中国东北软流圈地幔中的原始橄榄岩质地幔:来自大兴安岭地区新生代玄武岩的地球化学证据
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摘要
为了进一步了解中国东北新生代玄武岩地幔源区的物质属性,报道了大兴安岭哈拉哈河-柴河地区新生代玄武岩的全岩主量、微量元素和Sr、Nd、Pb、Hf同位素组成.哈拉哈河-柴河玄武岩属钠质碱性系列,具有与洋岛玄武岩相似的微量元素特征,如富集大离子亲石元素(LILEs)、明显的Nb、Ta正异常等.它们具有中等亏损的Sr-Nd-Hf同位素组成(~(87)Sr/~(86)Sr=0.703 5～0.703 9、ε_(Nd)=5.21～6.55、ε_(Hf)=10.00～11.25),接近中国东部新生代玄武岩的亏损端元.这些玄武岩具有中等的放射成因Pb同位素组成(~(206)Pb/~(204)Pb=18.37～18.57、~(207)Pb/~(204)Pb=15.52～15.54和~(208)Pb/~(204)Pb=38.24～38.43),在~(206)Pb/~(204)Pb-~(207)Pb/~(204)Pb相关图上位于4.42～4.45Ga的地球等时线之间.它们在Sr-Nd-Pb同位素相关图中均落入地幔柱来源的、高~3 He/~4 He比(>30Ra)的洋岛玄武岩范围内,暗示其源区可能存在来自深部地幔的古老原始地幔物质.此外,这些玄武岩具有高MgO(8.49%～11.58%)、高Ni(174×10~(-6)～362×10~(-6))和高Mg~#(59.1～66.9)的特征,表明它们接近于原始岩浆的成分.反演的哈拉哈河-柴河玄武岩的原始岩浆组成具有中等的SiO_2、低Al_2O_3以及高CaO/Al_2O_3比的特征,与石榴子石橄榄岩高压(>2.5GPa)实验熔体的成分相当,暗示玄武岩的源区岩性最可能为橄榄岩.对以原始地幔(而不是亏损地幔)的微量元素为初始成分的饱满石榴子石二辉橄榄岩进行低程度(1%～2%)部分熔融的模拟计算,产生的熔体与哈拉哈河-柴河玄武岩具有一致的微量元素特征,这进一步支持了上述推断.综上所述,认为大兴安岭地区哈拉哈河-柴河玄武岩的源区含有来自深部地幔的古老的橄榄岩质原始地幔组分.
In order to further explore the nature of mantle source beneath the Northeast China,it presents major,trace element,and Sr-Nd-Pb-Hf isotopic compositions for the Cenozoic intra-plate volcanic rocks from the Halaha-Chaihe field in the Greater Khingan Range.These volcanic rocks are mainly alkaline(sodic)basalts,and generally exhibit OIB-like incompatible trace element characteristics,e.g.enrichment in large lithophile elements(LILEs)and positive Nb-Ta anomalies.They show moderate depleted Sr-Nd-Hf isotopic compositions(~(87)Sr/~(86)Sr=0.703 5-0.703 9,ε_(Nd)=5.21-6.55,ε_(Hf)=10.00-11.25)and almost represent the most depleted mantle end-member among the Cenozoic basalts in eastern China.Their Pb isotopic compositions(~(206)Pb/~(204)Pb=18.37-18.57,~(207)Pb/~(204)Pb=15.52-15.54,~(208)Pb/~(204)Pb=38.24-38.43)range between 4.42 Ga and 4.45 Ga geochrons on the ~(207)Pb/~(204)Pb versus ~(206)Pb/~(204)Pb diagram.They also show similar Sr-Nd-Pb isotopic compositions with those mantle plume-derived ocean island basalts(~3 He/~4 He>30 Ra),which implies a deep mantle source.The high MgO(8.49%-11.58%),Ni(174×10~(-6)-362×10~(-6))contents and high Mg~#values(59.1-66.9)of these basalts imply that their compositions are close to those of the primary magmas.The calculated primitive compositions of Halaha-Chaihe basalts show moderate SiO_2,low Al_2O_3 contents and high CaO/Al_2O_3 ratios,which are accordant with the compositions of experimental melts of garnet peridotite under high pressure(>2.5 GPa)conditions,suggesting agarnet peridotitic mantle source.Moreover,traceelement modeling suggests low-degree melts from a primitive mantle(rather than a depleted mantle)are consistent with these basalts.In summary,it is suggested that the mantle source of the Halaha-Chaihe basalts from the Greater Khingan Range contains ancient,primordial,peridotitic component from the deep mantle.
In order to further explore the nature of mantle source beneath the Northeast China,it presents major,trace element,and Sr-Nd-Pb-Hf isotopic compositions for the Cenozoic intra-plate volcanic rocks from the Halaha-Chaihe field in the Greater Khingan Range.These volcanic rocks are mainly alkaline(sodic)basalts,and generally exhibit OIB-like incompatible trace element characteristics,e.g.enrichment in large lithophile elements(LILEs)and positive Nb-Ta anomalies.They show moderate depleted Sr-Nd-Hf isotopic compositions(~(87)Sr/~(86)Sr=0.703 5-0.703 9,ε_(Nd)=5.21-6.55,ε_(Hf)=10.00-11.25)and almost represent the most depleted mantle end-member among the Cenozoic basalts in eastern China.Their Pb isotopic compositions(~(206)Pb/~(204)Pb=18.37-18.57,~(207)Pb/~(204)Pb=15.52-15.54,~(208)Pb/~(204)Pb=38.24-38.43)range between 4.42 Ga and 4.45 Ga geochrons on the ~(207)Pb/~(204)Pb versus ~(206)Pb/~(204)Pb diagram.They also show similar Sr-Nd-Pb isotopic compositions with those mantle plume-derived ocean island basalts(~3 He/~4 He>30 Ra),which implies a deep mantle source.The high MgO(8.49%-11.58%),Ni(174×10~(-6)-362×10~(-6))contents and high Mg~#values(59.1-66.9)of these basalts imply that their compositions are close to those of the primary magmas.The calculated primitive compositions of Halaha-Chaihe basalts show moderate SiO_2,low Al_2O_3 contents and high CaO/Al_2O_3 ratios,which are accordant with the compositions of experimental melts of garnet peridotite under high pressure(>2.5 GPa)conditions,suggesting agarnet peridotitic mantle source.Moreover,traceelement modeling suggests low-degree melts from a primitive mantle(rather than a depleted mantle)are consistent with these basalts.In summary,it is suggested that the mantle source of the Halaha-Chaihe basalts from the Greater Khingan Range contains ancient,primordial,peridotitic component from the deep mantle.
引文
Adam,J.,Green,T.,2006.Trace Element Partitioning between Mica-and Amphibole-Bearing Garnet Lherzolite and Hydrous Basanitic Melt:1.Experimental Results and the Investigation of Controls on Partitioning Behaviour.Contributions to Mineralogy and Petrology,152(1):1-17.https://doi.org/10.1007/s00410-006-0085-4
Allègre,C.J.,Lewin,E.,1995.Isotopic Systems and Stirring Times of the Earth's Mantle.Earth and Planetary Science Letters,136(3-4):629-646.https://doi.org/10.1016/0012-821x(95)00184-e
Anders,E.,Grevesse,N.,1989.Abundances of the Elements:Meteoritic and Solar.Geochimica et Cosmochimica Acta,53(1):197-214.https://doi.org/10.1016/0016-7037(89)90286-x
Bouvier,A.,Vervoort,J.D.,Patchett,P.J.,2008.The Lu-Hf and Sm-Nd Isotopic Composition of CHUR:Constraints from Unequilibrated Chondrites and Implications for the Bulk Composition of Terrestrial Planets.Earth and Planetary Science Letters,273(1-2):48-57.https://doi.org/10.1016/j.epsl.2008.06.010
Boyet,M.,Carlsow,R.W.,2005.142 Nd Evidence for Early(>4.53Ga)Global Differentiation of the Silicate Earth.Science,309(5734):576-581.https://doi.org/10.1126/science.1113634
Chen,H.,Xia,Q.K.,Ingrin,J.,et al.,2017.Heterogeneous Source Components of Intraplate Basalts from NE China Induced by the Ongoing Pacific Slab Subduction.Earth and Planetary Science Letters,459:208-220.https://doi.org/10.1016/j.epsl.2016.11.030
Chen,L.H.,Zeng,G.,Hu,S.L.,et al.,2012.Crustal Recycling and Genesis of Continental Alkaline Basalts:Case Study of the Cenozoic Alkaline Basalts from Shandong Province,Eastern China.Geological Journal of China Universities,18(1):16-27(in Chinese with English abstract).
