provides new evidence for Indosinian orogeny in the southwestern Zhejiang.
There is a set of garnet amphibolite monzogneiss which developed typical garnet"white eye socket"structure from the Badu Group in Suichang-Dazhe region,southwestern Zhejiang Province.However,its genesis and metamorphic evolution remain unclear.In this study,mineral X-ray microprobe microanalysis,LA-ICP-MS zircon U-Pb dating and whole-rock major and trace element analyses were carried out to address these questions.Three stages of mineral assemblages have been identified:the prograde metamorphic assemblages(M_1)are mineral inclusions garnet+amphibole+plagioclase+quartz(Grt_1 +Amp_1+Pl_1 +Q)preserved in the garnet porphyroblasts,the peak metamorphic assemblages(M_2)are represented by the"garnet-mantles"and the matrix minerals garnet+K-feldspar+plagioclase+biotite+quartz(Grt_2 +Kf_2 +Pl_2 +Bt_2 +Q),whereas the retrograde assemblages(M_3)are composed of amphibole+plagioclase+biotite+ilmenite(Amp_3+Pl_3+Bt_3+Ilm)symplectites rimming the garnet porphyroblasts.Thermobarometric computation and phase equilibrium modeling show that the metamorphic conditions of the garnet amphibolite monzogneiss are 600-700 ℃/0.60-0.65 GPa for the M_1 stage,800-820℃/0.94-0.96 GPa for the metamorphic peak M_2 stage,and 550-700℃/0.56-0.71 GPa for the retrograde M_3 stage,respectively.Metamorphic grade reached granulite facies and metamorphism PTt paths are characterized by clockwise pattern involving the nearly isothermal decompression(ITD)segments,indicating crustal thickening and rapid exhumation process.Petrogeochemistry shows that the protolith of monzogneiss is metaluminous A-type granite with some mantle-derived components which formed in continental crust extensional environment during post orogeny.LA-ICP-MS zircon U-Pb dating indicates two-stage age characteristics,in which the diagenetic age of 1.83-1.85 Ga suggests the protolith of monzogneiss formed in the Paleoproterozoic and the metamorphic age of 220-230 Ma shows the reworking of Indosinian metamorphism to Paleoproterozoic granite.It is the response to the subduction of Indo Pacific plate into South China plate during Indosinian,which provides new evidence for Indosinian orogeny in the southwestern Zhejiang.
引文
Bonin,B.,2007.A-Type Granites and Related Rocks:Evolution of a Concept,Problems and Prospects.Lithos,97(1-2):1-29.https://doi.org/10.1016/j.lithos.2006.12.007
Carswell,D.A.,Wilson,R.N.,Zhai,M.G.,et al.,2000.Metamorphic Evolution,Mineral Chemistry and Thermobarometry of Schists and Orthogneisses Hosting UltraHigh Pressure Eclogites in the Dabiesan of Central China.Lithos,52(1-4):121-155.https://doi.org/10.1016/S0024-4937(99)00088-2
Charvet,J.,Shu,L.S.,Shi,Y.S.,et al.,1996.The Building of South China:Collision of Yangzi and Cathaysia Blocks,Problems and Tentative Answers.Journal of Southeast Asian Earth Sciences,13(3-5):223-235.https://doi.org/10.1016/0743-9547(96)00029-3
Chen,D.Y.,Zhang,B.T.,Sun,D.Z.,et al.,1997.Geochemistry and Relation to Uranium Mineralization of Gaoxi and Fucheng Granites in Wuyi Mountains,China.Acta Petrologica Sinica,13(1):71-84(in Chinese with English abstract).
Chen,G.D.,1956.Examples of“Activizing Region”in the Chinese Platform with Special Reference to the“Cathaysia”Problem.Acta Geologica Sinica,36(3):239-271(in Chinese with English abstract).
Chen,W.F.,Chen,P.R.,Huang,H.Y.,et al.,2007.Chronological and Geochemical Studies of Granite and Enclave in Baimashan Pluton,Hunan,South China.Sciencein China(Series D),37(7):873-893(in Chinese).
Chen,Y.P.,Wei,C.J.,Zhang,J.R.,et al.,2015.Metamorphism and Zircon U-Pb Dating of Garnet Amphibolite in the Baoyintu Group,Inner Mongolia.Science Bulletin,60(19):1698-1707.https://doi.org/10.1007/s11434-015-0890-0
Connolly,J.A.D.,2005.Computation of Phase Equilibria by Linear Programming:A Tool for Geodynamic Modeling and Its Application to Subduction Zone Decarbonation.Earth and Planetary Science Letters,236(1-2):524-541.https://doi.org/10.1016/j.epsl.2005.04.033
Dall'Agnol,R.,de Oliveira,D.C.D.,2007.Oxidized,Magnetite-Series,Rapakivi-Type Granites of Carajás,Brazil:Implications for Classification and Petrogenesis of A-Type Granites.Lithos,93(3-4):215-233.https://doi.org/10.1016/j.lithos.2006.03.065
Ding,X.,Chen,P.R.,Chen,W.F.,et al.,2005.Single Zircon LA-ICPMS U-Pb Dating of Weishan Granite(Hunan,South China)and Its Petrogenetic Significance.Science in China(Series D),35(7):606-616(in Chinese).
Enami,M.,1998.Pressure-Temperature Path of Sanbagawa Prograde Metamorphism Deduced from Grossular Zoning of Garnet.Journal of Metamorphic Geology,16(1):97-106.https://doi.org/10.1111/j.1525-1314.1998.00058.x
Ferrari,O.M.,Hochard,C.,Stampfli,G.M.,2008.An Alternative Plate Tectonic Model for the Palaeozoic-Early Mesozoic Palaeotethyan Evolution of Southeast Asia(Northern Thailand-Burma).Tectonophysics,451(1-4):346-365.https://doi.org/10.1016/j.tecto.2007.11.065
Frost,B.R.,Barnes,C.G.,Collins,W.J.,et al.,2001.A Geochemical Classification for Granitic Rocks.Journal of Petrology,42(11):2033-2048.https://doi.org/10.1093/petrology/42.11.2033
Frost,C.D.,Frost,B.R.,1997.Reduced Rapakivi-Type Granites:The Tholeiite Connection.Geology,25(7):647.https://doi.org/10.1130/0091-7613(1997)025<0647:rrtgtt>2.3.co;2
Frost,C.D.,Frost,B.R.,2011.On Ferroan(A-Type)Granitoids:Their Compositional Variability and Modes of Origin.Journal of Petrology,52(1):39-53.https://doi.org/10.1093/petrology/egq070
Gan,X.C.,Li,H,M.,Sun,D.,Z,et al.,1995.A Geochronological Study on Early Proterozoic Granitic Rocks,Southeastern Zhejiang.Acta Petrologica et Mineralogica,14(1):1-8(in Chinese with English abstract).
Gan,X.C.,Li,H.M.,Sun,D.Z.,et al.,1993.Geochronological Study on the Precambrian Metamorphic Basement in Northern Fujian.Geology of Fujian,12(1):17-32(in Chinese with English abstract).
