引文
[1]Dietz R S.Continent and ocean basin evolution by spreading of the sea floor[J].Nature,1961,190:854-857.
[2]Hess H H.History of Ocean Basins.Petrologic Studies(Buddington volume)[M].Geol Soc Amer.1962,599-620.
[3]Wilson J T.A new class of faults and their bearing on continental drift[J].Nature,1965,207:343-347.
[4]Morgan W J.Rises,trenches,great faults,and crustal blocks[J].Jour Geophys Res,1968,73:1959-1982.
[5]Morgan W J.Deep mantle convection plumes and plate motions[J].Amer Assoc Petrol Geol Bull,1972,56:203-213.
[6]Mackenzie D P,Morgan W J.Evolution of triple junctions[J].Narure,1969,224:125-133.
[7]Dewey J F,Bird J M.Mountain belts and the new global tectonics[J].Jour Geophys Res,1970,75:2625-2647.
[8]Richard Y,Doglioni C,Sabadini R.Differential rotation between lithosphere and mantle:a consequence of lateral mantle viscosity variation[J].Jour Geophys Res,1991,96:8407-8415.
[9]Stern R J.Subduction zones[J].Reviews of Geophysics,2002,40(4):1012-1049.
[10]Kerr B C,Klenpereer S.Wide-angle imaging of the Mariana sbuduction factory[J].2002,84(47),Full meet suppl.
[11]Tatsumi Y.The subduction factory:It’s role in the evolution of the Earth,ocean drilling in the 21stcentury[J].OD21 Newsletter,2003,14(3):5.
[12]周留煜.大洋板块俯冲带角度的变化特征及其影响因素分析[J].中山大学研究生学刊(自然科学、医学版),2012,33(1):44-62.
[13]罗立志.试论中国型(C-型)冲断带及其油气勘探问题[J].石油与天然气地质,1984,5(4):315-324.
[14]Bally A W.油气产状的地质动力背景[A].李汉渝,译.全球大地构造与石油勘探[C].北京:石油化学工业出版社,1975,10-31.
[15]罗志立,试评A-俯冲带术语在中国大地构造学中应用[J],石油实验地质,1994,16(4):317-324.
[16]Uyeda S,Kanamori H.Back-arc opening and the mode of subduction[J].Journal of Geophysical Research.1979,Part B:Solid Earth.84(B3):1049-1061.
[17]Cloos M,Shreve R L.Shear-zone thickness and the seismicity of Chilean-type and Marianas-type subduction zones[J].Geology,1996,24(2):107-110.
[18]Conrad C P,Bilek S et al.Great earthquakes and slab pull:interaction between seismic coupling and plate slab coupling[J].Earth And Planetary Science Letters,2004,218(1-2):109-122.
[19]Sugisaki R.Tectonic aspects of Andesite line[J].Nature physical science,1972,240:109-111.
[20]Sugisaki R.Chemical characteristics of volcanic rocks:Relation to plate movement[J].Lithos,1976,9(1):17-30.
[21]Miyashiro A.Volcanic Rock Series and Tectonic Setting[J].Annual Review of Earth And Planetary Sciences,1975,3:251-269.
[22]Jarrard R D.Relation among subduction parameters[J].Reviews of Geophysics,1986,24(2):217-284.
[23]Sdrolias M,Müller R D.“Controls on back-arc basin formation[J].”G-Cubed:Geochemistry,Geophysics,Geosystems:an electronic journal of the Earth sciences7(Q04016).2006.
[24]Molnar P,Atwater T.Interarc spreading and Cordilleran tectonics as alternates related to the age of subducted oceanic lithosphere[J].Earth and Planetary Sciences Letters,1978,41(3):330-340.
[25]姚华建,徐果明,肖翔,等.俯冲带几何特征的研究[J].地震地质,2003,25(2):220-226.
[26]曹明坚,秦克章,李继亮.平坦俯冲及其成矿效应的研究进展、实例分析与展望[J].岩石学报,2011,27(12):3727-3748.
[27]Gutscher M A,Maury R,Eissen J P,et al.Can slab melting be caused by flat subduction?[J].Geology,2000,28(6):535-538.
[28]Abbott D,Drury R,Smith W H,Flat to steep transition in subduction style.Geology,1994,22(10):937-940.
[29]Zhao D P.Global tomographic images of mantle plumes and subducting slabs insight in to deep dynamics[J].Physics of the Earth and Planetary Interiors,2004,146:3-34.
