板片深部俯冲动力学研究的新进展
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
高精度的层析成像结果显示了全球范围内形态各异的俯冲板片,这充分表明地球动力学过程的复杂性.本文简单回顾了影响板片俯冲的主要因素和对俯冲板片有关的,如对地震、火山、弧后变形等地球物理现象的各种合理解释.讨论中国东北新生代火山的地球动力学背景可能是不同于一般俯冲带火山的成因.
Global seismic tomography results with high resolution show that the slabs may have complex forms,which indicates the complicated process of geodynamics.Here,we collect main factors which influence slab subduction and reasonable views on geophysical scenarios related to slab subduction,such as earthquake,volcanism,and back-arc deformation,and discuss geodynamic settings of Cenozoic volcanism in NE China,which may be different from common volcanism related to subduction.
引文
[1]Schubert G,Turcotte D L,Olson P.Mantle convectionin the earth and planets[M].2003:Cambridge Univ.Press.
    [2]李荫亭.地幔对流(讲座)[J].地震地磁观测与研究,1997,18(2):1~10.Li Y T.Mantle convection(Lecture)[J].Seismological and Geomagnetic Observation and Research(in Chinese),1997,18(2):1~10.
    [3]石耀霖.地幔对流研究的一些新进展[J].地球科学进展,2001,16(4):496~500.Shi Y L.Advances in mantle convection study[J].Advances in Earth Science(in Chinese),2001,16(4):496~500.
    [4]朱涛.地幔动力学研究进展-地幔对流[J].地球物理学进展,2003,18(1):65~73.Zhu T.Progress in mantle dynamics--mantle convection[J].Progress in Geophysics(in Chinese),2003,18(1):65~73.
    [5]吴爱弟,李文军,等.地幔对流的数值模拟方法[J].地学前缘,1998,5(Suppl.):41~48.Wu A D,Li WJ.Areviewon the numerical simulation of the mantle convection[J].Earth Science Frontiers(in Chinese).1998,5(Suppl.):41~48.
    [6]Richter F M.Convection and the large-scale circulation of the mantle[J].J.Geophys.Res.,1973,78:8735~8745.
    [7]Christensen U R,Yuen D A.Layered convection induced by Phase Transitions[J].J.Geophys.Res.,1985,90:10291~10300.
    [8]Becker T W,Kellogg L H,O′Connell R J.Thermal con-straints on the survival of primitive blobs in the lower mantle[J].Earth Planet Sci Lett.,1999,171:351~365.
    [9]Kellogg L H,Hager B H,van der Hilst R D.Compositional stratificationin the deep mantle[J].Science,1999,283:1881~1884.
    [10]Bercovici D,Karato S I.Whole-mantle convection and the transition-zone water filter[J].Nature,2003,425(4):39~44.
    [11]Huang J S,Zhong S J,Hunen J V.Controls on sublithos-pheric small-scale convection[J].J.Geophys.Res.,2003,108(B8):1~13.
    [12]常筱华,张群山,董树谦,黄建华,傅蓉珊.利用地震层析成像数据计算地幔对流新模型的探讨[J].地球物理学报,2003,46(6):772~778.Chang X H,Zhang Q S,Dong S Q,Huang J H,Fu R S.A new mantle convection model constrained by seismic tomo-graphy data[J].Chinese J.Geophys.(in Chinese),2003,46(6):772~778.
    [13]van der Hilst R D,Karason H.Compositional heterogeneity in the bottom1000Kilometers of Earth′s mantle:toward a hybrid convection model[J].Science,1999,1885~1888.
    [14]朱涛,马宗晋,冯锐.三维地震波结构约束下的变黏度地幔对流及其动力学意义[J].地球物理学报,2006,49(5):1347~1358.Zhu T,Ma ZJ,Feng R.3-Dlateral variable viscosity mantle convection constrained by seismic wave velocity and its geo-dynamic implications[J].Chinese J.Geophys.(in Chinese),2006,49(5):1347~1358.