Garcia-Casco,A.,Torres-Roldan,R.L.,Millan,G.,et al.,2002.Oscillatory Zoning in Eclogitic Garnet and Amphibole,Northern Serpentinite Melange,Cuba:A Record of Tectonic Instability during Subduction?Journal of Metamorphic Geology,20(6):581-598.https://doi.org/10.1046/j.1525-1314.2002.00390.x
Gilder,S.A.,Gill,J.,Coe,R.S.,et al.,1996.Isotopic and Paleomagnetic Constraints on the Mesozoic Tectonic Evolution of South China.Journal of Geophysical Research:Solid Earth,101(B7):16137-16154.https://doi.org/10.1029/96jb00662
Grabau,A.W.,1924.Stratigraphy of China.Part I.Paleozoic and Older.The Geological Survey of Agriculture and Commerce,Beijing.
Guo,J.H.,Zhai,M.,G.,Li,Y.G.,et al.,1998.Cantrasting Metamorphic P-T Paths of Archaean High-Pressure Granulites from the North China Craton:Metamorphism and Tectonic Significance.Acta Petrologica Sinica,14(4):430-448(in Chinese with English abstract).
Guo,L.Z.,Shi,Y.S.,Ma,R.S.,1983.On the Formation and Evolution of the Mesozoic-Cenozoic Active Continental Margin and Island Arc Tectonics of the Western Pacific Ocean.Acta Geologica Sinica,57(1):11-21(in Chinese with English abstract).
Harris,N.B.W.,Pearce,J.A.,Tindle,A.G.,1986.Geochemical Characteristics of Collision Zone Magmatism.Geological Society,London,Special Publications,19(1):67-81.https://doi.org/10.1144/GSL.SP.1986.019.01.04
Henry,D.J.,Guidotti,C.V.,Thomson,J.A.,2005.The Ti-Saturation Surface for Low-to-Medium Pressure Metapelitic Biotites:Implications for Geothermometry and Ti-Substitution Mechanisms.American Mineralogist,90(2-3):316-328.https://doi.org/10.2138/am.2005.1498
Holdaway,M.J.,2000.Application of New Experimental and Garnet Margules Data to the Garnet-Biotite Geothermometer.American Mineralogist,85(7-8):881-892.https://doi.org/10.2138/am-2000-0701
Holland,T.,Blundy,J.,1994.Non-Ideal Interactions in Calcic Amphiboles and Their Bearing on Amphibole-Plagioclase Thermometry.Contributions to Mineralogy and Petrology,116(4):433-447.https://doi.org/10.1007/bf00310910
Holland,T.,Powell,R.,2003.Activity-Composition Relations for Phases in Petrological Calculations:An Asymmetric Multicomponent Formulation.Contributions to Mineralogy and Petrology,145(4):492-501.https://doi.org/10.1007/s00410-003-0464-z
Holland,T.J.B.,Powell,R.,1998.An Internally Consistent Thermodynamic Data Set for Phases of Petrological Interest.Journal of Metamorphic Geology,16(3):309-343.https://doi.org/10.1111/j.1525-1314.1998.00140.x
Hoskin,P.W.O.,2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62.https://doi.org/10.2113/0530027
Hoskin,P.W.O.,Ireland,T.R.,2000.Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator.Geology,28(7):627-630.https://doi.org/10.1130/0091-7613(2000)028<0627:reecoz>2.3.co;2
Hsü,K.J.,Li,J.L.,Chen,H.H.,et al.,1990.Tectonics of South China:Key to Understanding West Pacific Geology.Tectonophysics,183(1-4):9-39.https://doi.org/10.1016/0040-1951(90)90186-c
Hsü,K.J.,Sun,S.,Li,J.L.,et al.,1988.Mesozoic Overthrust Tectonics in South China.Geology,16(5):418.https://doi.org/10.1130/0091-7613(1988)016<0418:motisc>2.3.co;2
Hu,X.J.,Xu,J.K.,Tong,Z.X.,et al.,1991.The Precambrian Geology of Southwestern Zhejiang Province.Geological Publishing House,Beijing(in Chinese).
Huang,J.Q.,Ren,J.S.,Jiang,C.F.,et al.,1977.The Outline of the Tectonic Characteristics of China.Acta Geologica Sinica,51(2):117-135(in Chinese with English abstract).
Huang,J.Q.,Ren,J.S.,Jiang,C.F.,et al.,1980.The Tectonics and Evolution of Chinese Continent.Science Press,Beijing,99-102(in Chinese).
Jiang,Z.S.,Wang,G.D.,Xiao,L.L.,et al.,2011.Paleoproterozoic Metamorphic P-T-t Path and Tectonic Significance of the Luoning Metamorphic Complex at the Southern Terminal of the Trans-North China Orogen,Henan Province.Acta Petrologica Sinica,27(12):3701-3717(in Chinese with English abstract).
Jin,S.Q.,1991.Composition Characteristics of Calcic Amphibole from Different Regional Metamorphic Phases.Chinese Science Bulletin,36(11):851-854(in Chinese).
Kerr,A.,Fryer,B.J.,1993.Nd Isotope Evidence for Crust-Mantle Interaction in the Generation of A-Type Granitoid Suites in Labrador,Canada.Chemical Geology,104(1-4):39-60.https://doi.org/10.1016/0009-2541(93)90141-5
King,P.L.,White,A.J.R.,Chappell,B.W.,et al.,1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt,Southeastern Australia.Journal of Petrology,38(3):371-391.https://doi.org/10.1093/petroj/38.3.371
Kohn,M.J.,Spear,F.S.,1990.Two New Geobarometers for Garnet Amphibolites Gneisses,with Applications to Southeastern Vermont.American Mineralogist,75(1-2):89-96.https://doi.org/scopus/2-s2.0-0025205495
Leake,B.E.,Woolley,A.R.,Arps,C.E.S.,et al.,1997.Nomenclature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association,Commission on New Minerals and Mineral Names.The Canadian Mineralogist,35:219-246.
Li,X.H.,Li,J.Y.,Liu,Y.,et al.,1999.Geochemistry Characteristics of the Paleoproterozoic Meta-Volcanics in the Cathaysia Block and Its Tectonic Significance.Acta Petrologica Sinica,15(3):364-371(in Chinese with English abstract).
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2006.InitiationoftheIndosinian Orogeny in South China:Evidence for a Permian Magmatic Arc on Hainan Island.The Journal of Geology,114(3):341-353.https://doi.org/10.1086/501222
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2007.U-Pb Zircon,Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic I-and A-Type Granites from Central Guangdong,SE China:A Major Igneous Event in Response to Foundering of a Subducted Flat-Slab?Lithos,96(1-2):186-204.https://doi.org/10.1016/j.lithos.2006.09.018
Li,X.H.,Sun,M.,Wei,G.J.,et al.,2000.Geochemical and Sm-Nd Isotopic Study of Amphibolites in the Cathaysia Block,Southeastern China:Evidence for an Extremely Depleted Mantle in the Paleoproterozoic.Precambrian Research,102(3-4):251-262.https://doi.org/10.1016/s0301-9268(00)00067-x
Li,X.H.,Wang,Y.X.,Zhao,Z.H.,et al.,1998.SHRIMP U-Pb Zircon Geochronology for Amphibolite from the Pracambrian Basement in SW Zhejiang and NW Fujian Provinces.Geochimica,27(4):327-334(in Chinese with English abstract).
Li,Z.X.,Li,X.H.,2007.Formation of the 1300-km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China:A Flat-Slab Subduction Model.Geology,35(2):179.https://doi.org/10.1130/g23193a.1
Liu,R.,Zhou,H.W.,Zhang,L.,et al.,2009.Paleoproterozoic Reworking of Ancient Crust in the Cathaysia Block,South China:Evidence from Zircon Trace Elements,U-Pb and Lu-Hf Isotopes.Chinese Science Bulletin,54(9):1543-1554.https://doi.org/10.1007/s11434-009-0096-4
Ma,J.,Wang,R.M.,1997.P-T Evolution of Basic Granulite in Xuanhua and Miyun Based on Metamorphic Reaction Space.Science in China(Series D),27(1):52-58(in Chinese).
