利用宜昌台重力观测资料检测地球自由振荡
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
用宜昌台DZW微伽重力仪的数字化观测资料,利用功率谱密度估计方法,在没有对资料进行去重力潮汐和气压改正的情况下,准确获得了2004年12月26日发生的苏门答腊大地震激发的0S3~0S37基频球型自由振荡,并与PREM模型的理论自由振荡周期进行了对比,发现实测振荡周期与PREM预测的振荡周期相吻合,除0S3、0S4、0S50、S60、S10振型的观测周期和PREM模型理论周期的相对误差大于0.2%外,其他振型的观测周期和PREM模型理论周期的相对误差大都集中在0.1%左右。
By use of the digitiled observations of the DZW microgal gravimeter at Yichang station without the corections of gravity tide and prossure the spherical free oscillations of the baseband 0S3-0S37 excited by the 26 Dec.2004 Sumatra earthquake are exactly obtained with the method of power spectrum density estimation.After comparing it with the periods of the theoretical free oscillation calculated with the PREM model it is found out that the observed period coincides with the theoretical.Except for the 0S3,0S4,0S5,0S6 and 0S10 that their relative error between the observed period and the theoretical ones is more than 0.2%,for the most of the others the relative error is about 1%.
引文
1傅承义,陈运泰,祁贵仲.地球物理学基础[M].北京:科学出版社,1985.
    2 Garland G D.Introduction to Geophysics(Mantle,Core andCrust).2nd ed[M].Toronto:W B Saunders Company,2003.
    3 Benioff H,Press F and Smith S.Excitation of the free oscilla-tions of the earth by earthquakes[J].Geophys.Res,1961,66(2):605-619.
    4 Ness N R,Harrison C Tand Sliehter L B.Observation of thefree oscillation of the earth[J].Geophys Res,1961,66:621-629.
    5 Alsop L E,Sutton G H and Ewing M.Free oscillation ofEarth observed on strain and pendulum seismographs[J].Geophy.Res,1961,66(2):631-641.
    6 Bogert B P.An observation of free oscillations of the Earth[J].Geophys.Res,1961,66(2):643-646.
    7 Dziewonski AMand Gillbert F.Observation of normal modesfrom 84 recordings of the Alaskan earthquakes 0f 1964March 28[J].Geophys.J.R.Astr.Soc,1972,27:393-446.
    8 Bolt B A and Currie R G.Maximum entropy estimates ofEarth torsional eigenperiods from 1960 trieste data[J].Geo-phys.J.R.Astr.Soc,1975,40:107-114.
    9 Zadro M and Braitenberg C.Measurements and interpreta-tions of tiltstrain gauges in seismically active areas[J].EarthScience Reviews,1999,47:151-187.
    10吕永清,蔡亚先,周云耀.用JCZ-1超宽频带数字地震仪观测地球自由振荡[J].地壳形变与地震,1997,(3):103-105.
    11唐磊,邱泽华,阚宝祥.中国钻孔体应变台网观测到的地球自由振荡[J].大地测量与地球动力学,2007,(6):37-44.
    12任佳,等.数字化水位仪观测的苏门答腊大地震激发的地球球型自由振荡[J].地震研究,2009,32(4):333-338.
    13 Stein S and Okal E A.Speed and size of the Sumatra earth-quake[J].Nature,2005a,434:581-582.
    14邓娜,等.利用双阳台水管观测资料检测地球自由振荡[J].大地测量与地球动力学,2009,(增刊):41-44,58.
    15 Stein S and Okal E A.The 2004 Sumatra earthquake andIndia ocean tsunami:What happened and why[J].TheEarth’s Scientist,2005b,(2):6-11.
    16万永革,盛书中,周公威.中国数字地震台网记录的苏门答腊—安达曼地震激发的地球球型自由振荡的检测[J].地震学报,2007,29(4):369-381.
    17雷湘鄂,等.苏门达腊地震激发的地球自由振荡及其谱线分裂的检测与讨论[J].中国科学(D辑),2007,37(4):504-511.
    18邱泽华,等.钻孔差应变仪观测的苏门答腊大地震激发的地球环型自由振荡[J].地球物理学报,2007,50(3):797-805.
    19万永革.数字信号处理的MATLAB实现[M].北京:科学出版社,2007.
    20 Park J,et al.Earth’s free oscillations excited by the 26December2004 Sumatra Andaman earthquake[J].Science,2005,308:1 139-1 146.
    21 Beroza G C and Jordan T H.Searching for slow and silentearthquakes using free oscillations[J].Geophys Res.,1990,95(B3):2 485-2 510.

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