[30]King S D.Subduction zones:Observations and geodynamic models[J].Physics of the Earth and Planetary Interiors,2001,127:9-24.
[31]Burg J P.Two orogenic system and a transform-transfer Fault in the Himalayas:Evidence and consequences[J].Earth Science Frontiers,2006,13:27-46.
[32]Peacock S M,Wang K.Seismic consequences of warm versus cool subduction metamorphism:examples from southwest and northeast Japan[J].Science,1999,286:937-939.
[33]Kirby S.Taking the temperature of slabs[J].Nature,2000,403:31-34.
[34]Witze A.The start of the world as we know it[J].Nature,2006,442:128-131.
[35]Cawood P A,Kr ner A,Pisarevsky S.Precambrian plate tectonics:Criteria and evidence[J].GSA Today,2006,16(7):4-11.
[36]Stern R J.Evidence from ophiolites,blueschists,and ultra-high pressure metamorphic terranes that the modernepisode of subduction tectonics began in Neoproterozoic time[J].Geology,2005,33:557-560.
[37]Stern R J.板块构造启动的时间和机制:理论和经验探索[J].科学通报,2007,52(5):489-501.
[38]翟明国.华北克拉通的形成以及早期板块构造[J].地质学报,2012,86(9):1335-1349.
[39]翟明国.前寒武纪地质学——地球科学的基础学科[J].科技导报,2013,31(8):3.
[40]翟明国.华北前寒武纪成矿系统与重大地质事件的联系[J].岩石学报,2013,29(5):1759-1773.
[41]Condie K C and Kr ner A.When did plate tectonics begin?Evidence from the geologic record[J].Geological Society of America Special Paper,2008,440:281-294.
[42]牛耀龄.全球构造与地球动力学—岩石学与地球化学方法应用实例[M].科学出版社,2013,31-46.
[43]Simon T,Tracy R,Mark R,et al.Heading down early on?Start of subduction on Earth[J].Geology,2014,42(2):139-142.
[44]哈因V E.大地构造学和地球动力学现代问题——从板块构造学到全球动力学[J].长春地质学院院报,1996,26(4):361-367.
[45]万天丰.关于全球板块构造动力学的讨论[J].自然杂志,2005,27(5):262-268.
[46]Forsyth D,Uyeda S.On the relative importance of the driving forces of plate motion[J].The Geophysical Journal of the Royal Astronomical Society,1975,43:163-200.
[47]Lithgow-Bertelloni C,Richards M A.The dynamics of Cenozoic and Mesozoic plate motions[J].Reviews of Geophysics,1998,36(1):27-78.
[48]臧绍先,宁杰远.西太平洋俯冲带的研究及其动力学意义[J].地球物理学报,1996,39(2):188-202.
[49]张克亮,魏东平.环太平洋俯冲带内双地震带及其成因机制研究进展[J].地球物理学进展,2008,23(1):31-39.
[50]Müller R D,Landgrebe T C W.The link between great earthquakes and the subduction of oceanic fracture zones[J].Solid Earth,2012,3:447-465.
[51]Veith K F.The nature of the dual zone of seismicity in the Kurils arc[J].Eos Trans.AGU,1977,58,1232.
[52]Omoris,Kamiya S,Maruyama S,et al.Morphology of the intraslab seismic zone and devolatilization phase equilibria of the subducting slab peridotite[J].Bull Earth Res In st U niv Tokyo,2002,76:455-478.
[53]余日东,金振民.蛇纹石脱水与大洋俯冲带中源地震(70-300km)的关系[J].地学前缘,2006,13(2):191-204.
[54]黄德志,高俊,戴塔根.俯冲带流体作用的地球化学示踪[J].地学前缘,2001,8(3):131-140.
[55]Hans K.Earth’s deep water reservoir[J].Geology,2014,507:174-175.
[56]Thompson A B.Water in the Earth’s mantle[J].Nature,1992,358:295-302.
[57]Murakami.Water in erath’s lower mantle[J].Science,2002,295:1885-1887.
[58]刘嵘,陈能松,何谋春,等.俯冲带深部流体:来自超高压变质锆石晶内结构和包裹体的证据[J].地学前缘,2006,13(2):205-212.
[59]张立飞.洋壳深俯冲超高压变质作用研究及其地质意义[J].地质通报,2007,26(9):1079-1085.
[60]Bebout G E.The impact of subduction-zone metamorphism on mantle-ocean chemical cycling[J].Chem Geol,1995,126:191-218.