McDonough,W.F.,Sun,S.S.,1995.The Composition of the Earth.Chemical Geology,120(3-4):223-253.https://doi.org/10.1016/0009-2541(94)00140-4
Middlemost,E.A.K.,1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews,37(3-4):215-224.https://doi.org/10.1016/0012-8252(94)90029-9
Pearce,J.A.,1996.Sources and Settings of Granitic Rocks.Episodes,19(4):120-125.
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Qiu,Y.M.,Gao,S.,McNaughton,N.J.,et al.,2000.First Evidence of>3.2Ga Continental Crust in the Yangtze Craton of South China and Its Implications for Archean Crustal Evolution and Phanerozoic Tectonics.Geology,28(1):11-14.https://doi.org/10.1130/0091-7613(2000)028<0011:feogcc>2.3.co;2
Raase,P.,1974.Al and Ti Contents of Hornblende,Indicator of Pressure and Temperature of Regional Metamorphism.Contributions to Mineralogy and Petrology,45(3):231-236.
Ren,J.S.,1964.The Preliminary Study in a Few of Geotectonic Problem in Pre-Devonian,Southeast of China.Acta Geologica Sinica,44(4):418-431(in Chinese with Russian abstract).
Ren,J.S.,Chen,T.Y.,Niu,B.G.,1990.Continental Lithospheric Evolution and Mineralization in East China and Its Adjacent Areas.Science Press,Beijing(in Chinese).
Rodgers,J.,1989.Comment on“Mesozoic Overthrust Tectonics in South China”.Geology,17(7):671-672.https://doi.org/10.1130/0091-7613(1989)017<0669
Rowley,D.,Xue,F.,Tucker,R.,et al.,1997.Ages of Ultrahigh Pressure Metamorphism and Protolith Orthogneisses from the Eastern Dabie Shan:U/Pb Zircon Geochronology.Earth and Planetary Science Letters,151(3-4):191-203.https://doi.org/10.1016/S0012-821X(97)81848-1
Rubatto,D.,2002.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link between U-Pb Ages and Metamorphism.Chemical Geology,184(1-2):123-138.https://doi.org/10.1016/s0009-2541(01)00355-2
Shui,T.,1988.Tectonic Framework of the Continental Basement of Southeast China.Scientia Sinica(Series B),31(7):885-895(in Chinese).
Skjerlie,K.P.,Johnston,A.D.,1992.Vapor-Absent Melting at10kbar of a Biotite-and Amphibole-Bearing Tonalitic Gneiss:Implications for the Generation of A-Type Granites.Geology,20(3):263-266.https://doi.org/10.1130/0091-7613(1992)020<0263:va Mako>2.3.co;2
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Sun,Y.,Ma,C.Q.,Liu,Y.Y.,et al.,2011.Geochronological and Geochemical Constraints on the Petrogenesis of Late Triassic Aluminous A-Type Granites in Southeast China.Journal of Asian Earth Sciences,42(6):1117-1131.https://doi.org/10.1016/j.jseaes.2011.06.007
Sylvester,P.J.,1998.Post-Collisional Strongly Peraluminous Granites.Lithos,45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3
Taylor,S.R.,McLennan,S.M.,1985.The Continental Crust:Its Composition and Evolution.Blackwell Scientific Publication,London.
Turner,S.,Arnaud,N.,Liu,J.,et al.,1996.Post-Collision,Shoshonitic Volcanism on the Tibetan Plateau:Implications for Convective Thinning of the Lithosphere and the Source of Ocean Island Basalts.Journal of Petrology,37(1):45-71.https://doi.org/10.1093/petrology/37.1.45
Turner,S.P.,Foden,J.D.,Morrison,R.S.,1992.Derivation of Some A-Type Magmas by Fractionation of Basaltic Magma:An Example from the Padthaway Ridge,South Australia.Lithos,28(2):151-179.https://doi.org/10.1016/0024-4937(92)90029-x
Wang,L.J.,Yu,J.H.,Xu,X.S.,et al.,2007.Formation Age and Origin of the Gutian-Xiaotao Granitic Complex in the Southwestern Fujian Province,China.Acta Petrologica Sinica,23(6):1470-1484(in Chinese with English abstract).
Wang,Q.,Li,J.W.,Jian,P.,et al.,2005.Alkaline Syenites in Eastern Cathaysia(South China):Link to PermianTriassic Transtension.Earth and Planetary Science Letters,230(3-4):339-354.https://doi.org/10.1016/j.epsl.2004.11.023
Wang,X.,Chen,J.,Luo,D.,2008.Study on Petrogenesis of Zircons from the Danzhu Granodiorite and Its Geological Implications.Geological Review,54(3):387-398(in Chinese with English abstract).
Wang,Y.J.,Fan,W.M.,Sun,M.,et al.,2007.Geochronological,Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block:A Case Study in the Hunan Province.Lithos,96(3-4):475-502.https://doi.org/10.1016/j.lithos.2006.11.010
Wang,Y.J.,Zhang,Y.,Fan,W.M.,et al.,2002.Numerical Modeling of the Formation of Indo-Sinian Peraluminous Granitoids in Hunan Province:Basaltic Underplating versus Tectonic Thickening.Science China Earth Science,45(11):1042-1056.https://doi.org/10.1007/bf02911241
Wang,Y.X.,Zhao,Z.H.,Bao,Z.W.,et al.,1998.Geochemistry of Granitoid Rocks and Crustal Evolution,Zhejiang Province China-Ⅱ.Proterozoic Granitoid Rocks.Geochimica,26(6):57-68(in Chinese with English abstract).
Wang,Z.M.,Xiao,W.J.,Han,C.M.,et al.,2013.Metamorphism,Zircon U-Pb Dating and Tectonic Implications of Garnet Amphibolites from Hongliuxia,Dunhuang,Gansu Province.Acta Petrologica Sinica,29(5):1685-1697(in Chinese with English abstract).
Wei,C.J.,2016.Granulite Facies Metamorphism and Petrogenesis of Granite(Ⅱ):Quantitative Modeling of the HT-UHTPhase Equilibria for Metapelites and the Petrogenesis of S-Type Granite.Acta Petrologica Sinica,32(6):1611-1624(in Chinese with English abstract).
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Wu,C.M.,Zhang,J.,Ren,L.D.,2004.Empirical Garnet-Biotite-Plagioclase-Quartz(GBPQ)Geobarometry in Medium-to HighGrade Metapelites.Journal of Petrology,45(9):1907-1921.https://doi.org/10.1093/petrology/egh038
Wu,S.P.,Wang,M.Y.,Qi,K.J.,2007.Present Situation of Researches on A-Type Granites:A Review.Acta Petrologica et Mineralogica,26(1):57-66(in Chinese with English abstract).
Wu,Y.B.,Zheng,Y.F.,2004.Genetic Mineralogy of Zircon and Its Constraints on the Interpretation of U-Pb Age.Chinese Science Bulletin,49(16):1589-1604(in Chinese).
