Ito A. Earthquake swarm activity revealed from high-resolution relative hypocenters-clustering of microearthquakes. Tectonophysics, 1990, 175(1-3): 47-66.
[2]
Smith E G C. Scaling the equations of condition to improve conditioning. Bull. Seism. Soc. Am., 1976, 66(6): 2075-2076.
[3]
Spence W. Relative epicenter determination using P-wave arrival-time differences. Bull. Seism. Soc. Am., 1980, 70(1): 171-183.
[4]
Anderson K R. Robust earthquake location using M-estimates. Phys. Earth Planet. Interiors, 1982, 30(2-3): 119-130.
[5]
Thurber C H. Nonlinear earthquake location: theory and examples. Bull. Seism. Soc. Am., 1985, 75(3): 779-790.
[6]
Anderson K R. Epicentral location using arrival time order. Bull. Seism. Soc. Am., 1981, 71(2): 541-546.
[7]
Chave A D, Thomson D J, Ander M E. On the robust estimation of power spectra, coherences, and transfer functions. J. Geophys. Res., 1987, 92(B1): 633-648.
[8]
Andrews D F. A robust method for multiple linear regression. Technometrics, 1974, 16(4): 523-531.
[9]
Lilwall R C, Francis T J G. Hypocentral resolution of small ocean bottom seismic networks. Geophys. J. R. Astron. Soc., 1978, 54(3): 721-728.
[10]
Evernden J F. Precision of epicenters obtained by small numbers of world-wide stations. Bull. Seism. Soc. Am., 1969, 59(3): 1365-1398.
[11]
Krüger F, Ohrnberger M. Tracking the rupture of the MW=9.3 Sumatra earthquake over 1150 km at teleseismic distance. Nature, 2005, 435(7044): 937-939.
[12]
Ishii M, Shearer P, Houston H, et al. Extend, duration and speed of the 2004 Sumatra-Andaman earthquake imaged by the Hi-Net array. Nature, 2005, 435(7044): 933-936.
[13]
Geiger L. Herdbestimmtung bei Erdbeben ans den Ankunftszeiten. K. Gesel. Wiss. Gott., 1910, 331-349. Geiger L. Probability method for the determination of earthquake epicenters from the arrival time only. Bull. St. Louis. Univ., 1912, 8(1): 60-71.
[14]
Bratt S R, Bache T C. Locating events with a sparse network of regional arrays. Bull. Seism. Soc. Am., 1988, 78(2): 780-798.
[15]
Flinn E A. Confidence regions and error determinations for seismic event location. Rev. Geophys., 1965, 3(1): 157-185.
[16]
Buland R. The mechanics of locating earthquakes. Bull. Seism. Soc. Am., 1976, 66(1): 173-187.
[17]
Jordan T H, Sverdrup K A. Teleseismic location techniques and their application to earthquake clusters in the South-Central Pacific. Bull. Seism. Soc. Am., 1981, 71(4): 1105-1130.
[18]
Rowlett H, Forsyth D W. Recent faulting and microearthquakes at the intersection of the Vema Fracture Zone and the Mid-Atlantic Ridge. J. Geophys. Res., 1984, 89(B7): 6079-6094.
[19]
Ito A. High resolution relative hypocenters of similar earthquakes by cross-spectral analysis method. J. Phys. Earth., 1985, 33(4): 279-294.
[20]
Pavlis G L. Appraising earthquake hypocenter location errors: a complete, practical approach for single-event location. Bull. Seism. Soc. Am., 1986, 76(6): 1699-1717.
[21]
Bolt B A. The revision of earthquake epicentres, focal depths and origin-times using a high-speed computer. Geophys. J. R. Astron. Soc., 1960, 3(4): 433-440.
[22]
Waldhauser F, Ellsworth W L. A Double-difference earthquake location algorithm: Method and application to the Northern Hayward fault, California. Bull. Seism. Soc. Am., 2000, 90(6): 1353-1368.
[23]
Geller R J, Mueller C S. Four similar earthquakes in central California. Geophys. Res. Lett., 1980, 7(10): 821-824.
[24]
Deichmann N, Garcia-Fernandez M. Rupture geometry from high-precision relative hypocentre locations of microearthquake clusters. Geophys. J. Int., 1992, 110(3): 501-517.
[25]
Poupinet G, Ellsworth W L, Fréchet J. Monitoring velocity variations in the crust using earthquake doublets: an application to the Calaveras fault, California. J. Geophys. Res., 1984, 89(B7): 5719-5731.
[26]
Scherbaum F, Wendler J. Cross spectral analysis of Swabian Jura (SW Germany) three-component microearthquake recordings. J. Geophys., 1986, 60(2): 157-166.
[27]
Spudich P, Bostwick T. Studies of the seismic coda using an earthquake cluster as a deeply buried seismograph array. J. Geophys. Res., 1987, 92(B10): 10526-10546.
[28]
Frémont M J, Malone S D. High precision relative locations of earthquakes at Mount St. Helens, Washington. J. Geophys. Res., 1987, 92(B10): 10223-10236.
[29]
Console R, Di Giovambattista R. Local earthquake relative location by digital records. Phys. Earth. Planet. Inter., 1987, 47: 43-49.
[30]
Pechmann J C, Thorbjarnardottir B S. Waveform analysis of preshock-mainshock-aftershock sequence in Utah. Bull. Seism. Soc. Am., 1990, 80(3): 519-550.
[31]
Aki K, Richards P G. Quantitative Seismology. San Francisco: W. H. Freeman and Company, 1980: 38-40.
[32]
Xu Y, Koper K D, Sufri O, Zhu L P. Rupture imaging of the Mw7.9 12 May 2008 Wenchuan earthquake from back projection of teleseismic P waves. Geochem. Geophys. Geosyst., 2009, 10(4): Q04006.
[33]
杜海林. 2004年苏门答腊—安达曼大地震能量辐射源的时间域台阵技术分析[硕士论文]. 北京: 中国地震局地球物理研究所, 2007. Du H L. Analysis of the energy radiation sources of the 2004 Sumatra-Andaman earthquake using time-domain array techniques (in Chinese)[Master''s thesis]. Beijing: Institute of Geophysics, China Earthquake Administration, 2007.
[34]
Rost S, Thomas C. Array seismology: methods and applications. Rev. Geophys., 2002, 40(3): 2-1-2-27.
[35]
Larmat C, Montagner J P, Fink M, et al. Time-reversal imaging of seismic sources and application to the great Sumatra earthquake. Geophys. Res. Lett., 2006, 33(19): L19312.
[36]
Kennett B L N. Seismic Wave Propagation in Stratified Media. Cambridge: Cambridge University Press, 1983:1-342.