Chen,L.H.,Zeng,G.,Jiang,S.Y.,et al.,2009.Sources of Anfengshan Basalts:Subducted Lower Crust in the Sulu UHPBelt,China.Earth and Planetary Science Letters,286(3-4):426-435.https://doi.org/10.1016/j.epsl.2009.07.006
Chen,X.Y.,Chen,L.H.,Chen,Y.,et al.,2014.Distribution Summary of Cenozoic Basalts in Central and Eastern China.Geological Journal of China Universities,20(4):507-519(in Chinese with English abstract).
Chu,Z.Y.,Harvey,J.,Liu,C.Z.,et al.,2013.Source of Highly Potassic Basalts in Northeast China:Evidence from ReOs,Sr-Nd-Hf Isotopes and PGE Geochemistry.Chemical Geology,357:52-66.https://doi.org/10.1016/j.chemgeo.2013.08.007
Davis,F.A.,Hirschmann,M.M.,Humayun,M.,2011.The Composition of the Incipient Partial Melt of Garnet Peridotite at 3GPa and the Origin of OIB.Earth and Planetary Science Letters,308(3-4):380-390.https://doi.org/10.1016/j.epsl.2011.06.008
Fan,Q.,Hooper,P.R.,1991.The Cenozoic Basaltic Rocks of Eastern China:Petrology and Chemical Composition.Journal of Petrology,32(4):765-810.https://doi.org/10.1093/petrology/32.4.765
Fan,Q.C.,Sui,J.L.,Zhao,Y.W.,et al.,2008.Preliminary Study on Garnet Peridotite Xenolith of Quaternary Volcanic Rocks in Middle Daxing'an Mountain Range.Acta Petrologica Sinica,24(11):2563-2568(in Chinese with English abstract).
Fan,Q.C.,Zhao,Y.W.,Li,D.M.,et al.,2011.Studies on Quaternary Volcanism Stages of Halaha River and Chaoer River Area in the Great Xing'an Range:Evidence from K-Ar Dating and Volcanic Geology Features.Acta Petrologica Sinica,27(10):2827-2832(in Chinese with English abstract).
Gale,A.,Dalton,C.A.,Langmuir,C.H.,et al.,2013.The Mean Composition of Ocean Ridge Basalts.Geochemistry,Geophysics,Geosystems,14(3):489-518.https://doi.org/10.1029/2012gc004334
Geske,A.,Goldstein,R.H.,Mavromatis,V.,et al.,2015.The Magnesium Isotope(δ26 Mg)Signature of Dolomites.Geochimica et Cosmochimica Acta,149:131-151.https://doi.org/10.1016/j.gca.2014.11.003
Graham,D.W.,Larsen,L.M.,Hanan,B.B.,et al.,1998.Helium Isotope Composition of the Early Iceland Mantle Plume Inferred from the Tertiary Picrites of West Greenland.Earth and Planetary Science Letters,160(3-4):241-255.https://doi.org/10.1016/s0012-821x(98)00083-1
Graham,D.,Lupton,J.,Albarède,F.,et al.,1990.Extreme Temporal Homogeneity of Helium Isotopes at Piton de la Fournaise,Réunion Island.Nature,347(6293):545-548.https://doi.org/10.1038/347545a0
Green,T.H.,Blundy,J.D.,Adam,J.,et al.,2000.SIMS Determination of Trace Element Partition Coefficients between Garnet,Clinopyroxene and Hydrous Basaltic Liquids at 2-7.5GPa and 1 080-1 200℃.Lithos,53(3-4):165-187.https://doi.org/10.1016/s0024-4937(00)00023-2
Hart,S.R.,1984.A Large-Scale Isotope Anomaly in the Southern Hemisphere Mantle.Nature,309(5971):753-757.https://doi.org/10.1038/309753a0
Hilton,D.R.,Gr9nvold,K.,MacPherson,C.G.,et al.,1999.Extreme 3 He/4 He Ratios in Northwest Iceland:Constraining the Common Component in Mantle Plumes.Earth and Planetary Science Letters,173(1/2):53-60.https://doi.org/10.1016/s0012-821x(99)00215-0
Hirose,K.,Kushiro,I.,1993.Partial Melting of Dry Peridotites at High Pressures:Determination of Compositions of Melts Segregated from Peridotite Using Aggregates of Diamond.Earth and Planetary Science Letters,114(4):477-489.https://doi.org/10.1016/0012-821x(93)90077-m
Hirschmann,M.M.,Kogiso,T.,Baker,M.B.,et al.,2003.Alkalic Magmas Generated by Partial Melting of Garnet Pyroxenite.Geology,31(6):481.https://doi.org/10.1130/0091-7613(2003)0310481:amgbpm>2.0.co;2
Ho,K.S.,Ge,W.C.,Chen,J.C.,et al.,2013.Late Cenozoic Magmatic Transitions in the Central Great Xing'an Range,Northeast China:Geochemical and Isotopic Constraints on Petrogenesis.Chemical Geology,352:1-18.https://doi.org/10.1016/j.chemgeo.2013.05.040
Ho,K.S.,Liu,Y.,Chen,J.C.,et al.,2008.Elemental and SrNd-Pb Isotopic Compositions of Late Cenozoic Abaga Basalts,Inner Mongolia:Implications for Petrogenesis and Mantle Process.Geochemical Journal,42(4):339-357.https://doi.org/10.2343/geochemj.42.339
Hofmann,A.W.,1997.Mantle Geochemistry:The Message from Oceanic Volcanism.Nature,385(6613):219-229.https://doi.org/10.1038/385219a0
Hofmann,A.W.,Jochum,K.P.,Seufert,M.,et al.,1986.Nb and Pb in Oceanic Basalts:New Constraints on Mantle Evolution.Earth and Planetary Science Letters,79(1-2):33-45.https://doi.org/10.1016/0012-821x(86)90038-5
Holmes,A.,1946.An Estimate of the Age of the Earth.Nature,157(3995):680-684.https://doi.org/10.1038/157680a0
Hong,L.B.,Zhang,Y.H.,Qian,S.P.,et al.,2013.Constraints from Melt Inclusions and Their Host Olivines on the Petrogenesis of Oligocene-Early Miocene Xindian Basalts,Chifeng Area,North China Craton.Contributions to Mineralogy and Petrology,165(2):305-326.https://doi.org/10.1007/s00410-012-0810-0
Huang,J.L.,Zhao,D.P.,2006.High-Resolution Mantle Tomography of China and Surrounding Regions.Journal of Geophysical Research,111(B9):B09305.https://doi.org/10.1029/2005jb004066
Huang,J.,Li,S.G.,Xiao,Y.L.,et al.,2015.Origin of Lowδ26 Mg Cenozoic Basalts from South China Block and Their Geodynamic Implications.Geochimica et Cosmochimica Acta,164:298-317.https://doi.org/10.1016/j.gca.2015.04.054
Jackson,M.G.,Carlson,R.W.,Kurz,M.D.,et al.,2010.Evidence for the Survival of the Oldest Terrestrial Mantle Reservoir.Nature,466(7308):853-856.https://doi.org/10.1038/nature09287
Jackson,M.,Kurz,M.,Hart,S.,et al.,2007.New Samoan Lavas from Ofu Island Reveal a Hemispherically Heterogeneous High 3 He/4 He Mantle.Earth and Planetary Science Letters,264(3-4):360-374.https://doi.org/10.1016/j.epsl.2007.09.023
Jahn,B.M.,Wu,F.Y.,Chen,B.,2000.Granitoids of the Central Asian Orogenic Belt and Continental Growth in the Phanerozoic.Geological Society of America,Special Paper,350:181-193.https://doi.org/10.1130/0-8137-2350-7.181