Xia,Y.,Xu,X.S.,Zhu,K.Y.,2012.Paleoproterozoic S-and A-Type Granites in Southwestern Zhejiang:Magmatism,Metamorphism and Implications for the Crustal Evolution of the Cathaysia Basement.Precambrian Research,216-219:177-207.https://doi.org/10.1016/j.precamres.2012.07.001
Xiang,H.,Zhang,L.,Zhou,H.W.,et al.,2008.U-Pb Zircon Geochronology and Hf Isotope Study of Metamorphosed BasicUltrabasic Rocks from Metamorphic Basement in Southwestern Zhejiang:The Response of the Cathaysia Block to Indosinian Orogenic Event.Science in China(Series D),38(4):401-413(in Chinese).
Xiao,L.L.,Jiang,Z.S.,Wang,G.D.,et al.,2011.Metamorphic Reaction Textures and Metamorphic P-T-t Loops of the Precambrian Zanhuang Metamorphic Complex,Hebei,North China.Acta Petrologica Sinica,27(4):980-1002(in Chinese with English abstract).
Xie,J.R.,1961.China's Tectonic Problems.Acta Geologica Sinica,41(2):218-239(in Chinese).
Xu,X.S.,O'Reilly,S.Y.,Griffin,W.L.,et al.,2007.The Crust of Cathaysia:Age,Assembly and Reworking of Two Terranes.Precambrian Research,158(1-2):51-78.https://doi.org/10.1016/j.precamres.2007.04.010
Yu,J.H.,O'Reilly,S.Y.,Zhou,M.F.,et al.,2012.U-Pb Geochronology and Hf-Nd Isotopic Geochemistry of the Badu Complex,Southeastern China:Implications for the Precambrian Crustal Evolution and Paleogeography of the Cathaysia Block.Precambrian Research,222-223:424-449.https://doi.org/10.1016/j.precamres.2011.07.014
Yu,J.H.,Wang,L.J.,O'Reilly,S.Y.,et al.,2009.A Paleoproterozoic Orogeny Recorded in a Long-Lived Cratonic Remnant(Wuyishan Terrane),Eastern Cathaysia Block,China.Precambrian Research,174(3-4):347-363.https://doi.org/10.1016/j.precamres.2009.08.009
Zhang,S.B.,Zheng,Y.F.,Wu,Y.B.,et al.,2006.Zircon Isotope Evidence for≥3.5Ga Continental Crust in the Yangtze Craton of China.Precambrian Research,146(1-2):16-34.https://doi.org/10.1016/j.precamres.2006.01.002
Zhang,W.Y.,1959.Outline of China's Geodetic Structure.Science Press,Beijing(in Chinese).
Zhang,Y.Q.,Xu,X.B.,Jia,D.,et al.,2009.Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic.Earth Science Frontiers,16(1):234-247(in Chinese with English abstract).
Zhao,L.,Zhai,M.G.,Santosh,M.,et al.,2017.Early Mesozoic Retrograded Eclogite and Mafic Granulite from the Badu Complex of the Cathaysia Block,South China:Petrology and Tectonic Implications.Gondwana Research,42:84-103.https://doi.org/10.1016/j.gr.2016.10.002
Zhao,L.,Zhou,X.W.,2012.The Metamorphic Evolution and PTPath of Pelitic Granulite from the Badu Group in Southwestern Zhejiang Province.Acta Petrologica et Mineralogica,31(1):61-72(in Chinese with English abstract).
Zhao,L.,Zhou,X.W.,Zhai,M.G.,et al.,2014.Paleoproterozoic Tectonic Transition from Collision to Extension in the Eastern Cathaysia Block,South China:Evidence from Geochemistry,Zircon U-Pb Geochronology and Nd-Hf Isotopes of a Granite-Charnockite Suite in Southwestern Zhejiang.Lithos,184-187:259-280.https://doi.org/10.1016/j.lithos.2013.11.005
Zheng,J.P.,Griffin,W.L.,O'Reilly,S.Y.,et al.,2006.Widespread Archean Basement beneath the Yangtze Craton.Geology,34(6):417.https://doi.org/10.1130/g22282.1
Zhou,X.M.,Sun,T.,Shen,W.Z.,2006.Petrogenesis of Mesozoic Granitioids and Volcanic Rocks in South China:AResponse to Tectonic Evolution.Episodes,29:26-33(in Chinese with English abstract).
陈迪云,章邦桐,孙大中,等,1997.武夷山高溪和富城花岗岩体地球化学及其与铀成矿的关系.岩石学报,13(1):71-84.
陈国达,1956.中国地台“活化区”的实例并着重讨论“华夏古陆”问题.地质学报,36(3):239-271.
陈卫锋,陈培荣,黄宏业,等,2007.湖南白马山岩体花岗岩及其包体的年代学和地球化学研究.中国科学(D辑),37(7):873-893.
丁兴,陈培荣,陈卫锋,等,2005.湖南沩山花岗岩中锆石LA-ICPMSU-Pb定年:成岩启示和意义.中国科学(D辑),35(7):606-616.
甘晓春,李惠民,孙大中,等,1993.闽北前寒武纪基底的地质年代学研究.福建地质,12(1):17-13.
甘晓春,李惠民,孙大中,等,1995.浙西南早元古代花岗质岩石的年代.岩石矿物学杂志,14(1):1-8.
郭敬辉,翟明国,李永刚,等,1998.华北太古宙高压基性麻粒岩的两类PT轨迹及其构造意义:矿物化学和变质作用研究.岩石学报,14(4):430-448.
郭令智,施央申,马瑞士,1983.西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化.地质学报,57(1):11-21.
胡雄健,许金坤,童朝旭,等,1991.浙西南前寒武纪地质.北京:地质出版社.
黄汲清,任纪舜,姜春发,等,1977.中国大地构造基本轮廓.地质学报,51(2):117-135.
黄汲清,任纪舜,姜春发,等,1980.中国大地构造及其演化.北京:科学出版社,99-102.
蒋宗胜,王国栋,肖玲玲,等,2011.河南洛宁太华变质杂岩区早元古代变质作用P-T-t轨迹及其大地构造意义.岩石学报,27(12):3701-3717.
靳是琴,1991.不同区域变质相中钙质角闪石的成分特征.科学通报,36(11):851-854.
李献华,李寄嵎,刘颖,等,1999.华夏古陆古元古代变质火山岩的地球化学特征及其构造意义.岩石学报.15(3):364-371.
李献华,王一先,赵振华,等,1998.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学.27(4):327-334.
马军,王仁民,1997.从变质反应空间看宣化、密云两地基性麻粒岩不同的P-T演化.中国科学(D辑),27(1):52-58.
任纪舜,1964.中国东南部泥盆纪前几个大地构造问题的初步探讨.地质学报,44(4):418-431.
任纪舜,陈廷愚,牛宝贵,1990.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社.
水涛,1988.中国东南大陆基底构造格局.中国科学(B辑),31(7):885-896.
王丽娟,于津海,徐夕生,等,2007.闽西南古田-小陶花岗质杂岩体的形成时代和成因.岩石学报,23(6):1470-1484.
汪相,陈洁,罗丹,2008.浙西南淡竹花岗闪长岩中锆石的成因研究及其地质意义.地质评论,54(3):387-398.
王一先,赵振华,包志伟,等,1998.浙江花岗岩类地球化学与地壳演化-Ⅱ.元古宙花岗岩类,地球化学,26(6):57-68.
王忠梅,肖文交,韩春明,等,2013.甘肃敦煌红柳峡地区石榴石斜长角闪岩的变质特征、锆石U-Pb年龄及地质意义.岩石学报,29(5):1685-1697.