[61]Peacoch S M.Fluid processes in subduction zones[J].Science,1990,260:664-667.
[62]Davies J H,Stevenson D J.Physical model of source region of subduction zone volcanics[J].J Geophys Res,1992,97:2037-2070.
[63]Nadeau S,Philippot P,Pineau F.Fluid inclusion and mineral isotopic compositions(H-C-O)in eclogitic rocks as tracers of local fluid migration during highpressure metamorphism[J].Earth Planet Sci Lett,1993,114:431-448.
[64]Tatsumi Y.Migration of fluid phases and genesis of basalt magmas in subduction zones[J].J Geophys Res,1989,94:4697-4707.
[65]陈仁旭,郑永飞,龚冰.大陆俯冲带流体活动:超高压变质岩矿物水含量和稳定同位素制约[J].岩石学报,2011,27(2):451-468.
[66]Bourdon B,Turner S,Dosseto A.Dehydration and partial melting in subduction zones:Consraints from U-Series disequilibria[J].Journal of Geophysical Research,2003,108(B6):2291.
[67]Hawkesworth C J,Turner S P,Mcdermott F,et al.UTh isotopes in arc magmas:implications for element transfer from the subducted crust[J].1997,276:551-555.
[68]Turner S.On the time-scales of magmatism at islandarc volcanoes[J].Phil.Trans.R.Soc.London,2002,360:2853-2871.
[69]Ishikawa A,Kuritani T,Makishima A,et al.,Ancinet recycled crust beneth the Ontong Java Plateau:Isotopic evidence from the garnet clinopyroxenite xenoliths,Malaita,Solomom Islands[J].Earth and Planetary Science Letters,2007,259:134-148.
[70]李怀明,翟世奎,陶春辉,等.板块俯冲带岩浆作用过程的研究[J].海洋科学进展,2009,27(1):98-105.
[71]张树明,王方正.玄武岩在研究岩石圈深部过程及构造背景中的应用[J].地球科学进展,2002,17(5):685-692.
[72]邓鹤鸣,苏根利,李和平,等.俯冲带中水流体的化学性质研究进展[J].矿物岩石地球化学通报,2006,25(2):189-195.
[73]盛英明,郑永飞.大陆深俯冲带变质流体活动过程中原岩锆石的物理搬运和不活动性元素的化学迁移[J].科学通报,2013,58(22):2222-2226.
[74]赵振华,王强,熊小林.俯冲带复杂的壳幔相互作用[J].矿物岩石地球化学通报,2004,23(4):277-284.
[75]Nielsen S G,Rehkamper M,Brandon A D,et al.Thallium isotopes in Iceland and Azores lavas:Implication for the role of altered crust and mantle geochemistry[J].Earth and Planetary Science Letters,2007,264:332-345.
[76]Demidjuk Z,Turner S,Sandiford M,et al.U-series isotope and geodynamic constraints on mantle melting processes beneath the Newer Volcanic Province in South Australia[J].Earth and Planetary Science Letters,2007,261:517-533.
[77]Zellmer G F,Blake S,Vance D,et al.Plagioclase residence times at two island arc volcanoes(Kameni Island,Santorini,and Soufriere,St.Vincent)determined by diffusion systematics[J].Contributions to Mineralogy and Petrology,1999,136:345-357.
[78]Cashraman K V,Marsh B D,Crystal size distribution(CSD)in rocks and the kinetics and dynamics of crystallization(II Makaopuhi Lava Lake)[J].Global Geology,1992,63:118-136.
[79]Cheng Z M,Lu F X,Crystal size distribution in volcanic rocks in Laoshangou of Junggar Basin and significance of crystallization kinetics[J].Geoscience,1977,(2):149-156.
[80]Marsh B D,Crystal size distribution(CSD)in rocks and the kinetics and dynamics ofcrystallization I.Theory[J].Contributions to Mineralogy and Petrology,1988,99:277-291.
[81]Armienti P,Pareschi M T,Pompilio M.Effects of magma storage and ascent on the kinetics of crystal growth[J].Contributions to Mineralogy and Petrology,1994,115:402-414.
[82]Hawkesworth C J,O’ncons P K,Arculus R J.Nd and Sr isotope geochemistry of island arc volcanics,Grenada,Lesser Antilles[J].Earth Planet Sci Lett,1979,45:237-248.
[83]Perfit M R,Gust D A,Bence A E,et al.Chemical characteristics of island-arc basalts:Implications for mantle sources[J].Chem Geol,1980,30:227-256.