Jochum,K.P.,Weis,U.,Schwager,B.,et al.,2016.Reference Values Following ISO Guidelines for Frequently Requested Rock Reference Materials.Geostandards and Geoanalytical Research,40(3):333-350.https://doi.org/10.1111/j.1751-908x.2015.00392.x
Keshav,S.,Gudfinnsson,G.H.,Sen,G.,et al.,2004.HighPressure Melting Experiments on Garnet Clinopyroxenite and the Alkalic to Tholeiitic Transition in Ocean-Island Basalts.Earth and Planetary Science Letters,223(3-4):365-379.https://doi.org/10.1016/j.epsl.2004.04.029
Kogiso,T.,Hirschmann,M.M.,Frost,D.J.,2003.HighPressure Partial Melting of Garnet Pyroxenite:Possible Mafic Lithologies in the Source of Ocean Island Basalts.Earth and Planetary Science Letters,216(4):603-617.https://doi.org/10.1016/s0012-821x(03)00538-7
Kuritani,T.,Kimura,J.I.,Miyamoto,T.,et al.,2009.Intraplate Magmatism Related to Deceleration of Upwelling Asthenospheric Mantle:Implications from the Changbaishan Shield Basalts,Northeast China.Lithos,112(3-4):247-258.https://doi.org/10.1016/j.lithos.2009.02.007
Kuritani,T.,Kimura,J.I.,Ohtani,E.,et al.,2013.Transition Zone Origin of Potassic Basalts from Wudalianchi Volcano,Northeast China.Lithos,156-159:1-12.https://doi.org/10.1016/j.lithos.2012.10.010
Kuritani,T.,Nakamura,E.,2002.Precise Isotope Analysis of Nanogram-Level Pb for Natural Rock Samples without Use of Double Spikes.Chemical Geology,186(1-2):31-43.https://doi.org/10.1016/s0009-2541(02)00004-9
Kuritani,T.,Ohtani,E.,Kimura,J.I.,2011.Intensive Hydration of the Mantle Transition Zone beneath China Caused by Ancient Slab Stagnation.Nature Geoscience,4(10):713-716.https://doi.org/10.1038/ngeo1250
Kurz,M.D.,Jenkins,W.J.,Hart,S.R.,1982.Helium Isotopic Systematics of Oceanic Islands and Mantle Heterogeneity.Nature,297(5861):43-47.https://doi.org/10.1038/297043a0
Kushiro,I.,2013.Partial Melting of a Fertile Mantle Peridotite at High Pressures:An Experimental Study Using Aggregates of Diamond.In:Kushiro,I.,ed.,Earth Processes:Reading the Isotopic Code.American Geophysical Union,Washington,D.C.,109-122.https://doi.org/10.1029/gm095p0109
Le Bas,M.J.,Le Maitre,R.W.,Streckeisen,A.,et al.,1986.AChemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram.Journal of Petrology,27(3):745-750.https://doi.org/10.1093/petrology/27.3.745
Li,H.Y.,Xu,Y.G.,Ryan,J.G.,et al.,2017.Olivine and Melt Inclusion Chemical Constraints on the Source of Intracontinental Basalts from the Eastern North China Craton:Discrimination of Contributions from the Subducted Pacific Slab.Geochimica et Cosmochimica Acta,178:1-19.https://doi.org/10.1016/j.gca.2015.12.032
Li,S.G.,Yang,W.,Ke,S.,et al.,2016.Deep Carbon Cycles Constrained by a Large-Scale Mantle Mg Isotope Anomaly in Eastern China.National Science Review,4(1):111-120.https://doi.org/10.1093/nsr/nww070
Li,Y.Q.,Ma,C.Q.,Robinson,P.T.,et al.,2015.Recycling of Oceanic Crust from a Stagnant Slab in the Mantle Transition Zone:Evidence from Cenozoic Continental Basalts in Zhejiang Province,SE China.Lithos,230:146-165.https://doi.org/10.1016/j.lithos.2015.05.021
Liu,J.Q.,Chen,L.H.,Wang,X.J.,et al.,2017.The Role of Melt-Rock Interaction in the Formation of Quaternary High-MgO Potassic Basalt from the Greater Khingan Range,Northeast China.Journal of Geophysical Research:Solid Earth,122(1):262-280.https://doi.org/10.1002/2016jb013605
Liu,J.Q.,Ren,Z.Y.,Nichols,A.R.L.,et al.,2015.Petrogenesis of Late Cenozoic Basalts from North Hainan Island:Constraints from Melt Inclusions and Their Host Olivines.Geochimica et Cosmochimica Acta,152:89-121.https://doi.org/10.1016/j.gca.2014.12.023
Liu,S.A.,Wang,Z.Z.,Li,S.G.,et al.,2016.Zinc Isotope Evidence for a Large-Scale Carbonated Mantle beneath Eastern China.Earth and Planetary Science Letters,444:169-178.https://doi.org/10.1016/j.epsl.2016.03.051
Liu,R.,X.,1992.Geochronology and Geochemistry of Cenozoic Volcanic Rocks in China.Seismological Press,Beijing(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
Meng,F.C.,Safonova,I.,Chen,S.S.,et al.,2018.Late Cenozoic Intra-Plate Basalts of the Greater Khingan Range in NE China and Khangai Province in Central Mongolia.Gondwana Research,63:65-84.https://doi.org/10.1016/j.gr.2018.05.009
Pertermann,M.,Hirschmann,M.M.,2003.Anhydrous Partial Melting Experiments on MORB-Like Eclogite:Phase Relations,Phase Compositions and Mineral-Melt Partitioning of Major Elements at 2-3GPa.Journal of Petrology,44(12):2173-2201.https://doi.org/10.1093/petrology/egg074
Pu,W.,Gao,J.F.,Zhao,K.D.,et al.,2005.Separation Method of Rb-Sr,Sm-Nd Using DCTA and HIBA.Journal of Nanjing University(Natural Sciences),41(4):445-450(in Chinese with English abstract).
Roeder,P.L.,Emslie,R.F.,1970.Olivine-Liquid Equilibrium.Contributions to Mineralogy and Petrology,29(4):275-289.https://doi.org/10.1007/bf00371276
Rudnick,R.L.,Gao,S.,2003.Composition of the Continental Crust.In:Rudnick,R.L.,Gao,S.,eds.,Treatise on Geochemistry.Elsevier,Cambridge,1-64.https://doi.org/10.1016/b0-08-043751-6/03016-4
Saal,A.,Kurz,M.,Hart,S.,et al.,2007.The Role of Lithospheric Gabbros on the Composition of Galapagos Lavas.Earth and Planetary Science Letters,257(3-4):391-406.https://doi.org/10.1016/j.epsl.2007.02.040
Saenger,C.,Wang,Z.R.,2014.Magnesium Isotope Fractionation in Biogenic and Abiogenic Carbonates:Implications for Paleoenvironmental Proxies.Quaternary Science Reviews,90:1-21.https://doi.org/10.1016/j.quascirev.2014.01.014
Spandler,C.,Yaxley,G.,Green,D.H.,et al.,2007.Phase Relations and Melting of Anhydrous K-Bearing Eclogite from 1 200to 1 600℃and 3to 5GPa.Journal of Petrology,49(4):771-795.