魏春景,2016.麻粒岩相变质作用与花岗岩成因-Ⅱ:变质泥质岩高温-超高温变质相平衡与S型花岗岩成因的定量模拟.岩石学报,32(6):1611-1624.
吴锁平,王梅英,戚开静,2007.A型花岗岩研究现状及其述评.岩石矿物学杂志,26(1):57-66.
吴元保,郑永飞,2004,锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
向华,张利,周汉文,等,2008.浙西南变质基底基性-超基性变质岩锆石U-Pb年龄、Hf同位素研究:华厦地块变质基底对华南印支期造山的响应.中国科学(D辑),38(4):401-413.
肖玲玲,蒋宗胜,王国栋,等,2011.赞皇前寒武纪变质杂岩区变质反应结构与变质作用P-T-t轨迹.岩石学报,27(4):980-1002.
谢家荣,1961.中国大地构造问题.地质学报,41(2):218-239.
张文佑,1959.中国大地构造纲要.北京:科学出版社.
张岳桥,徐先兵,贾东,等,2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘,16(1):234-247.
赵磊,周喜文,2012.浙西南八都群泥质麻粒岩的变质演化与PT轨迹.岩石矿物学杂志,31(1):61-72.
周新民,孙涛,沈渭洲,2006.华南中生代花岗岩-火山岩成因与构造体制转换.地质幕,29:26-33.
Carswell,D.A.,Wilson,R.N.,Zhai,M.G.,et al.,2000.Metamorphic Evolution,Mineral Chemistry and Thermobarometry of Schists and Orthogneisses Hosting UltraHigh Pressure Eclogites in the Dabiesan of Central China.Lithos,52(1-4):121-155.https://doi.org/10.1016/S0024-4937(99)00088-2
Charvet,J.,Shu,L.S.,Shi,Y.S.,et al.,1996.The Building of South China:Collision of Yangzi and Cathaysia Blocks,Problems and Tentative Answers.Journal of Southeast Asian Earth Sciences,13(3-5):223-235.https://doi.org/10.1016/0743-9547(96)00029-3
Chen,D.Y.,Zhang,B.T.,Sun,D.Z.,et al.,1997.Geochemistry and Relation to Uranium Mineralization of Gaoxi and Fucheng Granites in Wuyi Mountains,China.Acta Petrologica Sinica,13(1):71-84(in Chinese with English abstract).
Chen,G.D.,1956.Examples of“Activizing Region”in the Chinese Platform with Special Reference to the“Cathaysia”Problem.Acta Geologica Sinica,36(3):239-271(in Chinese with English abstract).
Chen,W.F.,Chen,P.R.,Huang,H.Y.,et al.,2007.Chronological and Geochemical Studies of Granite and Enclave in Baimashan Pluton,Hunan,South China.Sciencein China(Series D),37(7):873-893(in Chinese).
Chen,Y.P.,Wei,C.J.,Zhang,J.R.,et al.,2015.Metamorphism and Zircon U-Pb Dating of Garnet Amphibolite in the Baoyintu Group,Inner Mongolia.Science Bulletin,60(19):1698-1707.https://doi.org/10.1007/s11434-015-0890-0
Connolly,J.A.D.,2005.Computation of Phase Equilibria by Linear Programming:A Tool for Geodynamic Modeling and Its Application to Subduction Zone Decarbonation.Earth and Planetary Science Letters,236(1-2):524-541.https://doi.org/10.1016/j.epsl.2005.04.033
Dall'Agnol,R.,de Oliveira,D.C.D.,2007.Oxidized,Magnetite-Series,Rapakivi-Type Granites of Carajás,Brazil:Implications for Classification and Petrogenesis of A-Type Granites.Lithos,93(3-4):215-233.https://doi.org/10.1016/j.lithos.2006.03.065
Ding,X.,Chen,P.R.,Chen,W.F.,et al.,2005.Single Zircon LA-ICPMS U-Pb Dating of Weishan Granite(Hunan,South China)and Its Petrogenetic Significance.Science in China(Series D),35(7):606-616(in Chinese).
Enami,M.,1998.Pressure-Temperature Path of Sanbagawa Prograde Metamorphism Deduced from Grossular Zoning of Garnet.Journal of Metamorphic Geology,16(1):97-106.https://doi.org/10.1111/j.1525-1314.1998.00058.x
Ferrari,O.M.,Hochard,C.,Stampfli,G.M.,2008.An Alternative Plate Tectonic Model for the Palaeozoic-Early Mesozoic Palaeotethyan Evolution of Southeast Asia(Northern Thailand-Burma).Tectonophysics,451(1-4):346-365.https://doi.org/10.1016/j.tecto.2007.11.065
Frost,B.R.,Barnes,C.G.,Collins,W.J.,et al.,2001.A Geochemical Classification for Granitic Rocks.Journal of Petrology,42(11):2033-2048.https://doi.org/10.1093/petrology/42.11.2033
Frost,C.D.,Frost,B.R.,1997.Reduced Rapakivi-Type Granites:The Tholeiite Connection.Geology,25(7):647.https://doi.org/10.1130/0091-7613(1997)025<0647:rrtgtt>2.3.co;2
Frost,C.D.,Frost,B.R.,2011.On Ferroan(A-Type)Granitoids:Their Compositional Variability and Modes of Origin.Journal of Petrology,52(1):39-53.https://doi.org/10.1093/petrology/egq070
Gan,X.C.,Li,H,M.,Sun,D.,Z,et al.,1995.A Geochronological Study on Early Proterozoic Granitic Rocks,Southeastern Zhejiang.Acta Petrologica et Mineralogica,14(1):1-8(in Chinese with English abstract).
Gan,X.C.,Li,H.M.,Sun,D.Z.,et al.,1993.Geochronological Study on the Precambrian Metamorphic Basement in Northern Fujian.Geology of Fujian,12(1):17-32(in Chinese with English abstract).
Garcia-Casco,A.,Torres-Roldan,R.L.,Millan,G.,et al.,2002.Oscillatory Zoning in Eclogitic Garnet and Amphibole,Northern Serpentinite Melange,Cuba:A Record of Tectonic Instability during Subduction?Journal of Metamorphic Geology,20(6):581-598.https://doi.org/10.1046/j.1525-1314.2002.00390.x
Gilder,S.A.,Gill,J.,Coe,R.S.,et al.,1996.Isotopic and Paleomagnetic Constraints on the Mesozoic Tectonic Evolution of South China.Journal of Geophysical Research:Solid Earth,101(B7):16137-16154.https://doi.org/10.1029/96jb00662
Grabau,A.W.,1924.Stratigraphy of China.Part I.Paleozoic and Older.The Geological Survey of Agriculture and Commerce,Beijing.
Guo,J.H.,Zhai,M.,G.,Li,Y.G.,et al.,1998.Cantrasting Metamorphic P-T Paths of Archaean High-Pressure Granulites from the North China Craton:Metamorphism and Tectonic Significance.Acta Petrologica Sinica,14(4):430-448(in Chinese with English abstract).
Guo,L.Z.,Shi,Y.S.,Ma,R.S.,1983.On the Formation and Evolution of the Mesozoic-Cenozoic Active Continental Margin and Island Arc Tectonics of the Western Pacific Ocean.Acta Geologica Sinica,57(1):11-21(in Chinese with English abstract).
