青藏高原区域地震波研究综述
|
摘要
区域地震波携带着大量的信息,可以很好地反映地壳和上地幔结构的变化.本文简要总结了青藏高原地区区域地震波的研究方法与进展;对青藏高原区域地震波研究的结论进行了总结,并探讨了它们的地质意义.最后分析了目前青藏高原区域地震波研究中存在的一些问题.
Regional seismic wave carries lots of information about structural variations in the crust and the upper mantle.In this article,the author provides a review of the research methods and the results and discusses their implications for the structure and tectonics beneath the Tibetan plateau. Finally,we probe into the problem existing in the research direction.
Regional seismic wave carries lots of information about structural variations in the crust and the upper mantle.In this article,the author provides a review of the research methods and the results and discusses their implications for the structure and tectonics beneath the Tibetan plateau. Finally,we probe into the problem existing in the research direction.
引文
[1]藤吉文,胡家富,张中杰,等.喜马拉雅碰撞造山带和羌塘盆地的瑞雷波频散与三维速度结构[J].石油地球物理学报,1998,33(5):632~648.
[2]Rapine R,Tilmann F,West M,Ni J,Rodgers A.Crustalstructure of northern and western Tibet from surface wave dis-persion analysiscture of northern and western Tibet from sur-face wave dispersion analysis[J].J Geophys Res,2003,108(B2):2120~2129.
[3]Ni J,Barazangi M.High-frequency seismic wave propagationbeneath the Indian shield,Himalayan Arc,Tibetan plateauand surrounding regions:high uppermost mantle velocities andefficient Sn propagation beneath Tibet[J].Geophys J R As-tron Soc,1983,72:665~689.
[4]McNamara D E,et al.Upper mantle velocity structure beneathTibetan plateau from Pn travel time tomography[J].J GeophyRes,1997,102(B1):493~505.
[5]吴庆举,等.用宽频带远震接收函数研究青藏高原的地壳结构[J].地球物理学报,1998,41(5):669~679.
[6]吴庆举,曾融生,赵文津.喜玛拉雅-青藏高原的上地幔倾斜构造与陆-陆碰撞过程[J].中国科学(D辑),2005,(已提交,待发表).
[7]Zhu L P,Thomas J Owens,George E.Randall.Lateral varia-tion in crustal structure of the northern tibetan plateau inferredfrom teleseismic receiver function[J].Bulletin of the Seismo-logical Society of America,1995,85(6):1531~1540.
[8]丁志峰,曾融生.青藏高原横波分裂的观测研究[J].地球物理学报,1996,39(2):211~219.
[9]Sandvol E,Ni J,Kind R.Azimuthal anisotropy beneath thesouthern Himalayas-Tibet collision zone[J].Journ GeophysRes,1997,102:17813~17823.
[10]Huang W C,et al.Seismic polarization anistrophy beneaththe central Tibetan plateau[J].J Geophys Res,2000,105(B12):27979~27989.
[11]Zhao W,Mechie J,Brown L D,Guo J,Haines S,Hearn T,et al.Crustal structure of the central Tibet as derived fromproject INDEPTH wide-angle seismic data[J].Geophys JInt,2001,145:486~498.
[12]Zhao W,Mechie J,Guol J,Wenzel F,Meissner R,Ratsch-bacher L,Steentoft H,Husen S.Seismic mapping of crustalstructures beneath the Indus-Yarlung Suture,Tibet[J].Ter-ra Nova,1997,9(2):42~46.
[13]Andrew R Ross,Larry D Brown,Passakorn Pananont K D.Nelson,Simon Klemperer,Seth Haines,Zhao Wenjin,GuoJingru.Deep reflection surveying in central Tibet:lower-crustal layering and crustal flow[J].Geophysical Journal In-ternational,2004,156(1):115~128.
[14]Oliver J,Ewing M.Higher mode surface waves and theirbearing on the structure of the Earth's mantle[J].Bull SeismSoc Am,1957,47:187~204.
[15]Gutenberg B.Channel waves in the Earth's crust[J].Geo-physics,1955,20:283~294.
[16]Mitchell B J,Pan Y,Xie J,Cong L.Lg coda Q variationacross Eurasia and its relation to crustal evolution[J].J Geo-phys Res,1997,102:22767~22780.
[17]丁志锋,曾融生,等.青藏高原的Pn波速度和Moho面的起伏[J].地震学报,1992,14(增刊):592~599.
[18]裴顺平.中国大陆上地幔顶部体波速度层析成像[D].北京:中国地震局地球物理研究所,2002.
[19]汪素云,等.中国大陆上地幔顶部Pn速度结构[J].中国科学(D辑),2001,31(6):449~454.
[20]汪素云,许忠淮,等.中国大陆Pn速度结构与强震孕育的深部背景[J].地球物理学报,2003,46(6):779~785.
[21]许忠淮,汪素云.青藏高原东北缘地区Pn波速度的横向变化.地震学报,2003,25(1):24~31.
[22]McNamara D E,Owens T J,Walter W R.Propagationcharacteristics of Lg across the Tibetan Plateau[J].Bull SeisSoc Am,1996,86:457~469.
[23]Rapine R R,Ni J F,Hearn T M.Regional wave propagationin China and its surrounding regions[J].Bull Seis Soc Am,1997,87:1622~1636.
