数值模拟在地球动力学中的研究进展
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摘要
本文主要针对有限单元法,对近10几年来数值模拟在地球动力学中的应用和发展作了回顾,分为构造应力场模拟;地幔热对流模拟;板块碰撞模拟;岩石圈流变学模拟;以及地震机制与预测模拟等部分.简单阐述了当前地球动力学数值模拟的发展趋势并论述了其面临的主要问题.
Just aimed at finite element method,this paper gives a general review on the development and application of the numerical modeling in the Geodynamics research since the nineties.It contains sections on: numerical simulation of stress field and deformation field in structural geology;simulation on thermal convection of the mantle;simulation on the plate collision and convergence,including Continent-Continent collision and Ocean-Continental collision;modeling of Lithospheric Rheology;simulation on the mechanical of earthquake,and so on.At the end,this paper discusses the development tendency and mainly facing questions of numerical modeling.
Just aimed at finite element method,this paper gives a general review on the development and application of the numerical modeling in the Geodynamics research since the nineties.It contains sections on: numerical simulation of stress field and deformation field in structural geology;simulation on thermal convection of the mantle;simulation on the plate collision and convergence,including Continent-Continent collision and Ocean-Continental collision;modeling of Lithospheric Rheology;simulation on the mechanical of earthquake,and so on.At the end,this paper discusses the development tendency and mainly facing questions of numerical modeling.
引文
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[11]Farhad S,Jafar A H,Thermo-mechanical modeling of sub-duction of continental lithosphere[J].Physics of the Earthand Planetary Interiors,2002,131:185~203.
[12]Magali I.Billen,Michael G,A low viscosity wedge in sub-duction zones[J].Earth and Planetary Science Letters,2001,193,227~236.
[13]Shi Y L,Wang C Y.Two-demensional modeling of the P-T-tpaths of regional metamorphism in simple overthrust terrains[J].Geology,1987,15:1048~1051.
[14]Liu M,Yang Y Q,Extensional collapse of the Tibetan Plat-eau:Results of three-dimensional finite element modeling[J].J.Geophys.Res.,2003,108(8):1~15.
[15]Pysklywec R N.Evolution of subducting mantle lithosphereat a continental plate boundary[J].Geophysical Reseach Let-ters,2001,28(23):4399~4402.
[16]Pysklywec R N,Beaumont C,Fullsack P.Lithospheric de-formation during the early stages of continental collision:Nu-merical experiments and comparison with South Island,NewZealand[J].J.Geophys.Res.,2002,107(B7):ETG 1~19..
[17]England P,Molnar P,Active deformation of Asia:from kine-matics to dynamics[J].Science,1997,278:647~650.
[18]Zhong S J,Zuber M T.Crustal compensation during moun-tain-building[J].Geophysical Reseach Letters,2000,27(18):3009~3012.
[19]Soofi M A,King S D.Oblique convergence between India andEurasia[J].J.Geophys.Res.,2002,107(b5):ETG 1~8.
[20]Pysklywec R N,Shahnas M H.Time-dependent surface to-pography in a coupled crust-mantle convection model[J].Geo-phys.J.Int.,2003,154:268~278.
[21]Zhong S J,Michael G,Dynamic interaction between tectonicplates,subducting slabs,and the mantle[J].Earth Interac-tions,1997,1(3):1~18.
[22]C.P.Conrad,B.H.Bager,Mantle convection with strongsubduction zones[J].Geophys.J.Int.,2001,144:271~288.
[23]Robl J,Stüwe K.The role of indenter rheology during conti-nental collision:Concepts and application to the EasternAlps.(GeoMod Abstr.vol.);Bollettino di Geofisica.2004,45(suppl.1):133~135.
[24]Hunen J v,A.P.van den Berg,N.J.Vlaar,Variousmechanisms to induce present-day shallow flat subduction andimplications for the younger Earth:a numerical parameterstudy[J].Physics of the Earth and Planetary Interiors,2004,146:179~194.
[25]Michael A.Eberle,Olivier Grasset,Christophe Sotin,Anumerical study of the interaction between the mantle wedge,subducting slab,and overriding plate[J].Physics of theEarth and Planetary Interiors,2002,4158:1~12.
[26]Gerbault M,Willingshofer E.Lower crust indentation orhorizontal ductile flow during continental collision?[J].Tec-tonophysics,2004,387:169~187.
[27]Willett S,Beaumont C,Fullsack P.Mechanical model for thetectonics of doubly vergent compressional orogens[J].GEOL-OGY,1993,21:371~374.
[28]Sean D.Willett,Christopher Beaumont,Subduction of Asianlithospheric mantle beneath Tibet inferred from models ofcontinental collision[J].Nature,1994,369:642~645.
[29]Liu Z,Peter B.Finite element modeling of neotectonics inNew Zealand[J].J.Geophys.Res,2002,107(B12):ETG 1~18.
[30]汪素云,陈培善.中国及邻区现代构造应力场的数值模拟[J].地球物理学报,1980,23(1):35~45.
[31]焦明若,张国民,车时,刘杰.中国大陆及其周边地区构造应力场的数值计算及其在地震活动性解释上的应用[J].地震学报,1999,21(2):123~132.
[32]梅世蓉,车时.我国现代构造应力场方向与大小的数值模拟及其与地震活动的关系[A].见:梅世蓉地震科学研究论文选集(1993)[C],北京:地震出版社42:8~447.
[33]肖兰喜,朱元清,陶九庆,杜宪宋.岩石圈流变强度与中国大陆构造运动关系的探讨[J].西北地震学报,2003,25(4):304~311.
[34]安美建,石耀霖,李方全.用遗传有限单元反演法研究东亚部分地区现今构造应力场的力源和影响因素[J].地震学报,1998,20(3):225~231.
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