Starkey,N.A.,Stuart,F.M.,Ellam,R.M.,et al.,2009.Helium Isotopes in Early Iceland Plume Picrites:Constraints on the Composition of High 3 He/4 He Mantle.Earth and Planetary Science Letters,277(1-2):91-100.https://doi.org/10.1016/j.epsl.2008.10.007
Stracke,A.,2012.Earth's Heterogeneous Mantle:A Product of Convection-Driven Interaction between Crust and Mantle.Chemical Geology,330/331:274-299.https://doi.org/10.1016/j.chemgeo.2012.08.007
Stuart,F.M.,Lass-Evans,S.,Godfrey Fitton,J.,et al.,2003.High 3 He/4 He Ratios in Picritic Basalts from Baffin Island and the Role of a Mixed Reservoir in Mantle Plumes.Nature,424(6944):57-59.https://doi.org/10.1038/nature01711
Sun,S.S.,1980.Lead Isotopic Study of Young Volcanic Rocks from Mid-Ocean Ridges,Ocean Islands and Island Arcs.Philosophical Transactions of the Royal Society A:Mathematical,Physical and Engineering Sciences,297(1431):409-445.https://doi.org/10.1098/rsta.1980.0224
Sun,Y.B.,Zhang,R.,Ding,C.C.,et al.,2016.Adsorption of U(VI)on Sericite in the Presence of Bacillus Subtilis:ACombined Batch,EXAFS and Modeling Techniques.Geochimica et Cosmochimica Acta,180:51-65.https://doi.org/10.1016/j.gca.2016.02.012
Sun,Y.,Ying,J.F.,Su,B.X.,et al.,2015.Contribution of Crustal Materials to the Mantle Sources of Xiaogulihe Ultrapotassic Volcanic Rocks,Northeast China:New Constraints from Mineral Chemistry and Oxygen Isotopes of Olivine.Chemical Geology,405:10-18.https://doi.org/10.1016/j.chemgeo.2015.04.005
Tang,Y.J.,Zhang,H.F.,Nakamura,E.,et al.,2007.Lithium Isotopic Systematics of Peridotite Xenoliths from Hannuoba,North China Craton:Implications for Melt-Rock Interaction in the Considerably Thinned Lithospheric Mantle.Geochimica et Cosmochimica Acta,71(17):4327-4341.https://doi.org/10.1016/j.gca.2007.07.006
Tao,K.,Niu,F.L.,Ning,J.Y.,et al.,2014.Crustal Structure beneath NE China Imaged by NECESSArray Receiver Function Data.Earth and Planetary Science Letters,398:48-57.https://doi.org/10.1016/j.epsl.2014.04.043
Teng,F.Z.,2017.Magnesium Isotope Geochemistry.Reviews in Mineralogy and Geochemistry,82(1):219-287.https://doi.org/10.2138/rmg.2017.82.7
Teng,F.Z.,Li,W.Y.,Ke,S.,et al.,2010.Magnesium Isotopic Composition of the Earth and Chondrites.Geochimica et Cosmochimica Acta,74(14):4150-4166.https://doi.org/10.1016/j.gca.2010.04.019
Vervoort,J.D.,Plank,T.,Prytulak,J.,2011.The Hf-Nd Isotopic Composition of Marine Sediments.Geochimica et Cosmochimica Acta,75(20):5903-5926.https://doi.org/10.1016/j.gca.2011.07.046
Walter,M.J.,1998.Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere.Journal of Petrology,39(1):29-60.https://doi.org/10.1093/petrology/39.1.29
Wang,X.J.,Chen,L.H.,Hofmann,A.W.,et al.,2017.Mantle Transition Zone-Derived EM1Component beneath NEChina:Geochemical Evidence from Cenozoic Potassic Basalts.Earth and Planetary Science Letters,465:16-28.https://doi.org/10.1016/j.epsl.2017.02.028
Wang,Y.,Zhao,Z.F.,Zheng,Y.F.,et al.,2011.Geochemical Constraints on the Nature of Mantle Source for Cenozoic Continental Basalts in East-Central China.Lithos,125(3-4):940-955.https://doi.org/10.1016/j.lithos.2011.05.007
Wei,W.,Xu,J.D.,Zhao,D.P.,et al.,2012.East Asia Mantle Tomography:New Insight into Plate Subduction and Intraplate Volcanism.Journal of Asian Earth Sciences,60:88-103.https://doi.org/10.1016/j.jseaes.2012.08.001
Weis,D.,Kieffer,B.,Maerschalk,C.,et al.,2006.HighPrecision Isotopic Characterization of USGS Reference Materials by TIMS and MC-ICP-MS.Geochemistry,Geophysics,Geosystems,7(8).https://doi.org/10.1029/2006gc001283
Wombacher,F.,Eisenhauer,A.,B9hm,F.,et al.,2011.Magnesium Stable Isotope Fractionation in Marine Biogenic Calcite and Aragonite.Geochimica et Cosmochimica Acta,75(19):5797-5818.https://doi.org/10.1016/j.gca.2011.07.017
Workman,R.K.,Hart,S.R.,2005.Major and Trace Element Composition of the Depleted MORB Mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72.https://doi.org/10.1016/j.epsl.2004.12.005
Xiao,W.J.,Windley,B.F.,Sun,S.,et al.,2015.A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia:Oroclines,Sutures,and Terminal Accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507.https://doi.org/10.1146/annurev-earth-060614-105254
Xu,Y.G.,2007.Diachronous Lithospheric Thinning of the North China Craton and Formation of the Daxin'anlingTaihangshan Gravity Lineament.Lithos,96(1-2):281-298.https://doi.org/10.1016/j.lithos.2006.09.013
Xu,Y.G.,Li,H.Y.,Hong,L.B.,et al.,2018.Generation of Cenozoic Intraplate Basalts in the Big Mantle Wedge under Eastern Asia.Science China Earth Sciences,48(7):825-843(in Chinese).
Xu,Y.G.,Zhang,H.H.,Qiu,H.N.,et al.,2012.Oceanic Crust Components in Continental Basalts from Shuangliao,Northeast China:Derived from the Mantle Transition Zone?.Chemical Geology,328:168-184.https://doi.org/10.1016/j.chemgeo.2012.01.027
Xu,Z.,Zheng,Y.F.,Zhao,Z.F.,2017.The Origin of Cenozoic Continental Basalts in East-Central China:Constrained by Linking Pb Isotopes to Other Geochemical Variables.Lithos,268-271:302-319.https://doi.org/10.1016/j.lithos.2016.11.006
Yang,W.,Teng,F.Z.,Zhang,H.F.,et al.,2012.Magnesium Isotopic Systematics of Continental Basalts from the North China Craton:Implications for Tracing Subducted Carbonate in the Mantle.Chemical Geology,328:185-194.https://doi.org/10.1016/j.chemgeo.2012.05.018
Yang,Y.H.,Zhang,H.F.,Chu,Z.Y.,et al.,2010.Combined Chemical Separation of Lu,Hf,Rb,Sr,Sm and Nd from a Single Rock Digest and Precise and Accurate Isotope Determinations of Lu-Hf,Rb-Sr and Sm-Nd Isotope Systems Using Multi-Collector ICP-MS and TIMS.International Journal of Mass Spectrometry,290(2-3):120-126.https://doi.org/10.1016/j.ijms.2009.12.011
Yang,Z.F.,Li,J.,Liang,W.F.,et al.,2016.On the Chemical Markers of Pyroxenite Contributions in Continental Basalts in Eastern China:Implications for Source Lithology and the Origin of Basalts.Earth-Science Reviews,157:18-31.https://doi.org/10.1016/j.earscirev.2016.04.001
Yasuda,A.,Fujii,T.,Kurita,K.,1994.Melting Phase Relations of an Anhydrous Mid-Ocean Ridge Basalt from 3to 20GPa:Implications for the Behavior of Subducted Oceanic Crust in the Mantle.Journal of Geophysical Research:Solid Earth,99(B5):9401-9414.https://doi.org/10.1029/93jb03205
Yaxley,G.M.,Sobolev,A.V.,2007.High-Pressure Partial Melting of Gabbro and Its Role in the Hawaiian Magma Source.Contributions to Mineralogy and Petrology,154(4):371-383.https://doi.org/10.1007/s00410-007-0198-4
Yaxley,G.M.,Green,D.H.1998.Reactions between Eclogite and Peridotite:Mantle Refertilisation by Subduction of Oceanic Crust.Schweiz.Mineral.Petrogr.Mitt.,78(2):243-255.
Yu,S.Y.,Xu,Y.G.,Zhou,S.H.,et al.,2018.Late Cenozoic Basaltic Lavas from the Changbaishan-Baoqing Volcanic Belt,NE China:Products of Lithosphere-Asthenosphere Interaction Induced by Subduction of the Pacific Plate.Journalof Asian Earth Sciences,164:260-273.https://doi.org/10.1016/j.jseaes.2018.06.031
Zeng,G.,Chen,L.H.,Hofmann,A.W.,et al.,2011.Crust Recycling in the Sources of Two Parallel Volcanic Chains in Shandong,North China.Earth and Planetary Science Letters,302(3-4):359-368.https://doi.org/10.1016/j.epsl.2010.12.026
Zeng,G.,Chen,L.H.,Xu,X.S.,et al.,2010.Carbonated Mantle Sources for Cenozoic Intra-Plate Alkaline Basalts in Shandong,North China.Chemical Geology,273(1-2):35-45.https://doi.org/10.1016/j.chemgeo.2010.02.009
Zeng,G.,Chen,L.H.,Yu,X.,et al.,2017.Magma-Magma Interaction in the Mantle beneath Eastern China.Journal of Geophysical Research:Solid Earth,122(4):2763-2779.https://doi.org/10.1002/2017jb014023
Zhang,J.J.,Zheng,Y.F.,Zhao,Z.F.,2009.Geochemical Evidence for Interaction between Oceanic Crust and Lithospheric Mantle in the Origin of Cenozoic Continental Basalts in East-Central China.Lithos,110(1):305-326.https://doi.org/10.1016/j.lithos.2009.01.006
Zhang,L.Y.,Prelevi,D.,Li,N.,et al.,2016.Variation of Olivine Composition in the Volcanic Rocks in the Songliao Basin,NE China:Lithosphere Control on the Origin of the K-Rich Intraplate Mafic Lavas.Lithos,262:153-168.https://doi.org/10.1016/j.lithos.2016.06.028
Zhang,M.L.,Guo,Z.F.,2016.Origin of Late Cenozoic AbagaDalinuoer Basalts,Eastern China:Implications for a Mixed Pyroxenite-Peridotite Source Related with Deep Subduction of the Pacific Slab.GondwanaResearch,37:130-151.https://doi.org/10.1016/j.gr.2016.05.014
Zhang,R.Q.,Wu,Q.J.,Sun,L.,et al.,2014.Crustal and Lithospheric Structure of Northeast China from S-Wave Receiver Functions.Earth and Planetary Science Letters,401:196-205.https://doi.org/10.1016/j.epsl.2014.06.017
Zhang,Y.L.,Liu,C.Z.,Ge,W.C.,et al.,2011.Ancient SubContinental Lithospheric Mantle(SCLM)beneath the Eastern Part of the Central Asian Orogenic Belt(CAOB):Implications for Crust-Mantle Decoupling.Lithos,126(3-4):233-247.https://doi.org/10.1016/j.lithos.2011.07.022
Zhao,Y.W.,Fan,Q.C.,2011.Characteristics of Lithospheric Mantle beneath the Great Xing'an Range:Evidence from Spinel Peridotite Xenoliths in the Halaha River and Chaoer River Area.Acta Petrologica Sinica,27(10):2833-2841(in Chinese with English abstract).