Harris,N.B.W.,Pearce,J.A.,Tindle,A.G.,1986.Geochemical Characteristics of Collision Zone Magmatism.Geological Society,London,Special Publications,19(1):67-81.https://doi.org/10.1144/GSL.SP.1986.019.01.04
Henry,D.J.,Guidotti,C.V.,Thomson,J.A.,2005.The Ti-Saturation Surface for Low-to-Medium Pressure Metapelitic Biotites:Implications for Geothermometry and Ti-Substitution Mechanisms.American Mineralogist,90(2-3):316-328.https://doi.org/10.2138/am.2005.1498
Holdaway,M.J.,2000.Application of New Experimental and Garnet Margules Data to the Garnet-Biotite Geothermometer.American Mineralogist,85(7-8):881-892.https://doi.org/10.2138/am-2000-0701
Holland,T.,Blundy,J.,1994.Non-Ideal Interactions in Calcic Amphiboles and Their Bearing on Amphibole-Plagioclase Thermometry.Contributions to Mineralogy and Petrology,116(4):433-447.https://doi.org/10.1007/bf00310910
Holland,T.,Powell,R.,2003.Activity-Composition Relations for Phases in Petrological Calculations:An Asymmetric Multicomponent Formulation.Contributions to Mineralogy and Petrology,145(4):492-501.https://doi.org/10.1007/s00410-003-0464-z
Holland,T.J.B.,Powell,R.,1998.An Internally Consistent Thermodynamic Data Set for Phases of Petrological Interest.Journal of Metamorphic Geology,16(3):309-343.https://doi.org/10.1111/j.1525-1314.1998.00140.x
Hoskin,P.W.O.,2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62.https://doi.org/10.2113/0530027
Hoskin,P.W.O.,Ireland,T.R.,2000.Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator.Geology,28(7):627-630.https://doi.org/10.1130/0091-7613(2000)028<0627:reecoz>2.3.co;2
Hsü,K.J.,Li,J.L.,Chen,H.H.,et al.,1990.Tectonics of South China:Key to Understanding West Pacific Geology.Tectonophysics,183(1-4):9-39.https://doi.org/10.1016/0040-1951(90)90186-c
Hsü,K.J.,Sun,S.,Li,J.L.,et al.,1988.Mesozoic Overthrust Tectonics in South China.Geology,16(5):418.https://doi.org/10.1130/0091-7613(1988)016<0418:motisc>2.3.co;2
Hu,X.J.,Xu,J.K.,Tong,Z.X.,et al.,1991.The Precambrian Geology of Southwestern Zhejiang Province.Geological Publishing House,Beijing(in Chinese).
Huang,J.Q.,Ren,J.S.,Jiang,C.F.,et al.,1977.The Outline of the Tectonic Characteristics of China.Acta Geologica Sinica,51(2):117-135(in Chinese with English abstract).
Huang,J.Q.,Ren,J.S.,Jiang,C.F.,et al.,1980.The Tectonics and Evolution of Chinese Continent.Science Press,Beijing,99-102(in Chinese).
Jiang,Z.S.,Wang,G.D.,Xiao,L.L.,et al.,2011.Paleoproterozoic Metamorphic P-T-t Path and Tectonic Significance of the Luoning Metamorphic Complex at the Southern Terminal of the Trans-North China Orogen,Henan Province.Acta Petrologica Sinica,27(12):3701-3717(in Chinese with English abstract).
Jin,S.Q.,1991.Composition Characteristics of Calcic Amphibole from Different Regional Metamorphic Phases.Chinese Science Bulletin,36(11):851-854(in Chinese).
Kerr,A.,Fryer,B.J.,1993.Nd Isotope Evidence for Crust-Mantle Interaction in the Generation of A-Type Granitoid Suites in Labrador,Canada.Chemical Geology,104(1-4):39-60.https://doi.org/10.1016/0009-2541(93)90141-5
King,P.L.,White,A.J.R.,Chappell,B.W.,et al.,1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt,Southeastern Australia.Journal of Petrology,38(3):371-391.https://doi.org/10.1093/petroj/38.3.371
Kohn,M.J.,Spear,F.S.,1990.Two New Geobarometers for Garnet Amphibolites Gneisses,with Applications to Southeastern Vermont.American Mineralogist,75(1-2):89-96.https://doi.org/scopus/2-s2.0-0025205495
Leake,B.E.,Woolley,A.R.,Arps,C.E.S.,et al.,1997.Nomenclature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association,Commission on New Minerals and Mineral Names.The Canadian Mineralogist,35:219-246.
Li,X.H.,Li,J.Y.,Liu,Y.,et al.,1999.Geochemistry Characteristics of the Paleoproterozoic Meta-Volcanics in the Cathaysia Block and Its Tectonic Significance.Acta Petrologica Sinica,15(3):364-371(in Chinese with English abstract).
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2006.InitiationoftheIndosinian Orogeny in South China:Evidence for a Permian Magmatic Arc on Hainan Island.The Journal of Geology,114(3):341-353.https://doi.org/10.1086/501222
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2007.U-Pb Zircon,Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic I-and A-Type Granites from Central Guangdong,SE China:A Major Igneous Event in Response to Foundering of a Subducted Flat-Slab?Lithos,96(1-2):186-204.https://doi.org/10.1016/j.lithos.2006.09.018
Li,X.H.,Sun,M.,Wei,G.J.,et al.,2000.Geochemical and Sm-Nd Isotopic Study of Amphibolites in the Cathaysia Block,Southeastern China:Evidence for an Extremely Depleted Mantle in the Paleoproterozoic.Precambrian Research,102(3-4):251-262.https://doi.org/10.1016/s0301-9268(00)00067-x
Li,X.H.,Wang,Y.X.,Zhao,Z.H.,et al.,1998.SHRIMP U-Pb Zircon Geochronology for Amphibolite from the Pracambrian Basement in SW Zhejiang and NW Fujian Provinces.Geochimica,27(4):327-334(in Chinese with English abstract).
Li,Z.X.,Li,X.H.,2007.Formation of the 1300-km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China:A Flat-Slab Subduction Model.Geology,35(2):179.https://doi.org/10.1130/g23193a.1
Liu,R.,Zhou,H.W.,Zhang,L.,et al.,2009.Paleoproterozoic Reworking of Ancient Crust in the Cathaysia Block,South China:Evidence from Zircon Trace Elements,U-Pb and Lu-Hf Isotopes.Chinese Science Bulletin,54(9):1543-1554.https://doi.org/10.1007/s11434-009-0096-4
Ma,J.,Wang,R.M.,1997.P-T Evolution of Basic Granulite in Xuanhua and Miyun Based on Metamorphic Reaction Space.Science in China(Series D),27(1):52-58(in Chinese).
McDonough,W.F.,Sun,S.S.,1995.The Composition of the Earth.Chemical Geology,120(3-4):223-253.https://doi.org/10.1016/0009-2541(94)00140-4
Middlemost,E.A.K.,1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews,37(3-4):215-224.https://doi.org/10.1016/0012-8252(94)90029-9
Pearce,J.A.,1996.Sources and Settings of Granitic Rocks.Episodes,19(4):120-125.
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Qiu,Y.M.,Gao,S.,McNaughton,N.J.,et al.,2000.First Evidence of>3.2Ga Continental Crust in the Yangtze Craton of South China and Its Implications for Archean Crustal Evolution and Phanerozoic Tectonics.Geology,28(1):11-14.https://doi.org/10.1130/0091-7613(2000)028<0011:feogcc>2.3.co;2
Raase,P.,1974.Al and Ti Contents of Hornblende,Indicator of Pressure and Temperature of Regional Metamorphism.Contributions to Mineralogy and Petrology,45(3):231-236.