    [15]傅蓉珊,王毅,黄建华,等.黏滞分层地幔中密度异常驱动对流模型的研究[J].地球物理学报,2005,48(4):824~833.Fu R S,Wang Y,Huang J H,Chang X H,Zha X J,Dai Z Y.Effect of rheology structure on flow patterns driven by density anomaly in the mantle[J].Chinese J.Geophys.(in Chinese),2005,48(4):824~833
    [16]Ricards M R,Gordon R,van der Hilst R D.Processes and consequences of deep subduction:introduction[J].,Phys.Earth Planet.Int.,2001,127:1~7.
    [17]Widiyantoro S,Kennett B L N,van der Hilst R D.Seismic tomography with Pand S data revealslateral variationsinthe rigidity of deep slabs[J].Earth Planet.Sci.Lett.,1999,173:91~100.
    [18]King S D.Subduction zones:observations and geodynamics models[J].Phys.Earth Planet.Int.,2001,127:9~24.
    [19]Guillou-Frottier L,Buttles J,Olson P A.laboratory experi-ments on the structure of subducted oceanic lithosphere[J].Earth Planet.Sci.Lett.,1995,133:19~34.
    [20]Christensen U R,Yuen D A.The interaction of a subducting lithospheric slab with a chemical or phase boundary[J].J.Geophys.Res.,1984,89:4389~4402.
    [21]Gurnis M,Hager B H.Controls on the structure on subduc-ted slabs[J].nature,1988,335:317~321
    [22]Gaherty J B,Hager B H.Compositional versus thermal buoyancy and the evolution of subducted lithosphere[J].Geophys,Res.Lett.,1994,21:141~144.
    [23]Houseman G A,Gubbins D.Deformation of subducted oce-anic lithosphere[J].Geophys.J.In.,1997,131:535~551.
    [24]Cizkova H,Matyska C.Layered convection with aninterface at a depth of1000km:stability and generation of slab-like downwellings[J].Phys.Earth Planet.Int.,2004,141:269~279.
    [25]Cserepes L,Yuen D A,Schroeder B A.Effect of the mid-mantle viscosity and phase-transition structure[J].Phys.Earth Planet.Int.,2000,118:135~148.
    [26]Zhong S,Zuber MT.Role of temperature-dependent viscosi-ty and surface plates in spherical shell models of mantle con-vection[J].J.Geophys.Res.,2000,105(B5):11063~11082.
    [27]Watts A B,Zhong S.Observations of flexure andthe rheolo-gy of oceanic lithosphere[J].Geophys.Res.Lett.,2000,142:855~875.
    [28]Zhong S,Gurnis M.Dynamic interaction between tectonic plates,subducting slabs,and the mantle[J].Earth Interac-tions,1997,1(3):1~18.
    [29]唐户俊一郎,著.何昌荣,等译.流变与地球动力学[M].北京:地震出版社,2005,99~105.
    [30]Solheim L P,Peltier WR.Phase boundary deflections at660kmdepth and episodically layered isochemical convection in the mantle[J].J.Geophys.Res.,1994,99(B8):15861~15875.
    [31]Tackley P J.On the penetration of an endothermic phase transition by upwellings and downwellings[J].J.Geophys.Res.,1995,100(B8):15477~15488.
    [32]Ita J,King S D,Sensitivity of convection with an endother-mic phase change to the form of governing equations,initial conditions,boundary conditions,and equation of state[J].J.Geophys.Res.,1994,99(B8):15919~15938.
    [33]Murakami M,Hirose K,Kawamura K.Post-perovs-kitephase transitionin MgSi O3[J].Science,2004,304:855~858.
    [34]Nakagawa T,Tackley P J.Effects of a perovskite-postper-ovskite phase change near core-mantle boundaryincompressi-ble mantle convection[J].Geophys.Res.Lett.,2004,31,L16611,doi:10.1029/2004GL020648
    [35]Matyska C,Yuen D A.The importance of radiative heat.transfer on superplumes in the lower mantle with the new post-perovskite phase change[J].Earth Planet.Sci Lett.,2005,234:71~81.
