SUN KEZHONGup, FENG RUIup2, YAO ZHENGSHENGup3, ZHOU HAINANup2loans.com sh advancelucashadv. 1989: LITHOSPHERIC STRUCTURE IN THE TIBET-JAPAN PROFILE. Acta Seismologica Sinica, 11(2): 161-169.
Citation: SUN KEZHONGup, FENG RUIup2, YAO ZHENGSHENGup3, ZHOU HAINANup2loans.com sh advancelucashadv. 1989: LITHOSPHERIC STRUCTURE IN THE TIBET-JAPAN PROFILE. Acta Seismologica Sinica, 11(2): 161-169.

LITHOSPHERIC STRUCTURE IN THE TIBET-JAPAN PROFILE

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  • Published Date: September 01, 2011
  • The authors have utilized the data of surface wave recorded by long period digital seismometers to study the lithospheric structure in the Tibet-Japan profile. In data processing certain computational approaches to pure-path effect of surface waves and the continuous velocity model are taken into account for obtaining velocity distributions in the lithosphere of the Asian continental margin, North China and the Tibetan plateau. The velocity structures of the upper mantle in the first two regions are somewhat similar in the characteristics of thin lithosphere and alternating distribution of high-and low-velocity layers, which show some features of active tectonics. The upper mantle structure in the Tibetan plateau is like that in a stable platform and the corresponding crustal stucture shows active tectonic feature. The differences in the stuctures among the above three tectonic units are likely to extend from the crust down to 200 km deep in the upper mantle, this indicates the different movements of the Indian and Pacific ocean plates. It is inferred that the dynamic process of seismicity in North China and Japan is of the crust-mantle type, however in the Tibetan plateau is of intra-crust type.
  • [1] 吴佳翼、郁曙君、何淑韵,1979.华北地震同日本地震的相关性.地球物理学报,22, 415——438.

    [2] 阎志德、郭履灿,1979.我国华北地区与西南地区地震的相关性.地震研究,3, 56——58.

    [3] Knopoff, L., 1983. The thickness of the lithosphere from the dispersion of surface waves, Geophys. J. R. astr., 74,55——81.

    [4] 滕吉文、魏斯禹、李金森、赵静娴,1982.华北平原邢台地震活动地区的上地慢结构和地慢低速层.地球物理学报,25, 58——64,

    [5] 邵学钟、张家茹、章斯亚、李振江,1982.京津唐地区地壳上地慢立体构造.地震地质,4,1,1——10,

    [6] 冯锐、郑书真,1987.对华北岩石圈构造的综合研究.科学通报,32,22,1713—— 1727,

    [7] 宋仲和、安昌强、陈立华、仇志荣,1986.中国大陆和边缘海的上地幔P波速度结构.地震学报,8, 263——274.

    [8] 宋仲和、安昌强、王椿铺、仇志荣、张丽娟,1935.青藏高原及南北带上地幔P波速度结构.地球物理学报,28,增刊1,148——161,

    [9] 赵珠,1983.华北地区上地慢速度结构.地球物理学报,26, 3 11——354,

    [10] 冯锐、周海南、姚政生、孙克忠,1987,面波的频散、反演和层析成象.中国地震,3,1,15——28.

    [11] 冯锐、朱介寿、丁楹玉,陈国英、何正勤、杨讨彬、周海南、孙克忠,1981刊用地震面波研究中国地壳结构.地震学报,3,335——350,

    [12] 冯锐,1985.中国地壳厚度及上地慢密度分布(三维重力反演结果).地震学报,7,143——157,

    [13] 孙克忠、滕吉文,1935.由长周期地震面波研究西藏高原地区的地壳和上地慢的速度分布.地球物理学报,28,增刊1,43——53,

    [14] Johert, N.,B., G., Journet, A., Jobert, Hirn,and K.Z. Sun, 1985. Deep structure of southern Tibet inferred from the dispersion of Rayleigh waves through a long——period seismic network. Nature, 313, 6001, 386——338,

    [15] Knopoff, L.,1972. Observation and inversion of surface——wave dispersion. Tectonophysics, 13,1——4,497——519.

    [16] Kovach, R.L., 1978. Seismic surface waves and crustal and upper mantle structure. Rev, Geophys. Space phyr., 16,1.

    [17] Kaminuma, K.and K., Aki, 1963. Crustal structure in Japan from the phase velocity of Rayleigh waves, Part2. Rayleigh waves from Aleution Shock of March 9,1957. Bull. T'arthq. Res. Inst,41, 217——241,

    [18] Wier, S., 1982. Surface wave dispersion and Earth structure in southeastern China. Geophys. J, R. astr. Soc. 69,33——47.