Zhao,Y.W.,Fan,Q.C.,2012.Mantle Sources and Magma Genesis of Quaternary Volcanic Rocks in the Halaha River and Chaoer River Area,Great Xing'an Range.Acta Petrologica Sinica,28(4):1119-1129(in Chinese with English abstract).
Zhao,Y.W.,Fan,Q.C.,Bai,Z.D.,et al.,2008.Preliminary Study on Quaternary Volcanoes in the Halaha River and Chaoer River Area in Daxing'an Mountain Range.Acta Petrologica Sinica,24(11):2569-2575(in Chinese with English abstract).
Zhou,X.,Armstrong,R.,1982.Cenozoic Volcanic Rocks of Eastern China:Secular and Geographic Trends in Chemistry and Strontium Isotopic Composition.Earth and Planetary Science Letters,58(3):301-329.https://doi.org/10.1016/0012-821x(82)90083-8
Zou,H.B.,Zindler,A.,Xu,X.S.,et al.,2000.Major,Trace Element,and Nd,Sr and Pb Isotope Studies of Cenozoic Basalts in SE China:Mantle Sources,Regional Variations,and Tectonic Significance.Chemical Geology,171(1-2):33-47.https://doi.org/10.1016/s0009-2541(00)00243-6
陈立辉,曾罡,胡森林,等,2012.地壳再循环与大陆碱性玄武岩的成因:以山东新生代碱性玄武岩为例.高校地质学报,18(1):16-27.
陈霞玉,陈立辉,陈晹,等,2014.中国中-东部地区新生代玄武岩的分布规律与面积汇总.高校地质学报,20(4):507-519.
樊祺诚,隋建立,赵勇伟,等,2008.大兴安岭中部第四纪火山岩中石榴石橄榄岩捕虏体的初步研究.岩石学报,24(11):2563-2568.
樊祺诚,赵勇伟,李大明,等,2011.大兴安岭哈拉哈河-绰尔河第四纪火山分期:K-Ar年代学与火山地质特征.岩石学报,27(10):2827-2832.
刘若新,1992.中国新生代火山岩年代学与地球化学.北京:地震出版社.
濮巍,高剑峰,赵葵东,等,2005.利用DCTA和HIBA快速有效分离Rb-Sr、Sm-Nd的方法.南京大学学报(自然科学版),41(4):445-450.
徐义刚,李洪颜,洪路兵,等,2018.东亚大地幔楔与中国东部新生代板内玄武岩成因.中国科学:地球科学,48(7):825-843.
赵勇伟,樊祺诚,2011.大兴安岭岩石圈地幔特征:哈拉哈河-绰尔河橄榄岩捕虏体的证据.岩石学报,27(10):2833-2841.
赵勇伟,樊祺诚,2012.大兴安岭哈拉哈河-绰尔河第四纪火山岩地幔源区与岩浆成因.岩石学报,28(4):1119-1129.
赵勇伟,樊祺诚,白志达,等,2008.大兴安岭哈拉哈河-淖尔河地区第四纪火山活动初步研究.岩石学报,24(11):2569-2575.
Allègre,C.J.,Lewin,E.,1995.Isotopic Systems and Stirring Times of the Earth's Mantle.Earth and Planetary Science Letters,136(3-4):629-646.https://doi.org/10.1016/0012-821x(95)00184-e
Anders,E.,Grevesse,N.,1989.Abundances of the Elements:Meteoritic and Solar.Geochimica et Cosmochimica Acta,53(1):197-214.https://doi.org/10.1016/0016-7037(89)90286-x
Bouvier,A.,Vervoort,J.D.,Patchett,P.J.,2008.The Lu-Hf and Sm-Nd Isotopic Composition of CHUR:Constraints from Unequilibrated Chondrites and Implications for the Bulk Composition of Terrestrial Planets.Earth and Planetary Science Letters,273(1-2):48-57.https://doi.org/10.1016/j.epsl.2008.06.010
Boyet,M.,Carlsow,R.W.,2005.142 Nd Evidence for Early(>4.53Ga)Global Differentiation of the Silicate Earth.Science,309(5734):576-581.https://doi.org/10.1126/science.1113634
Chen,H.,Xia,Q.K.,Ingrin,J.,et al.,2017.Heterogeneous Source Components of Intraplate Basalts from NE China Induced by the Ongoing Pacific Slab Subduction.Earth and Planetary Science Letters,459:208-220.https://doi.org/10.1016/j.epsl.2016.11.030
Chen,L.H.,Zeng,G.,Hu,S.L.,et al.,2012.Crustal Recycling and Genesis of Continental Alkaline Basalts:Case Study of the Cenozoic Alkaline Basalts from Shandong Province,Eastern China.Geological Journal of China Universities,18(1):16-27(in Chinese with English abstract).
Chen,L.H.,Zeng,G.,Jiang,S.Y.,et al.,2009.Sources of Anfengshan Basalts:Subducted Lower Crust in the Sulu UHPBelt,China.Earth and Planetary Science Letters,286(3-4):426-435.https://doi.org/10.1016/j.epsl.2009.07.006
Chen,X.Y.,Chen,L.H.,Chen,Y.,et al.,2014.Distribution Summary of Cenozoic Basalts in Central and Eastern China.Geological Journal of China Universities,20(4):507-519(in Chinese with English abstract).
Chu,Z.Y.,Harvey,J.,Liu,C.Z.,et al.,2013.Source of Highly Potassic Basalts in Northeast China:Evidence from ReOs,Sr-Nd-Hf Isotopes and PGE Geochemistry.Chemical Geology,357:52-66.https://doi.org/10.1016/j.chemgeo.2013.08.007
Davis,F.A.,Hirschmann,M.M.,Humayun,M.,2011.The Composition of the Incipient Partial Melt of Garnet Peridotite at 3GPa and the Origin of OIB.Earth and Planetary Science Letters,308(3-4):380-390.https://doi.org/10.1016/j.epsl.2011.06.008
Fan,Q.,Hooper,P.R.,1991.The Cenozoic Basaltic Rocks of Eastern China:Petrology and Chemical Composition.Journal of Petrology,32(4):765-810.https://doi.org/10.1093/petrology/32.4.765
Fan,Q.C.,Sui,J.L.,Zhao,Y.W.,et al.,2008.Preliminary Study on Garnet Peridotite Xenolith of Quaternary Volcanic Rocks in Middle Daxing'an Mountain Range.Acta Petrologica Sinica,24(11):2563-2568(in Chinese with English abstract).
Fan,Q.C.,Zhao,Y.W.,Li,D.M.,et al.,2011.Studies on Quaternary Volcanism Stages of Halaha River and Chaoer River Area in the Great Xing'an Range:Evidence from K-Ar Dating and Volcanic Geology Features.Acta Petrologica Sinica,27(10):2827-2832(in Chinese with English abstract).