[24]Zhao Cuiping,Kennettl B L N,Furumura T.Contrasts inregional seismic wave propagation to station WMQ in centralAsia[J].Geophys J Int,2003,155:44~56.
[25]Hearn T M.Anisotropic Pn tomography in the western Unit-ed States[J].J Geophys Res,1996,101(B4):8403~8414.
[26]Haines S S,et al.INDEPTH-Ⅲseismic data:from surfaceobservations to deep crustal processes in Tibet[J].Tectonics,2003,22(1):1~18.
[2]Rapine R,Tilmann F,West M,Ni J,Rodgers A.Crustalstructure of northern and western Tibet from surface wave dis-persion analysiscture of northern and western Tibet from sur-face wave dispersion analysis[J].J Geophys Res,2003,108(B2):2120~2129.
[3]Ni J,Barazangi M.High-frequency seismic wave propagationbeneath the Indian shield,Himalayan Arc,Tibetan plateauand surrounding regions:high uppermost mantle velocities andefficient Sn propagation beneath Tibet[J].Geophys J R As-tron Soc,1983,72:665~689.
[4]McNamara D E,et al.Upper mantle velocity structure beneathTibetan plateau from Pn travel time tomography[J].J GeophyRes,1997,102(B1):493~505.
[5]吴庆举,等.用宽频带远震接收函数研究青藏高原的地壳结构[J].地球物理学报,1998,41(5):669~679.
[6]吴庆举,曾融生,赵文津.喜玛拉雅-青藏高原的上地幔倾斜构造与陆-陆碰撞过程[J].中国科学(D辑),2005,(已提交,待发表).
[7]Zhu L P,Thomas J Owens,George E.Randall.Lateral varia-tion in crustal structure of the northern tibetan plateau inferredfrom teleseismic receiver function[J].Bulletin of the Seismo-logical Society of America,1995,85(6):1531~1540.
[8]丁志峰,曾融生.青藏高原横波分裂的观测研究[J].地球物理学报,1996,39(2):211~219.
[9]Sandvol E,Ni J,Kind R.Azimuthal anisotropy beneath thesouthern Himalayas-Tibet collision zone[J].Journ GeophysRes,1997,102:17813~17823.
[10]Huang W C,et al.Seismic polarization anistrophy beneaththe central Tibetan plateau[J].J Geophys Res,2000,105(B12):27979~27989.
[11]Zhao W,Mechie J,Brown L D,Guo J,Haines S,Hearn T,et al.Crustal structure of the central Tibet as derived fromproject INDEPTH wide-angle seismic data[J].Geophys JInt,2001,145:486~498.
[12]Zhao W,Mechie J,Guol J,Wenzel F,Meissner R,Ratsch-bacher L,Steentoft H,Husen S.Seismic mapping of crustalstructures beneath the Indus-Yarlung Suture,Tibet[J].Ter-ra Nova,1997,9(2):42~46.
[13]Andrew R Ross,Larry D Brown,Passakorn Pananont K D.Nelson,Simon Klemperer,Seth Haines,Zhao Wenjin,GuoJingru.Deep reflection surveying in central Tibet:lower-crustal layering and crustal flow[J].Geophysical Journal In-ternational,2004,156(1):115~128.
[14]Oliver J,Ewing M.Higher mode surface waves and theirbearing on the structure of the Earth's mantle[J].Bull SeismSoc Am,1957,47:187~204.
[15]Gutenberg B.Channel waves in the Earth's crust[J].Geo-physics,1955,20:283~294.
[16]Mitchell B J,Pan Y,Xie J,Cong L.Lg coda Q variationacross Eurasia and its relation to crustal evolution[J].J Geo-phys Res,1997,102:22767~22780.
[17]丁志锋,曾融生,等.青藏高原的Pn波速度和Moho面的起伏[J].地震学报,1992,14(增刊):592~599.
[18]裴顺平.中国大陆上地幔顶部体波速度层析成像[D].北京:中国地震局地球物理研究所,2002.
[19]汪素云,等.中国大陆上地幔顶部Pn速度结构[J].中国科学(D辑),2001,31(6):449~454.
[20]汪素云,许忠淮,等.中国大陆Pn速度结构与强震孕育的深部背景[J].地球物理学报,2003,46(6):779~785.
[21]许忠淮,汪素云.青藏高原东北缘地区Pn波速度的横向变化.地震学报,2003,25(1):24~31.
[22]McNamara D E,Owens T J,Walter W R.Propagationcharacteristics of Lg across the Tibetan Plateau[J].Bull SeisSoc Am,1996,86:457~469.
[23]Rapine R R,Ni J F,Hearn T M.Regional wave propagationin China and its surrounding regions[J].Bull Seis Soc Am,1997,87:1622~1636.
[24]Zhao Cuiping,Kennettl B L N,Furumura T.Contrasts inregional seismic wave propagation to station WMQ in centralAsia[J].Geophys J Int,2003,155:44~56.
[25]Hearn T M.Anisotropic Pn tomography in the western Unit-ed States[J].J Geophys Res,1996,101(B4):8403~8414.
[26]Haines S S,et al.INDEPTH-Ⅲseismic data:from surfaceobservations to deep crustal processes in Tibet[J].Tectonics,2003,22(1):1~18.
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