    [36]王建,叶正仁.地幔对流对全球岩石圈应力产生与分布的作用[J].地球物理学报,2005,48(3):584~590.Wang J,Ye Z R.Effects of mantle flow on generation and distribution of global lithospheric stress field[J].Chinese J.Geophys.(in Chinese),2005,48(3):584~590
    [37]Becker T W,O'Connell R J.Predicting plate velocities with mantle circulation models[J].Geochem.Geophy.,Geosyst.,2001,2(10.1029/2001GC000171).
    [38]叶正仁.全球地表热流的产生与分布[J].地球物理学报,2001,44(2):171~179.Ye Z R.Generation and distribution of global heat flow[J].Chinese J.Geophys.(in Chinese),2001,44(2):171~179.
    [39]叶正仁,王建.上地幔变黏度小尺度对流的数值研究[J].地球物理学报,2003,46(3):335~344.Ye Z R,Wang J.A numerical research on the small-scale convection with variable viscosity in the upper mantle[J].Chinese J.Geophys.(in Chinese),2003,46(3):335~344.
    [40]Becker T,Boschi L.A Comparison of tomographic geody-namic mantle models[J].Geochem.,Geophy.,Geosyst.,2002,3(10.129/2001GC000168).
    [41]Tackley P J,Stevenson DJ,Glatzmaizer G A,et al.Effects os multiple phase transitions in a three-dimensional spherical model of convectionin Earth’s mantle[J].J.Geophys.Res.,1994,99(B8):15877~15901.
    [42]Zhong S,Grunis M.Role of plates and temperature-depend-ent viscosityin phase change dynamics[J].J.Geophys.Res.,1994,99(B8):15903~15917.
    [43]孙荀英,王其允.海沟后退对地幔对流的影响[J].地球物理学报,1994,37(6):738~746.
    [44]Lebedev S,Chevrot S,van der Hilst R D.The660-km dis-continuity within the subducting NW-Pacific lithospheric slab[J].Earth Planet.Sci.Lett.,2002,205:25~35.
    [45]Gou Fujie,Ito A,Kodaira S,et al.Confirming sharp bending of the Pacific plate in the northern Japan trench subduction zone by applying a traveltime mapping method[J].Earth Planet.Sci.Lett.,2006,157:72~85.
    [46]Monnereau M,Quere S.Spherical shell models of mantle con-vection with tectonic plates[J].Earth Planet.Sci.Lett.,2001,184:575~587.
    [47]Bercovici D.The generation of plate tectonics from mantle convection[J].Phys.Earth Planet.Int.,2003,205:107~121.
    [48]Schellart WP.Influence of the subducting plate velocity on the geometry of the slab and migration of the subduction hinge[J].Earth Planet.Sci.Lett.,2005,231:197~219.
    [49]Davies J H.Simple analytical model for subduction zone ther-mal structure[J].Geophys.J.Int.,1999,139:823~828.
    [50]Hunen J V,van der Berg AP,Vlaar NJ.Athermo-mechan-ical model of horizontal subduction belowan overriding plate[J].Earth Planet.Sci.Lett.,2000,182:157~169.
    [51]Frohlich C.Asimple analytical method to calculate the ther-mal parameter and temperature within subducted lithosphere[J].Phys.Earth Planet.Int.,2006,155:281~285.
    [52]Bilen MI,Gurnis M.Alow viscosity wedge in subduction zones[J].Earth Planet.Sci.Lett.,2001,193:227~236.
    [53]Eberle M A,Grasset O,Sotin C.A numerical study of the interaction between the mantle wedge,subducting slab and overriding plate[J].Phys.Earth Planet.Int.,2002,134:191~202.
    [54]Gerya T V,Yuen D A,Maresch W V.Thermomechanical modeling of slab detachment[J].Earth Planet.Sci.Lett.,2004,226:101~116.
    [55]Karason H,van der Hilst R D.Constraints on mantle convec-tion fromseismic tomography[J].American Geophysical U-nion,Washington,DC.Geophys.Mon.,2000,121:277~288.
    [56]Bilek S L,Conrad C P,Bertelloni C L.Slab pull,slab weake-ning,and their relation to deepintra-slab seismicity[J].Geo-phys.Res.Lett.,2005,32:L14305.
    [57]Conrad C P,Billek S,Lithgoe-Bertelloni C.Great earth-quake and slab pull:interaction between seismic coupling and plate-slab coupling[J].Earth Planet.Sci.Lett.,2004,218:109~122.