Gale,A.,Dalton,C.A.,Langmuir,C.H.,et al.,2013.The Mean Composition of Ocean Ridge Basalts.Geochemistry,Geophysics,Geosystems,14(3):489-518.https://doi.org/10.1029/2012gc004334
Geske,A.,Goldstein,R.H.,Mavromatis,V.,et al.,2015.The Magnesium Isotope(δ26 Mg)Signature of Dolomites.Geochimica et Cosmochimica Acta,149:131-151.https://doi.org/10.1016/j.gca.2014.11.003
Graham,D.W.,Larsen,L.M.,Hanan,B.B.,et al.,1998.Helium Isotope Composition of the Early Iceland Mantle Plume Inferred from the Tertiary Picrites of West Greenland.Earth and Planetary Science Letters,160(3-4):241-255.https://doi.org/10.1016/s0012-821x(98)00083-1
Graham,D.,Lupton,J.,Albarède,F.,et al.,1990.Extreme Temporal Homogeneity of Helium Isotopes at Piton de la Fournaise,Réunion Island.Nature,347(6293):545-548.https://doi.org/10.1038/347545a0
Green,T.H.,Blundy,J.D.,Adam,J.,et al.,2000.SIMS Determination of Trace Element Partition Coefficients between Garnet,Clinopyroxene and Hydrous Basaltic Liquids at 2-7.5GPa and 1 080-1 200℃.Lithos,53(3-4):165-187.https://doi.org/10.1016/s0024-4937(00)00023-2
Hart,S.R.,1984.A Large-Scale Isotope Anomaly in the Southern Hemisphere Mantle.Nature,309(5971):753-757.https://doi.org/10.1038/309753a0
Hilton,D.R.,Gr9nvold,K.,MacPherson,C.G.,et al.,1999.Extreme 3 He/4 He Ratios in Northwest Iceland:Constraining the Common Component in Mantle Plumes.Earth and Planetary Science Letters,173(1/2):53-60.https://doi.org/10.1016/s0012-821x(99)00215-0
Hirose,K.,Kushiro,I.,1993.Partial Melting of Dry Peridotites at High Pressures:Determination of Compositions of Melts Segregated from Peridotite Using Aggregates of Diamond.Earth and Planetary Science Letters,114(4):477-489.https://doi.org/10.1016/0012-821x(93)90077-m
Hirschmann,M.M.,Kogiso,T.,Baker,M.B.,et al.,2003.Alkalic Magmas Generated by Partial Melting of Garnet Pyroxenite.Geology,31(6):481.https://doi.org/10.1130/0091-7613(2003)0310481:amgbpm>2.0.co;2
Ho,K.S.,Ge,W.C.,Chen,J.C.,et al.,2013.Late Cenozoic Magmatic Transitions in the Central Great Xing'an Range,Northeast China:Geochemical and Isotopic Constraints on Petrogenesis.Chemical Geology,352:1-18.https://doi.org/10.1016/j.chemgeo.2013.05.040
Ho,K.S.,Liu,Y.,Chen,J.C.,et al.,2008.Elemental and SrNd-Pb Isotopic Compositions of Late Cenozoic Abaga Basalts,Inner Mongolia:Implications for Petrogenesis and Mantle Process.Geochemical Journal,42(4):339-357.https://doi.org/10.2343/geochemj.42.339
Hofmann,A.W.,1997.Mantle Geochemistry:The Message from Oceanic Volcanism.Nature,385(6613):219-229.https://doi.org/10.1038/385219a0
Hofmann,A.W.,Jochum,K.P.,Seufert,M.,et al.,1986.Nb and Pb in Oceanic Basalts:New Constraints on Mantle Evolution.Earth and Planetary Science Letters,79(1-2):33-45.https://doi.org/10.1016/0012-821x(86)90038-5
Holmes,A.,1946.An Estimate of the Age of the Earth.Nature,157(3995):680-684.https://doi.org/10.1038/157680a0
Hong,L.B.,Zhang,Y.H.,Qian,S.P.,et al.,2013.Constraints from Melt Inclusions and Their Host Olivines on the Petrogenesis of Oligocene-Early Miocene Xindian Basalts,Chifeng Area,North China Craton.Contributions to Mineralogy and Petrology,165(2):305-326.https://doi.org/10.1007/s00410-012-0810-0
Huang,J.L.,Zhao,D.P.,2006.High-Resolution Mantle Tomography of China and Surrounding Regions.Journal of Geophysical Research,111(B9):B09305.https://doi.org/10.1029/2005jb004066
Huang,J.,Li,S.G.,Xiao,Y.L.,et al.,2015.Origin of Lowδ26 Mg Cenozoic Basalts from South China Block and Their Geodynamic Implications.Geochimica et Cosmochimica Acta,164:298-317.https://doi.org/10.1016/j.gca.2015.04.054
Jackson,M.G.,Carlson,R.W.,Kurz,M.D.,et al.,2010.Evidence for the Survival of the Oldest Terrestrial Mantle Reservoir.Nature,466(7308):853-856.https://doi.org/10.1038/nature09287
Jackson,M.,Kurz,M.,Hart,S.,et al.,2007.New Samoan Lavas from Ofu Island Reveal a Hemispherically Heterogeneous High 3 He/4 He Mantle.Earth and Planetary Science Letters,264(3-4):360-374.https://doi.org/10.1016/j.epsl.2007.09.023
Jahn,B.M.,Wu,F.Y.,Chen,B.,2000.Granitoids of the Central Asian Orogenic Belt and Continental Growth in the Phanerozoic.Geological Society of America,Special Paper,350:181-193.https://doi.org/10.1130/0-8137-2350-7.181
Jochum,K.P.,Weis,U.,Schwager,B.,et al.,2016.Reference Values Following ISO Guidelines for Frequently Requested Rock Reference Materials.Geostandards and Geoanalytical Research,40(3):333-350.https://doi.org/10.1111/j.1751-908x.2015.00392.x
Keshav,S.,Gudfinnsson,G.H.,Sen,G.,et al.,2004.HighPressure Melting Experiments on Garnet Clinopyroxenite and the Alkalic to Tholeiitic Transition in Ocean-Island Basalts.Earth and Planetary Science Letters,223(3-4):365-379.https://doi.org/10.1016/j.epsl.2004.04.029
Kogiso,T.,Hirschmann,M.M.,Frost,D.J.,2003.HighPressure Partial Melting of Garnet Pyroxenite:Possible Mafic Lithologies in the Source of Ocean Island Basalts.Earth and Planetary Science Letters,216(4):603-617.https://doi.org/10.1016/s0012-821x(03)00538-7
Kuritani,T.,Kimura,J.I.,Miyamoto,T.,et al.,2009.Intraplate Magmatism Related to Deceleration of Upwelling Asthenospheric Mantle:Implications from the Changbaishan Shield Basalts,Northeast China.Lithos,112(3-4):247-258.https://doi.org/10.1016/j.lithos.2009.02.007
Kuritani,T.,Kimura,J.I.,Ohtani,E.,et al.,2013.Transition Zone Origin of Potassic Basalts from Wudalianchi Volcano,Northeast China.Lithos,156-159:1-12.https://doi.org/10.1016/j.lithos.2012.10.010
Kuritani,T.,Nakamura,E.,2002.Precise Isotope Analysis of Nanogram-Level Pb for Natural Rock Samples without Use of Double Spikes.Chemical Geology,186(1-2):31-43.https://doi.org/10.1016/s0009-2541(02)00004-9
Kuritani,T.,Ohtani,E.,Kimura,J.I.,2011.Intensive Hydration of the Mantle Transition Zone beneath China Caused by Ancient Slab Stagnation.Nature Geoscience,4(10):713-716.https://doi.org/10.1038/ngeo1250
Kurz,M.D.,Jenkins,W.J.,Hart,S.R.,1982.Helium Isotopic Systematics of Oceanic Islands and Mantle Heterogeneity.Nature,297(5861):43-47.https://doi.org/10.1038/297043a0
Kushiro,I.,2013.Partial Melting of a Fertile Mantle Peridotite at High Pressures:An Experimental Study Using Aggregates of Diamond.In:Kushiro,I.,ed.,Earth Processes:Reading the Isotopic Code.American Geophysical Union,Washington,D.C.,109-122.https://doi.org/10.1029/gm095p0109
Le Bas,M.J.,Le Maitre,R.W.,Streckeisen,A.,et al.,1986.AChemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram.Journal of Petrology,27(3):745-750.https://doi.org/10.1093/petrology/27.3.745
Li,H.Y.,Xu,Y.G.,Ryan,J.G.,et al.,2017.Olivine and Melt Inclusion Chemical Constraints on the Source of Intracontinental Basalts from the Eastern North China Craton:Discrimination of Contributions from the Subducted Pacific Slab.Geochimica et Cosmochimica Acta,178:1-19.https://doi.org/10.1016/j.gca.2015.12.032
Li,S.G.,Yang,W.,Ke,S.,et al.,2016.Deep Carbon Cycles Constrained by a Large-Scale Mantle Mg Isotope Anomaly in Eastern China.National Science Review,4(1):111-120.https://doi.org/10.1093/nsr/nww070
Li,Y.Q.,Ma,C.Q.,Robinson,P.T.,et al.,2015.Recycling of Oceanic Crust from a Stagnant Slab in the Mantle Transition Zone:Evidence from Cenozoic Continental Basalts in Zhejiang Province,SE China.Lithos,230:146-165.https://doi.org/10.1016/j.lithos.2015.05.021
Liu,J.Q.,Chen,L.H.,Wang,X.J.,et al.,2017.The Role of Melt-Rock Interaction in the Formation of Quaternary High-MgO Potassic Basalt from the Greater Khingan Range,Northeast China.Journal of Geophysical Research:Solid Earth,122(1):262-280.https://doi.org/10.1002/2016jb013605
Liu,J.Q.,Ren,Z.Y.,Nichols,A.R.L.,et al.,2015.Petrogenesis of Late Cenozoic Basalts from North Hainan Island:Constraints from Melt Inclusions and Their Host Olivines.Geochimica et Cosmochimica Acta,152:89-121.https://doi.org/10.1016/j.gca.2014.12.023
Liu,S.A.,Wang,Z.Z.,Li,S.G.,et al.,2016.Zinc Isotope Evidence for a Large-Scale Carbonated Mantle beneath Eastern China.Earth and Planetary Science Letters,444:169-178.https://doi.org/10.1016/j.epsl.2016.03.051
Liu,R.,X.,1992.Geochronology and Geochemistry of Cenozoic Volcanic Rocks in China.Seismological Press,Beijing(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
Meng,F.C.,Safonova,I.,Chen,S.S.,et al.,2018.Late Cenozoic Intra-Plate Basalts of the Greater Khingan Range in NE China and Khangai Province in Central Mongolia.Gondwana Research,63:65-84.https://doi.org/10.1016/j.gr.2018.05.009
Pertermann,M.,Hirschmann,M.M.,2003.Anhydrous Partial Melting Experiments on MORB-Like Eclogite:Phase Relations,Phase Compositions and Mineral-Melt Partitioning of Major Elements at 2-3GPa.Journal of Petrology,44(12):2173-2201.https://doi.org/10.1093/petrology/egg074
Pu,W.,Gao,J.F.,Zhao,K.D.,et al.,2005.Separation Method of Rb-Sr,Sm-Nd Using DCTA and HIBA.Journal of Nanjing University(Natural Sciences),41(4):445-450(in Chinese with English abstract).