    [19] Pines, Land T.L., Teng, 1980. A surface wave dispersion study of the crustal and upper mantle structure of China. J. Ccophys. Res., 85,B7,3829——3844,

    [20] Bruise, J. and J. Dorman, 1963. Seismic waves and earth structure in the Canadian shield. Bull. Seism. Soc.Amer., 53, 167,

    [21] 秦建业,T. V. McEvilly, 1985.西藏岩石圈结构的地震学新证据.地球物理学报,28,增刊1,135——147,

    [22] 陈国英、曾融生,1985.用地震面波频散研究喜马拉雅山与西藏高原岩石圈构造的差异.地球物理学报,28,增刊1,161——173,

    [23] 汪集汤、汪辑安,1986.辽河裂谷盆地地慢热流.地球物理学报,29, 450——459,

    [24] 冯锐、王均、郑书真、黄桂芳,严惠芬、周海南、张若水,1987.论华北地区的均衡状态(一).地震学报,9,406——416,

    [25] 姚虹、冯锐,1988.中国东西剖面的地壳Q结构研究.地震研究,11,6,539 ——550.

    [26] 环文林、汪素云、时振粱、鄢家全,1980,青藏高原震源分布与板块运动.地球物理学报,23,269——280.

    [27] Dziewonski, A.M. and D. L., Anderson, 1984, Seismic tomography of the Earth's interior. American Scientirts, 72, 483——494.

    [1] 吴佳翼、郁曙君、何淑韵,1979.华北地震同日本地震的相关性.地球物理学报,22, 415——438.

    [2] 阎志德、郭履灿,1979.我国华北地区与西南地区地震的相关性.地震研究,3, 56——58.

    [3] Knopoff, L., 1983. The thickness of the lithosphere from the dispersion of surface waves, Geophys. J. R. astr., 74,55——81.

    [4] 滕吉文、魏斯禹、李金森、赵静娴,1982.华北平原邢台地震活动地区的上地慢结构和地慢低速层.地球物理学报,25, 58——64,

    [5] 邵学钟、张家茹、章斯亚、李振江,1982.京津唐地区地壳上地慢立体构造.地震地质,4,1,1——10,

    [6] 冯锐、郑书真,1987.对华北岩石圈构造的综合研究.科学通报,32,22,1713—— 1727,

    [7] 宋仲和、安昌强、陈立华、仇志荣,1986.中国大陆和边缘海的上地幔P波速度结构.地震学报,8, 263——274.

    [8] 宋仲和、安昌强、王椿铺、仇志荣、张丽娟,1935.青藏高原及南北带上地幔P波速度结构.地球物理学报,28,增刊1,148——161,

    [9] 赵珠,1983.华北地区上地慢速度结构.地球物理学报,26, 3 11——354,

    [10] 冯锐、周海南、姚政生、孙克忠,1987,面波的频散、反演和层析成象.中国地震,3,1,15——28.

    [11] 冯锐、朱介寿、丁楹玉,陈国英、何正勤、杨讨彬、周海南、孙克忠,1981刊用地震面波研究中国地壳结构.地震学报,3,335——350,

    [12] 冯锐,1985.中国地壳厚度及上地慢密度分布(三维重力反演结果).地震学报,7,143——157,

    [13] 孙克忠、滕吉文,1935.由长周期地震面波研究西藏高原地区的地壳和上地慢的速度分布.地球物理学报,28,增刊1,43——53,

    [14] Johert, N.,B., G., Journet, A., Jobert, Hirn,and K.Z. Sun, 1985. Deep structure of southern Tibet inferred from the dispersion of Rayleigh waves through a long——period seismic network. Nature, 313, 6001, 386——338,

    [15] Knopoff, L.,1972. Observation and inversion of surface——wave dispersion. Tectonophysics, 13,1——4,497——519.

    [16] Kovach, R.L., 1978. Seismic surface waves and crustal and upper mantle structure. Rev, Geophys. Space phyr., 16,1.

    [17] Kaminuma, K.and K., Aki, 1963. Crustal structure in Japan from the phase velocity of Rayleigh waves, Part2. Rayleigh waves from Aleution Shock of March 9,1957. Bull. T'arthq. Res. Inst,41, 217——241,

    [18] Wier, S., 1982. Surface wave dispersion and Earth structure in southeastern China. Geophys. J, R. astr. Soc. 69,33——47.

    [19] Pines, Land T.L., Teng, 1980. A surface wave dispersion study of the crustal and upper mantle structure of China. J. Ccophys. Res., 85,B7,3829——3844,

    [20] Bruise, J. and J. Dorman, 1963. Seismic waves and earth structure in the Canadian shield. Bull. Seism. Soc.Amer., 53, 167,

    [21] 秦建业,T. V. McEvilly, 1985.西藏岩石圈结构的地震学新证据.地球物理学报,28,增刊1,135——147,

    [22] 陈国英、曾融生,1985.用地震面波频散研究喜马拉雅山与西藏高原岩石圈构造的差异.地球物理学报,28,增刊1,161——173,

    [23] 汪集汤、汪辑安,1986.辽河裂谷盆地地慢热流.地球物理学报,29, 450——459,

    [24] 冯锐、王均、郑书真、黄桂芳,严惠芬、周海南、张若水,1987.论华北地区的均衡状态(一).地震学报,9,406——416,

    [25] 姚虹、冯锐,1988.中国东西剖面的地壳Q结构研究.地震研究,11,6,539 ——550.

    [26] 环文林、汪素云、时振粱、鄢家全,1980,青藏高原震源分布与板块运动.地球物理学报,23,269——280.

    [27] Dziewonski, A.M. and D. L., Anderson, 1984, Seismic tomography of the Earth's interior. American Scientirts, 72, 483——494.
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