    [58]Burnley P C,Green II H W.Faulting associated with the oli-vine to spinel transformationin Mg2GeO4anditsimplications for deep-focus earthquakes[J].J.Geophys.Res.,2002,96:425~443.
    [59]Mosenfelder J L,Marton F C,Ross II C R,et al.Experimen-tal constraints onthe depth of olivine metastabilityin subduc-ting lithosphere[J].Phys.Earth Planet.Int.,2001,127:165~180.
    [60]Collier J D,Helffrich G R,Wood BJ.Seismic discontinuitiesand subduction zones[J].Phys.Earth Planet.Int.,2001,127:35~49.
    [61]Brudzinski M R,Chen WP.Earthquakes and strain in sub-horizontal slabs[J].J.Geophys.Res.,2005,110:B08303.
    [62]Das S.Seismicity gaps and the shape of the seismic zone in the Banda Sea regionfromrelocated hypocenters[J].J.Geo-phys.Res.,2004,109:B12303.
    [63]Bina C R.Patterns of deep seismicity reflect buoyancy stres-ses due to phase transitions.Geophys,Res.Lett.,1997,24(24):3301~3304.
    [64]Regard V,Faccenna C,Martinod J,et al.Slab pull andinden-tation tectonics:insights from3Dlaboratory experiments[J].Phys.Earth Planet.Int.,2005,149:99~113.
    [65]石耀霖,张健.中国东北远离海沟陆内弧后扩张形成新生代火山的深部地球动力学背景[J].地震学报,2004,26(Supp):1~8.Shi Y L,Zhang J.Deep geodynamics of far field interconti-nental back-arc extension formation of cenozoic volcanoes in northeastern china[J].Acta Seismologica Sinica(in Chi-nese),2004,26(Supp):1~8.
    [66]石耀霖,张健.活动海岭俯冲与岛弧火山活动的热模拟研究[J].地球物理学报,1998,41(2):174~181.Shi Y L,Zhang J.Thermal modeling of active ridge subduc-tion and arc volcanism[J].Acta Geophysica Sinica(in Chi-nese),1998,41(2):174~181.
    [67]Wang Z,Zhao D.VpandVstomography of Kyushu,Japan:Newinsight into arc magmatismand forearc seismotectonics[J].Earth Planet.Int.Phys.,2006,157:269~285.
    [68]Honda S,Saito M.Small-scale convection under the back-arc occurringin the low viscosity wedge[J].Earth Planet.Sci.Lett.,2003,216:703~715.
    [69]Arcay D,Tric E,Doin M P.Numerical simulations of sub-duction zones:Effect of slab dehydration on the mantle wedge dynamics[J].Phys.Earth Planet.Inter.,2005,149:133~153.
    [70]Gerya T V,Connolly J A D,Yuen D A,et al.Seismic impli-cations of mantle wedge plumes[J].Phys.Earth Planet.In-ter.,2006,156:59~74.
    [71]ten Brink US,Shimizu N,Molzer P C.Plate deformation at depth under northern California:slab gap or stretched slab?[J].Tectonics,1999,18:1084~1098.
    [72]van Wijk J W,Govers R,Furlong K P.Thre-dimensional thermal modeling of the California upper mantle:a slab win-dowvs.stalled slab[J].Earth Planet.Sci.Lett.,2001,186:175~186.
    [73]Currie C A,Hyndman R D.The thermal structure of sub-duction zone back arcs[J].J.Geophys.Res.,2006,111:B08404.
    [74]Kelley K A,Plank T,and Grove T L,et al.Mantle melting as a function of water content beneath back-arc basins[J].J.Geophys.Res.,2006,111:B09208.
    [75]Heure A,Lallemand S.Plate motions,slab dynamics and back-arc deformation[J].Earth Planet.Sci.Lett.,2005,149:31~51.
    [76]Faccenna C,Funiciello F,Giardini D.Episodic back-arc ex-tension during restricted mantle convection in the Central Mediterranean[J].Earth Planet.Sci.Lett.,2001,187:105~116.