Roeder,P.L.,Emslie,R.F.,1970.Olivine-Liquid Equilibrium.Contributions to Mineralogy and Petrology,29(4):275-289.https://doi.org/10.1007/bf00371276
Rudnick,R.L.,Gao,S.,2003.Composition of the Continental Crust.In:Rudnick,R.L.,Gao,S.,eds.,Treatise on Geochemistry.Elsevier,Cambridge,1-64.https://doi.org/10.1016/b0-08-043751-6/03016-4
Saal,A.,Kurz,M.,Hart,S.,et al.,2007.The Role of Lithospheric Gabbros on the Composition of Galapagos Lavas.Earth and Planetary Science Letters,257(3-4):391-406.https://doi.org/10.1016/j.epsl.2007.02.040
Saenger,C.,Wang,Z.R.,2014.Magnesium Isotope Fractionation in Biogenic and Abiogenic Carbonates:Implications for Paleoenvironmental Proxies.Quaternary Science Reviews,90:1-21.https://doi.org/10.1016/j.quascirev.2014.01.014
Spandler,C.,Yaxley,G.,Green,D.H.,et al.,2007.Phase Relations and Melting of Anhydrous K-Bearing Eclogite from 1 200to 1 600℃and 3to 5GPa.Journal of Petrology,49(4):771-795.
Starkey,N.A.,Stuart,F.M.,Ellam,R.M.,et al.,2009.Helium Isotopes in Early Iceland Plume Picrites:Constraints on the Composition of High 3 He/4 He Mantle.Earth and Planetary Science Letters,277(1-2):91-100.https://doi.org/10.1016/j.epsl.2008.10.007
Stracke,A.,2012.Earth's Heterogeneous Mantle:A Product of Convection-Driven Interaction between Crust and Mantle.Chemical Geology,330/331:274-299.https://doi.org/10.1016/j.chemgeo.2012.08.007
Stuart,F.M.,Lass-Evans,S.,Godfrey Fitton,J.,et al.,2003.High 3 He/4 He Ratios in Picritic Basalts from Baffin Island and the Role of a Mixed Reservoir in Mantle Plumes.Nature,424(6944):57-59.https://doi.org/10.1038/nature01711
Sun,S.S.,1980.Lead Isotopic Study of Young Volcanic Rocks from Mid-Ocean Ridges,Ocean Islands and Island Arcs.Philosophical Transactions of the Royal Society A:Mathematical,Physical and Engineering Sciences,297(1431):409-445.https://doi.org/10.1098/rsta.1980.0224
Sun,Y.B.,Zhang,R.,Ding,C.C.,et al.,2016.Adsorption of U(VI)on Sericite in the Presence of Bacillus Subtilis:ACombined Batch,EXAFS and Modeling Techniques.Geochimica et Cosmochimica Acta,180:51-65.https://doi.org/10.1016/j.gca.2016.02.012
Sun,Y.,Ying,J.F.,Su,B.X.,et al.,2015.Contribution of Crustal Materials to the Mantle Sources of Xiaogulihe Ultrapotassic Volcanic Rocks,Northeast China:New Constraints from Mineral Chemistry and Oxygen Isotopes of Olivine.Chemical Geology,405:10-18.https://doi.org/10.1016/j.chemgeo.2015.04.005
Tang,Y.J.,Zhang,H.F.,Nakamura,E.,et al.,2007.Lithium Isotopic Systematics of Peridotite Xenoliths from Hannuoba,North China Craton:Implications for Melt-Rock Interaction in the Considerably Thinned Lithospheric Mantle.Geochimica et Cosmochimica Acta,71(17):4327-4341.https://doi.org/10.1016/j.gca.2007.07.006
Tao,K.,Niu,F.L.,Ning,J.Y.,et al.,2014.Crustal Structure beneath NE China Imaged by NECESSArray Receiver Function Data.Earth and Planetary Science Letters,398:48-57.https://doi.org/10.1016/j.epsl.2014.04.043
Teng,F.Z.,2017.Magnesium Isotope Geochemistry.Reviews in Mineralogy and Geochemistry,82(1):219-287.https://doi.org/10.2138/rmg.2017.82.7
Teng,F.Z.,Li,W.Y.,Ke,S.,et al.,2010.Magnesium Isotopic Composition of the Earth and Chondrites.Geochimica et Cosmochimica Acta,74(14):4150-4166.https://doi.org/10.1016/j.gca.2010.04.019
Vervoort,J.D.,Plank,T.,Prytulak,J.,2011.The Hf-Nd Isotopic Composition of Marine Sediments.Geochimica et Cosmochimica Acta,75(20):5903-5926.https://doi.org/10.1016/j.gca.2011.07.046
Walter,M.J.,1998.Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere.Journal of Petrology,39(1):29-60.https://doi.org/10.1093/petrology/39.1.29
Wang,X.J.,Chen,L.H.,Hofmann,A.W.,et al.,2017.Mantle Transition Zone-Derived EM1Component beneath NEChina:Geochemical Evidence from Cenozoic Potassic Basalts.Earth and Planetary Science Letters,465:16-28.https://doi.org/10.1016/j.epsl.2017.02.028
Wang,Y.,Zhao,Z.F.,Zheng,Y.F.,et al.,2011.Geochemical Constraints on the Nature of Mantle Source for Cenozoic Continental Basalts in East-Central China.Lithos,125(3-4):940-955.https://doi.org/10.1016/j.lithos.2011.05.007
Wei,W.,Xu,J.D.,Zhao,D.P.,et al.,2012.East Asia Mantle Tomography:New Insight into Plate Subduction and Intraplate Volcanism.Journal of Asian Earth Sciences,60:88-103.https://doi.org/10.1016/j.jseaes.2012.08.001
Weis,D.,Kieffer,B.,Maerschalk,C.,et al.,2006.HighPrecision Isotopic Characterization of USGS Reference Materials by TIMS and MC-ICP-MS.Geochemistry,Geophysics,Geosystems,7(8).https://doi.org/10.1029/2006gc001283
Wombacher,F.,Eisenhauer,A.,B9hm,F.,et al.,2011.Magnesium Stable Isotope Fractionation in Marine Biogenic Calcite and Aragonite.Geochimica et Cosmochimica Acta,75(19):5797-5818.https://doi.org/10.1016/j.gca.2011.07.017
Workman,R.K.,Hart,S.R.,2005.Major and Trace Element Composition of the Depleted MORB Mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72.https://doi.org/10.1016/j.epsl.2004.12.005
Xiao,W.J.,Windley,B.F.,Sun,S.,et al.,2015.A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia:Oroclines,Sutures,and Terminal Accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507.https://doi.org/10.1146/annurev-earth-060614-105254
Xu,Y.G.,2007.Diachronous Lithospheric Thinning of the North China Craton and Formation of the Daxin'anlingTaihangshan Gravity Lineament.Lithos,96(1-2):281-298.https://doi.org/10.1016/j.lithos.2006.09.013
Xu,Y.G.,Li,H.Y.,Hong,L.B.,et al.,2018.Generation of Cenozoic Intraplate Basalts in the Big Mantle Wedge under Eastern Asia.Science China Earth Sciences,48(7):825-843(in Chinese).