Ren,J.S.,1964.The Preliminary Study in a Few of Geotectonic Problem in Pre-Devonian,Southeast of China.Acta Geologica Sinica,44(4):418-431(in Chinese with Russian abstract).
Ren,J.S.,Chen,T.Y.,Niu,B.G.,1990.Continental Lithospheric Evolution and Mineralization in East China and Its Adjacent Areas.Science Press,Beijing(in Chinese).
Rodgers,J.,1989.Comment on“Mesozoic Overthrust Tectonics in South China”.Geology,17(7):671-672.https://doi.org/10.1130/0091-7613(1989)017<0669
Rowley,D.,Xue,F.,Tucker,R.,et al.,1997.Ages of Ultrahigh Pressure Metamorphism and Protolith Orthogneisses from the Eastern Dabie Shan:U/Pb Zircon Geochronology.Earth and Planetary Science Letters,151(3-4):191-203.https://doi.org/10.1016/S0012-821X(97)81848-1
Rubatto,D.,2002.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link between U-Pb Ages and Metamorphism.Chemical Geology,184(1-2):123-138.https://doi.org/10.1016/s0009-2541(01)00355-2
Shui,T.,1988.Tectonic Framework of the Continental Basement of Southeast China.Scientia Sinica(Series B),31(7):885-895(in Chinese).
Skjerlie,K.P.,Johnston,A.D.,1992.Vapor-Absent Melting at10kbar of a Biotite-and Amphibole-Bearing Tonalitic Gneiss:Implications for the Generation of A-Type Granites.Geology,20(3):263-266.https://doi.org/10.1130/0091-7613(1992)020<0263:va Mako>2.3.co;2
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Sun,Y.,Ma,C.Q.,Liu,Y.Y.,et al.,2011.Geochronological and Geochemical Constraints on the Petrogenesis of Late Triassic Aluminous A-Type Granites in Southeast China.Journal of Asian Earth Sciences,42(6):1117-1131.https://doi.org/10.1016/j.jseaes.2011.06.007
Sylvester,P.J.,1998.Post-Collisional Strongly Peraluminous Granites.Lithos,45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3
Taylor,S.R.,McLennan,S.M.,1985.The Continental Crust:Its Composition and Evolution.Blackwell Scientific Publication,London.
Turner,S.,Arnaud,N.,Liu,J.,et al.,1996.Post-Collision,Shoshonitic Volcanism on the Tibetan Plateau:Implications for Convective Thinning of the Lithosphere and the Source of Ocean Island Basalts.Journal of Petrology,37(1):45-71.https://doi.org/10.1093/petrology/37.1.45
Turner,S.P.,Foden,J.D.,Morrison,R.S.,1992.Derivation of Some A-Type Magmas by Fractionation of Basaltic Magma:An Example from the Padthaway Ridge,South Australia.Lithos,28(2):151-179.https://doi.org/10.1016/0024-4937(92)90029-x
Wang,L.J.,Yu,J.H.,Xu,X.S.,et al.,2007.Formation Age and Origin of the Gutian-Xiaotao Granitic Complex in the Southwestern Fujian Province,China.Acta Petrologica Sinica,23(6):1470-1484(in Chinese with English abstract).
Wang,Q.,Li,J.W.,Jian,P.,et al.,2005.Alkaline Syenites in Eastern Cathaysia(South China):Link to PermianTriassic Transtension.Earth and Planetary Science Letters,230(3-4):339-354.https://doi.org/10.1016/j.epsl.2004.11.023
Wang,X.,Chen,J.,Luo,D.,2008.Study on Petrogenesis of Zircons from the Danzhu Granodiorite and Its Geological Implications.Geological Review,54(3):387-398(in Chinese with English abstract).
Wang,Y.J.,Fan,W.M.,Sun,M.,et al.,2007.Geochronological,Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block:A Case Study in the Hunan Province.Lithos,96(3-4):475-502.https://doi.org/10.1016/j.lithos.2006.11.010
Wang,Y.J.,Zhang,Y.,Fan,W.M.,et al.,2002.Numerical Modeling of the Formation of Indo-Sinian Peraluminous Granitoids in Hunan Province:Basaltic Underplating versus Tectonic Thickening.Science China Earth Science,45(11):1042-1056.https://doi.org/10.1007/bf02911241
Wang,Y.X.,Zhao,Z.H.,Bao,Z.W.,et al.,1998.Geochemistry of Granitoid Rocks and Crustal Evolution,Zhejiang Province China-Ⅱ.Proterozoic Granitoid Rocks.Geochimica,26(6):57-68(in Chinese with English abstract).
Wang,Z.M.,Xiao,W.J.,Han,C.M.,et al.,2013.Metamorphism,Zircon U-Pb Dating and Tectonic Implications of Garnet Amphibolites from Hongliuxia,Dunhuang,Gansu Province.Acta Petrologica Sinica,29(5):1685-1697(in Chinese with English abstract).
Wei,C.J.,2016.Granulite Facies Metamorphism and Petrogenesis of Granite(Ⅱ):Quantitative Modeling of the HT-UHTPhase Equilibria for Metapelites and the Petrogenesis of S-Type Granite.Acta Petrologica Sinica,32(6):1611-1624(in Chinese with English abstract).
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Wu,C.M.,Zhang,J.,Ren,L.D.,2004.Empirical Garnet-Biotite-Plagioclase-Quartz(GBPQ)Geobarometry in Medium-to HighGrade Metapelites.Journal of Petrology,45(9):1907-1921.https://doi.org/10.1093/petrology/egh038
Wu,S.P.,Wang,M.Y.,Qi,K.J.,2007.Present Situation of Researches on A-Type Granites:A Review.Acta Petrologica et Mineralogica,26(1):57-66(in Chinese with English abstract).
Wu,Y.B.,Zheng,Y.F.,2004.Genetic Mineralogy of Zircon and Its Constraints on the Interpretation of U-Pb Age.Chinese Science Bulletin,49(16):1589-1604(in Chinese).
Xia,Y.,Xu,X.S.,Zhu,K.Y.,2012.Paleoproterozoic S-and A-Type Granites in Southwestern Zhejiang:Magmatism,Metamorphism and Implications for the Crustal Evolution of the Cathaysia Basement.Precambrian Research,216-219:177-207.https://doi.org/10.1016/j.precamres.2012.07.001
Xiang,H.,Zhang,L.,Zhou,H.W.,et al.,2008.U-Pb Zircon Geochronology and Hf Isotope Study of Metamorphosed BasicUltrabasic Rocks from Metamorphic Basement in Southwestern Zhejiang:The Response of the Cathaysia Block to Indosinian Orogenic Event.Science in China(Series D),38(4):401-413(in Chinese).
Xiao,L.L.,Jiang,Z.S.,Wang,G.D.,et al.,2011.Metamorphic Reaction Textures and Metamorphic P-T-t Loops of the Precambrian Zanhuang Metamorphic Complex,Hebei,North China.Acta Petrologica Sinica,27(4):980-1002(in Chinese with English abstract).
Xie,J.R.,1961.China's Tectonic Problems.Acta Geologica Sinica,41(2):218-239(in Chinese).