    [77]Bellahsen N,Faccenna C,Funiciello F.Dynamics of subduc-tion and plate motionin laboratory experiments:insights into the“plate tectonics”behavior of the Earth[J].J.Geophys.Res.,2005,110:B01401.
    [78]何建坤,刘福田.俯冲板片形貌特征和活动大陆边缘演化体制的关系[J].地球物理学进展,1998,13(2):15~25.
    [79]赵大鹏,雷建设,唐荣余.中国东北长白山火山的起源:地震层析成像证据[J].科学通报,2004,49(14):1439~1446.
    [80]雷建设,赵大鹏.长白山火山的起源和太平洋俯冲板块之间的关系[J].地球科学进展,2004,19(3):364~367.Lei J S,Zhao D P.The relationship betweenthe origin of the intraplte changbai volcano andthe subducting pacific slab[J].Advances in Earth Science(in Chinese),2004,19(3):364~367.
    [81]刘嘉麒.论中国东北大陆裂谷系的形成与演化[J].地质科学,1989,3:209~216.
    [82]王东方.中国东部中新生代裂谷火山岩带[J].长春地质学院学报,1985,3:49~56.
    [83]Wang F,Zhou X H,Zhang L C,et al.Late mesozoic volcan-ismin the great Xing'an range(NE China):Timing andimpli-cations for the dynamic setting of NE Asia[J].Earth Planet Sci Lett.,2006,25:179~198.
    [84]刘嘉麒,王松山.长白山火山与天池的形成时代[J].科学通报,1982,21:1312~1315.
    [85]杨卓欣,张先康,赵金仁,杨健,段玉玲,王帅军.长白山天池火山区三维地壳结构层析成像[J].地球物理学报,2005,48(1):106~114.Yang Z X,Zhang X K,Zhao J R,Yang J,Duan Y L,Wang S J.Tomographic imaging of3-D crustal structure beneath Changbaishan-Tianchi volcano region[J].Chinese J.Geo-phys.(in Chinese),2005,48(1):106~114.
    [86]段永红,张先康,刘志,原秦喜,王夫运,方盛明,杨卓欣.长白山-镜泊湖火山区地壳结构接收函数研究[J].地球物理进展,2005,48(2):352~358.Duan Y H,Zhang X K,Liu Z,Yuan Q X,Xu Z F,Wang F Y,Fang S M,Yang Z X.A study on crustal structures of Changbaishan-Jingpohu volcanic area using receiver functions[J].Chinese J.Geophys.(in Chinese),2005,48(2):352~358
    [87]程先琼,朱介寿,蔡学林.全球地幔垂直流动速度研究[J].地球物理学报,2006,49(4):1022~1028.Cheng X Q,Zhu J S,Cai X L.Astudy of global vertical ve-locity of mantle flow[J].Chinese J.Geophys.(in Chinese),2006,49(4):1022~1028
    [88]Xiaoge H,Yousheng X,shun-ichiro K.Water content in the transition zone fromelectrical conductivity of wadsleyite andringwoodite[J].Nature,2005,434:746~749.
    [89]段永红,张先康,刘志,方盛明,王夫运,徐朝繁,原秦喜.长白山-镜泊湖火山区上地幔间断面接收函数研究[J].地球物理学报,2005,48(4):834~842.Duan Y H,Zhang X K,Liu Z,Fang S M,Wang F Y,Xu Z F,Yuan Q X.Study on upper mantle discontinuities using the receiver functionin the Changbaishan—Jingpohu volcan-ic area[J].Chinese J.Geophys.(in Chinese),2005,48(4):834~842
    [90]Shearer P M,Flanagan M P.Seismic velocity and density jumps across the410and660kilometer discontinuities[J].Science,1999,285(3):1545~1548.
    [91]张瑞青,李永华,姚雪绒.西北太平洋俯冲带东北地区壳幔结构研究进展[J].地球物理学进展,2006,21(4):1080~1085.Zhang R Q,Li Y H,Yao X R.Areviewof latest crustal and upper mantle discontinuities studies beneath northeast China in northwest Pacific subduction zone[J].Progress in Geo-physics(in Chinese),2006,21(4):1080~1085.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心