Xu,Y.G.,Zhang,H.H.,Qiu,H.N.,et al.,2012.Oceanic Crust Components in Continental Basalts from Shuangliao,Northeast China:Derived from the Mantle Transition Zone?.Chemical Geology,328:168-184.https://doi.org/10.1016/j.chemgeo.2012.01.027
Xu,Z.,Zheng,Y.F.,Zhao,Z.F.,2017.The Origin of Cenozoic Continental Basalts in East-Central China:Constrained by Linking Pb Isotopes to Other Geochemical Variables.Lithos,268-271:302-319.https://doi.org/10.1016/j.lithos.2016.11.006
Yang,W.,Teng,F.Z.,Zhang,H.F.,et al.,2012.Magnesium Isotopic Systematics of Continental Basalts from the North China Craton:Implications for Tracing Subducted Carbonate in the Mantle.Chemical Geology,328:185-194.https://doi.org/10.1016/j.chemgeo.2012.05.018
Yang,Y.H.,Zhang,H.F.,Chu,Z.Y.,et al.,2010.Combined Chemical Separation of Lu,Hf,Rb,Sr,Sm and Nd from a Single Rock Digest and Precise and Accurate Isotope Determinations of Lu-Hf,Rb-Sr and Sm-Nd Isotope Systems Using Multi-Collector ICP-MS and TIMS.International Journal of Mass Spectrometry,290(2-3):120-126.https://doi.org/10.1016/j.ijms.2009.12.011
Yang,Z.F.,Li,J.,Liang,W.F.,et al.,2016.On the Chemical Markers of Pyroxenite Contributions in Continental Basalts in Eastern China:Implications for Source Lithology and the Origin of Basalts.Earth-Science Reviews,157:18-31.https://doi.org/10.1016/j.earscirev.2016.04.001
Yasuda,A.,Fujii,T.,Kurita,K.,1994.Melting Phase Relations of an Anhydrous Mid-Ocean Ridge Basalt from 3to 20GPa:Implications for the Behavior of Subducted Oceanic Crust in the Mantle.Journal of Geophysical Research:Solid Earth,99(B5):9401-9414.https://doi.org/10.1029/93jb03205
Yaxley,G.M.,Sobolev,A.V.,2007.High-Pressure Partial Melting of Gabbro and Its Role in the Hawaiian Magma Source.Contributions to Mineralogy and Petrology,154(4):371-383.https://doi.org/10.1007/s00410-007-0198-4
Yaxley,G.M.,Green,D.H.1998.Reactions between Eclogite and Peridotite:Mantle Refertilisation by Subduction of Oceanic Crust.Schweiz.Mineral.Petrogr.Mitt.,78(2):243-255.
Yu,S.Y.,Xu,Y.G.,Zhou,S.H.,et al.,2018.Late Cenozoic Basaltic Lavas from the Changbaishan-Baoqing Volcanic Belt,NE China:Products of Lithosphere-Asthenosphere Interaction Induced by Subduction of the Pacific Plate.Journalof Asian Earth Sciences,164:260-273.https://doi.org/10.1016/j.jseaes.2018.06.031
Zeng,G.,Chen,L.H.,Hofmann,A.W.,et al.,2011.Crust Recycling in the Sources of Two Parallel Volcanic Chains in Shandong,North China.Earth and Planetary Science Letters,302(3-4):359-368.https://doi.org/10.1016/j.epsl.2010.12.026
Zeng,G.,Chen,L.H.,Xu,X.S.,et al.,2010.Carbonated Mantle Sources for Cenozoic Intra-Plate Alkaline Basalts in Shandong,North China.Chemical Geology,273(1-2):35-45.https://doi.org/10.1016/j.chemgeo.2010.02.009
Zeng,G.,Chen,L.H.,Yu,X.,et al.,2017.Magma-Magma Interaction in the Mantle beneath Eastern China.Journal of Geophysical Research:Solid Earth,122(4):2763-2779.https://doi.org/10.1002/2017jb014023
Zhang,J.J.,Zheng,Y.F.,Zhao,Z.F.,2009.Geochemical Evidence for Interaction between Oceanic Crust and Lithospheric Mantle in the Origin of Cenozoic Continental Basalts in East-Central China.Lithos,110(1):305-326.https://doi.org/10.1016/j.lithos.2009.01.006
Zhang,L.Y.,Prelevi,D.,Li,N.,et al.,2016.Variation of Olivine Composition in the Volcanic Rocks in the Songliao Basin,NE China:Lithosphere Control on the Origin of the K-Rich Intraplate Mafic Lavas.Lithos,262:153-168.https://doi.org/10.1016/j.lithos.2016.06.028
Zhang,M.L.,Guo,Z.F.,2016.Origin of Late Cenozoic AbagaDalinuoer Basalts,Eastern China:Implications for a Mixed Pyroxenite-Peridotite Source Related with Deep Subduction of the Pacific Slab.GondwanaResearch,37:130-151.https://doi.org/10.1016/j.gr.2016.05.014
Zhang,R.Q.,Wu,Q.J.,Sun,L.,et al.,2014.Crustal and Lithospheric Structure of Northeast China from S-Wave Receiver Functions.Earth and Planetary Science Letters,401:196-205.https://doi.org/10.1016/j.epsl.2014.06.017
Zhang,Y.L.,Liu,C.Z.,Ge,W.C.,et al.,2011.Ancient SubContinental Lithospheric Mantle(SCLM)beneath the Eastern Part of the Central Asian Orogenic Belt(CAOB):Implications for Crust-Mantle Decoupling.Lithos,126(3-4):233-247.https://doi.org/10.1016/j.lithos.2011.07.022
Zhao,Y.W.,Fan,Q.C.,2011.Characteristics of Lithospheric Mantle beneath the Great Xing'an Range:Evidence from Spinel Peridotite Xenoliths in the Halaha River and Chaoer River Area.Acta Petrologica Sinica,27(10):2833-2841(in Chinese with English abstract).
Zhao,Y.W.,Fan,Q.C.,2012.Mantle Sources and Magma Genesis of Quaternary Volcanic Rocks in the Halaha River and Chaoer River Area,Great Xing'an Range.Acta Petrologica Sinica,28(4):1119-1129(in Chinese with English abstract).
Zhao,Y.W.,Fan,Q.C.,Bai,Z.D.,et al.,2008.Preliminary Study on Quaternary Volcanoes in the Halaha River and Chaoer River Area in Daxing'an Mountain Range.Acta Petrologica Sinica,24(11):2569-2575(in Chinese with English abstract).
Zhou,X.,Armstrong,R.,1982.Cenozoic Volcanic Rocks of Eastern China:Secular and Geographic Trends in Chemistry and Strontium Isotopic Composition.Earth and Planetary Science Letters,58(3):301-329.https://doi.org/10.1016/0012-821x(82)90083-8
Zou,H.B.,Zindler,A.,Xu,X.S.,et al.,2000.Major,Trace Element,and Nd,Sr and Pb Isotope Studies of Cenozoic Basalts in SE China:Mantle Sources,Regional Variations,and Tectonic Significance.Chemical Geology,171(1-2):33-47.https://doi.org/10.1016/s0009-2541(00)00243-6
陈立辉,曾罡,胡森林,等,2012.地壳再循环与大陆碱性玄武岩的成因:以山东新生代碱性玄武岩为例.高校地质学报,18(1):16-27.
陈霞玉,陈立辉,陈晹,等,2014.中国中-东部地区新生代玄武岩的分布规律与面积汇总.高校地质学报,20(4):507-519.
樊祺诚,隋建立,赵勇伟,等,2008.大兴安岭中部第四纪火山岩中石榴石橄榄岩捕虏体的初步研究.岩石学报,24(11):2563-2568.
樊祺诚,赵勇伟,李大明,等,2011.大兴安岭哈拉哈河-绰尔河第四纪火山分期:K-Ar年代学与火山地质特征.岩石学报,27(10):2827-2832.
刘若新,1992.中国新生代火山岩年代学与地球化学.北京:地震出版社.
濮巍,高剑峰,赵葵东,等,2005.利用DCTA和HIBA快速有效分离Rb-Sr、Sm-Nd的方法.南京大学学报(自然科学版),41(4):445-450.
徐义刚,李洪颜,洪路兵,等,2018.东亚大地幔楔与中国东部新生代板内玄武岩成因.中国科学:地球科学,48(7):825-843.
赵勇伟,樊祺诚,2011.大兴安岭岩石圈地幔特征:哈拉哈河-绰尔河橄榄岩捕虏体的证据.岩石学报,27(10):2833-2841.
赵勇伟,樊祺诚,2012.大兴安岭哈拉哈河-绰尔河第四纪火山岩地幔源区与岩浆成因.岩石学报,28(4):1119-1129.
赵勇伟,樊祺诚,白志达,等,2008.大兴安岭哈拉哈河-淖尔河地区第四纪火山活动初步研究.岩石学报,24(11):2569-2575.