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On reproducibility of relative locations of recurrent earthquakes recovered from similarity of their waveforms at a single station

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Języki publikacji
EN
Abstrakty
EN
Relative locations of recurrent earthquakes can be recovered from values of cross-correlation coefficients between their waveforms at a single station, provided that an idea of Menke (1999) that the values depend inversely exponentially from separation between the sources is true. An algorithm developed in Gnyp (2013) based on this idea was applied here for recovering relative locations of the two groups of the 2005-2006 recurrent earthquakes in Mukacheve, Ukraine, from the sets of crosscorrelation coefficients between their records at the four local network stations to find out whether the locations were in principle reproducible independently at each of the stations, at epicentral distances from about 6 to 64 km. The resulting sets of locations occurred in good agreement with each other, which may be considered as an experimental evidence for validity of the Menke’s dependence over the corresponding range of distances. The reproducibility of relative locations has been analyzed in terms of existence and uniqueness of the inverse problem’s solution, and in connection with data completeness and the influence of noise on it.
Czasopismo
Rocznik
Strony
1246--1261
Opis fizyczny
Bibliogr. 13 poz.
Twórcy
autor
  • Carpathian Branch of Subbotin Institute of Geophysics, National Academy of Sciences of Ukraine, Lviv, Ukraine
Bibliografia
  • [1] Aki, K., and P.G. Richards (1980), Quantitative Seismology: Theory and Methods, Vols. 1 and 2, Freeman and Co., San Francisco, 932 pp.
  • [2] Baisch, S., L. Ceranna, and H.-P. Harjes (2008), Earthquake cluster: What can we learn from waveform similarity? Bull. Seismol. Soc. Am. 98,6, 2806–2814, DOI: 10.1785/0120080018. http://dx.doi.org/10.1785/0120080018
  • [3] Davis, J.C. (1986), Statistics and Data Analysis in Geology, 2nd ed., John Wiley & Sons, New York, 383 pp.
  • [4] Gnyp, A. (2010), Refining locations of the 2005–2006 recurrent earthquakes in Mukacheve, West Ukraine, and implications for their source mechanism and the local tectonics, Acta Geophys. 58,4, 587–603, DOI: 10.2478/s11600-010-0006-9. http://dx.doi.org/10.2478/s11600-010-0006-9
  • [5] Gnyp, A. (2013), Recovering relative locations of the 2005–2006 Mukacheve earthquakes from similarity of their waveforms at a single station, Acta Geophys. 61,5, 1074–1087, DOI: 10.2478/s11600-012-0096-7. http://dx.doi.org/10.2478/s11600-012-0096-7
  • [6] Khomenko, V.I. (1971), Deep Structure of the Transcarpathian Depression, Naukova Dumka, Kyiv, 230 pp. (in Ukrainian).
  • [7] Khomenko, V.I. (1987), Deep Structure of the South-West Edge of the East-European Platform, Naukova Dumka, Kyiv, 140 pp. (in Russian).
  • [8] Kummerow, J. (2010), Using the value of the cross-correlation coefficient to locate microseismic events, Geophysics 75,4, MA47–MA52, DOI: 10.1190/1.3463713. http://dx.doi.org/10.1190/1.3463713
  • [9] Menke, W. (1999), Using waveform similarity to constrain earthquake locations, Bull. Seismol. Soc. Am. 89,4, 1143–1146.
  • [10] Pustovitenko, B.G. (ed.) (2007), Seismological bulletin of Ukraine 2005, Institute of Geophysics, National Academy of Sciences of Ukraine, Simferopol (in Russian).
  • [11] Pustovitenko, B.G. (ed.) (2008), Seismological bulletin of Ukraine 2006, Institute of Geophysics, National Academy of Sciences of Ukraine, Simferopol (in Russian).
  • [12] Shearer, P.M. (1997), Improving local earthquake locations using the L1 norm and waveform cross correlation: Application to the Whittier Narrows, California, aftershock sequence, J. Geophys. Res. 102,B4, 8269–8283, DOI: 10.1029/96JB03228. http://dx.doi.org/10.1029/96JB03228
  • [13] Shearer, P., E. Hauksson, and G. Lin (2005), Southern California hypocenter relocation with waveform cross-correlation. Part 2: Results using source-specific station terms and cluster analysis, Bull. Seismol. Soc. Am. 95,3, 904–915, DOI: 10.1785/0120040168. http://dx.doi.org/10.1785/0120040168
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-9f1848a6-1de0-4824-883c-c1448b556aa0
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