[84]Mc Culloch M T,Gamble J A.Geochemical and geodynamical constraints on subduction zone magmatism[J].Earth Planet Sci Lett,1991,102:358-374.
[85]Brenan J M,Shaw H F,Ryerson F J,et al.Mineralaqueous fluid partitioning of trace element at 900℃and2.0 GPa:constraints on the trace element chemistry of mantle and deep crustal fluids[J].Geochimica et Cosmochimica Acta,1995,59:3331-3350.
[86]Keppler H.Constraints from partitioning experiment on the composition of subduction-zone fluids[J].1996,380:237-240.
[87]Turner S,Hawkeworth C.Constrains on flux rates and mantle dynamics beneath island arcs from Tonga-Kermadec[J].Nature,1997,389:568-573.
[88]Debaille V,Doucelance R,Weis D,et al.Multi-stage mixing in subduction zones:application to Merapi volcano(Java island,Sunda arc)[J].Geochimica Cosmochimica Acta,2006,70:723-741.
[89]刘肇昌.板块构造学[M].成都:四川科学技术出版社,1983.
[90]王之田,秦克章,张守林.大型铜矿地质与找矿[M].北京:冶金工业出版社,1994.
[91]Thieblemont D,Stein G,Lescuyer J L.Gisements epithermaux et porphyriques:la connexion adakite[J].Earth Planet.Sci.Lett,1997,325:103-109.
[92]孙卫东,凌明星,杨晓勇,等.洋脊俯冲与斑岩铜金矿成矿[J].中国科学:地球科学,2010,40(2):127-137.
[93]芮宗瑶,侯增谦,李光明,等.俯冲、碰撞、深断裂和埃达克岩与斑岩铜矿[J].地质与勘探,2006,42(1):1-6.
[94]王元龙,张旗,王强,等.埃达克质岩与Cu-Au成矿作用关系的初步探讨[J].岩石学报,2003,19(3):543-550.
[95]刘洪涛,张旗,刘建明,等.埃达克岩与Cu-Au成矿作用:有待深入研究岩浆成矿关系[J].岩石学报,2004,20(2):205-218.
[96]曹明坚,秦克章,李继亮.平坦俯冲及其成矿效应的研究进展、实例分析与展望[J].岩石学报,2011,27(12):3727-3748.
[97]Defant M J,Drummond M S.Derivation of some modern arc magmas by melting of young subducted lithosphere[J].Nature,1990,347:662-665.
[98]Sajona F G,Maury R C.Association of adakites with gold and copper mineralization in the Philillines[J].CR ACAD SCI II A,1998,326(1):27-34.
[99]Rapp R P,Watson E B,Miller C F,Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites[J].Precambrian Research,1991,51:1-25.
[100]Rapp R P,Watson E B.Dehydration melting of metabasalt at 832 kbar:implications for continental growth and crust mantle recycling[J].Journal of Petrology,1995,36:891-931.
[101]Rapp R P,Shimizu N,Norman M D,et al.Reaction between slab-derived melts and peridotite in the mantle wedge:experimental constraints at 3.8 Gpa[J].Chemical Geology,1999,160:335-356.
[102]Sen C,Dunn T.Dehydration melting of a bassltic composition amphibolite at 1.5 and 2.0GPa:implications for the origin of adakites[J].Contributions to Mineralogy and Petrology,1994,117:394-409.
[103]Hedenquist J W,Lowenstern J B.The role of magmas in the formation of hydrothermal ore deposites[J].Nature,1994,70:519-526.
[104]Kay S M,Mpodozis C.Central Andean ore deposits linker to evolving shallow subduction systems and thicking crust[J].GSA Today,2001,4-9.
[105]Atherton M P,Petford N.Generation of sodium-rich magmas from newly underplated basaltic crust[J].Nature,1993,362:144-146.
[106]Mungall J E.Roasting the mantle:Slab melting and the genesis of major Au-rich Cu deposits[J].Geology,2002,30:915-918.
[107]张玉泉,谢应霞,梁华英,等.1998.藏东玉龙铜矿带含矿斑岩及成岩系列[J].27(3):236-243.
[108]张旗,许继峰,王焰,等.埃达克岩的多样性[J].地质通报,2004,23(9-10):957-965.
[109]侯增谦,莫宣学,高永丰,等.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩—以西藏和智利斑岩铜矿为例[J].矿床地质,2003,22(1):1-12.