Xu,X.S.,O'Reilly,S.Y.,Griffin,W.L.,et al.,2007.The Crust of Cathaysia:Age,Assembly and Reworking of Two Terranes.Precambrian Research,158(1-2):51-78.https://doi.org/10.1016/j.precamres.2007.04.010
Yu,J.H.,O'Reilly,S.Y.,Zhou,M.F.,et al.,2012.U-Pb Geochronology and Hf-Nd Isotopic Geochemistry of the Badu Complex,Southeastern China:Implications for the Precambrian Crustal Evolution and Paleogeography of the Cathaysia Block.Precambrian Research,222-223:424-449.https://doi.org/10.1016/j.precamres.2011.07.014
Yu,J.H.,Wang,L.J.,O'Reilly,S.Y.,et al.,2009.A Paleoproterozoic Orogeny Recorded in a Long-Lived Cratonic Remnant(Wuyishan Terrane),Eastern Cathaysia Block,China.Precambrian Research,174(3-4):347-363.https://doi.org/10.1016/j.precamres.2009.08.009
Zhang,S.B.,Zheng,Y.F.,Wu,Y.B.,et al.,2006.Zircon Isotope Evidence for≥3.5Ga Continental Crust in the Yangtze Craton of China.Precambrian Research,146(1-2):16-34.https://doi.org/10.1016/j.precamres.2006.01.002
Zhang,W.Y.,1959.Outline of China's Geodetic Structure.Science Press,Beijing(in Chinese).
Zhang,Y.Q.,Xu,X.B.,Jia,D.,et al.,2009.Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic.Earth Science Frontiers,16(1):234-247(in Chinese with English abstract).
Zhao,L.,Zhai,M.G.,Santosh,M.,et al.,2017.Early Mesozoic Retrograded Eclogite and Mafic Granulite from the Badu Complex of the Cathaysia Block,South China:Petrology and Tectonic Implications.Gondwana Research,42:84-103.https://doi.org/10.1016/j.gr.2016.10.002
Zhao,L.,Zhou,X.W.,2012.The Metamorphic Evolution and PTPath of Pelitic Granulite from the Badu Group in Southwestern Zhejiang Province.Acta Petrologica et Mineralogica,31(1):61-72(in Chinese with English abstract).
Zhao,L.,Zhou,X.W.,Zhai,M.G.,et al.,2014.Paleoproterozoic Tectonic Transition from Collision to Extension in the Eastern Cathaysia Block,South China:Evidence from Geochemistry,Zircon U-Pb Geochronology and Nd-Hf Isotopes of a Granite-Charnockite Suite in Southwestern Zhejiang.Lithos,184-187:259-280.https://doi.org/10.1016/j.lithos.2013.11.005
Zheng,J.P.,Griffin,W.L.,O'Reilly,S.Y.,et al.,2006.Widespread Archean Basement beneath the Yangtze Craton.Geology,34(6):417.https://doi.org/10.1130/g22282.1
Zhou,X.M.,Sun,T.,Shen,W.Z.,2006.Petrogenesis of Mesozoic Granitioids and Volcanic Rocks in South China:AResponse to Tectonic Evolution.Episodes,29:26-33(in Chinese with English abstract).
陈迪云,章邦桐,孙大中,等,1997.武夷山高溪和富城花岗岩体地球化学及其与铀成矿的关系.岩石学报,13(1):71-84.
陈国达,1956.中国地台“活化区”的实例并着重讨论“华夏古陆”问题.地质学报,36(3):239-271.
陈卫锋,陈培荣,黄宏业,等,2007.湖南白马山岩体花岗岩及其包体的年代学和地球化学研究.中国科学(D辑),37(7):873-893.
丁兴,陈培荣,陈卫锋,等,2005.湖南沩山花岗岩中锆石LA-ICPMSU-Pb定年:成岩启示和意义.中国科学(D辑),35(7):606-616.
甘晓春,李惠民,孙大中,等,1993.闽北前寒武纪基底的地质年代学研究.福建地质,12(1):17-13.
甘晓春,李惠民,孙大中,等,1995.浙西南早元古代花岗质岩石的年代.岩石矿物学杂志,14(1):1-8.
郭敬辉,翟明国,李永刚,等,1998.华北太古宙高压基性麻粒岩的两类PT轨迹及其构造意义:矿物化学和变质作用研究.岩石学报,14(4):430-448.
郭令智,施央申,马瑞士,1983.西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化.地质学报,57(1):11-21.
胡雄健,许金坤,童朝旭,等,1991.浙西南前寒武纪地质.北京:地质出版社.
黄汲清,任纪舜,姜春发,等,1977.中国大地构造基本轮廓.地质学报,51(2):117-135.
黄汲清,任纪舜,姜春发,等,1980.中国大地构造及其演化.北京:科学出版社,99-102.
蒋宗胜,王国栋,肖玲玲,等,2011.河南洛宁太华变质杂岩区早元古代变质作用P-T-t轨迹及其大地构造意义.岩石学报,27(12):3701-3717.
靳是琴,1991.不同区域变质相中钙质角闪石的成分特征.科学通报,36(11):851-854.
李献华,李寄嵎,刘颖,等,1999.华夏古陆古元古代变质火山岩的地球化学特征及其构造意义.岩石学报.15(3):364-371.
李献华,王一先,赵振华,等,1998.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学.27(4):327-334.
马军,王仁民,1997.从变质反应空间看宣化、密云两地基性麻粒岩不同的P-T演化.中国科学(D辑),27(1):52-58.
任纪舜,1964.中国东南部泥盆纪前几个大地构造问题的初步探讨.地质学报,44(4):418-431.
任纪舜,陈廷愚,牛宝贵,1990.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社.
水涛,1988.中国东南大陆基底构造格局.中国科学(B辑),31(7):885-896.
王丽娟,于津海,徐夕生,等,2007.闽西南古田-小陶花岗质杂岩体的形成时代和成因.岩石学报,23(6):1470-1484.
汪相,陈洁,罗丹,2008.浙西南淡竹花岗闪长岩中锆石的成因研究及其地质意义.地质评论,54(3):387-398.
王一先,赵振华,包志伟,等,1998.浙江花岗岩类地球化学与地壳演化-Ⅱ.元古宙花岗岩类,地球化学,26(6):57-68.
王忠梅,肖文交,韩春明,等,2013.甘肃敦煌红柳峡地区石榴石斜长角闪岩的变质特征、锆石U-Pb年龄及地质意义.岩石学报,29(5):1685-1697.
魏春景,2016.麻粒岩相变质作用与花岗岩成因-Ⅱ:变质泥质岩高温-超高温变质相平衡与S型花岗岩成因的定量模拟.岩石学报,32(6):1611-1624.
吴锁平,王梅英,戚开静,2007.A型花岗岩研究现状及其述评.岩石矿物学杂志,26(1):57-66.
吴元保,郑永飞,2004,锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
向华,张利,周汉文,等,2008.浙西南变质基底基性-超基性变质岩锆石U-Pb年龄、Hf同位素研究:华厦地块变质基底对华南印支期造山的响应.中国科学(D辑),38(4):401-413.
肖玲玲,蒋宗胜,王国栋,等,2011.赞皇前寒武纪变质杂岩区变质反应结构与变质作用P-T-t轨迹.岩石学报,27(4):980-1002.
谢家荣,1961.中国大地构造问题.地质学报,41(2):218-239.
张文佑,1959.中国大地构造纲要.北京:科学出版社.
张岳桥,徐先兵,贾东,等,2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘,16(1):234-247.
赵磊,周喜文,2012.浙西南八都群泥质麻粒岩的变质演化与PT轨迹.岩石矿物学杂志,31(1):61-72.
周新民,孙涛,沈渭洲,2006.华南中生代花岗岩-火山岩成因与构造体制转换.地质幕,29:26-33.