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The accuracy of source parameters estimated from the source time function of seismic events at Rudna copper mine in Poland

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The source time function of43 seismic events from Rudna copper mine was retrieved using empirical Greem's function deconvolution technique in the frequency and time domains. Thirty four events were studied preciously and nine new events were added, with moment magnitude raging from 2.1 to 3.6. the records of smaller events from the same area, with moment magnitude ranging from 1.5 to 2.7, were accepted as Grees's functions. Bith methods, the spectral division and the projected Landweber deconvolution, provided consistent results, but from an error analysis it follows that the classec spectral division solutions seem to be more reliable than the Lndweber solution. The relative source time functions retrieved from the records of a number of seismic stations (from 10 to 42) by the spectral division for 32 events and by the Landweber deconvolution for 36 events display directivity effects, implying unilaterally propagating ruptures. The rupture propagation direction and rupture velocity were estimated from the distribution of pulse widths and pulse maximum amplitudes as a function of station azimuths. The rupture velocity ranges from 0.25 to 0.9 of the shear wave velocity. Its values can be divided into two distinct sets: low velocity values in comparison with those from natural earthquakes, between 0.25 and 0.6 of shear wave velocity, and high velocity values greater than 0.6 of the shear wave velocity. The rupture velocity depends also to some extent on the rupture direction.
Rocznik
Strony
347--367
Opis fizyczny
Bibliogr. 24 poz.
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa Poland
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa Poland
Bibliografia
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  • 2. Bertero, M., D. Bindi, P. Boccacci, M. Cattaneo, C. Eva and V. Lanza, 1997, Application of the projected Landweber method to the estimation of the source time function in seismology, Inverse Problems 13, 465-486.
  • 3. Boatwright, J., 1980, A spectral theory for circular seismic sources: Simple estimates of source dimension, dynamic stress drop, and radiated energy, Bull. Seism. Soc. Am. 70, 1-28.
  • 4. Bour, M., and M. Cara, 1997, Test of a simple Green's function method on moderate-sized earthquakes, Bull. Seism. Soc. Am. 87, 668-683.
  • 5. Courboulex, F., N. Deichmann and J.-C. Gariel, 1999, Rupture complexity of a moderate intra-plate earthquake in the Alps: the 1996 M5 Epagny-Annecy earthquake, Geophys. J. Int. 139, 152-160.
  • 6. Dębski, W., and B. Domański, 2002, An application of the pseudo-spectral technique to retrieving source time function, Acta Geophys. Pol. 50, 207-221.
  • 7. Domański, B., and S.J. Gibowicz, 2001, Comparison of source time functions retrieved in the frequency and time domains for seismic events in a copper mine in Poland, Acta Geo¬phys. Pol. 49, 169-188.
  • 8. Domański, B., S.J. Gibowicz and P. Wiejacz, 2001, Source time functions of seismic events induced at a copper mine in Poland: Empirical Green's function approach in the frequency and time domains. In: G. van Aswegen, R.J. Durrheim and W.D. Ortlepp (eds.), "Dynamic Rock Mass Response to Mining", pp. 99-108, South African Institute of Mining and Metallurgy, Johannesburg.
  • 9. Domański, B., S.J. Gibowicz and P. Wiejacz, 2002a, Source time function of seismic events at Rudna copper mine, Poland, Pure Appl. Geophys. 159, 131-144.
  • 10. Domański, B., S.J. Gibowicz and P. Wiejacz, 2002b, Source parameters of seismic events in a copper mine in Poland based on empirical Green 's functions. In: H. Ogasawara, T. Yanagidani and M. Ando (eds.), "Seismogenic Process Monitoring", pp. 75-89, Balkema, Rotterdam.
  • 11. Domański, B., S.J. Gibowicz and P. Wiejacz, 2002c, Source time functions of seismic events induced at a copper mine in Poland: Empirical Green's function approach in the frequency and time domains, Publs. Inst. Geophys. Pol. Acad. Sc. M-24 (340), 5-27 (in Polish with English abstract and figure captions).
  • 12. Gibowicz, S.J., and B. Domański, 2002, New results of source time function studies by empirical Green's function approach for seismic events at Rudna copper mine, Publs. Inst. Geophys. Pol. Acad. Sc. M-27 (352), 63-78 (in Polish with English abstract and figure captions).
  • 13. Gibowicz, S.J., and A. Kijko, 1994, An Introduction to Mining Seismology, Academic Press, San Diego.
  • 14. Hanks, T.C., and H. Kanamori, 1979, A moment magnitude scale, J. Geophys. Res. 84, 2348-2350.
  • 15. Hartzell, S.H., 1978, Earthquake after-shocks as Green's functions, Geophys. Res. Lett. 5, 1-5.
  • 16. Hough, S.E., 1997, Empirical Green's function analysis: Taking the next step, J. Geophys. Res. 102, 5369-5384.
  • 17. Hough, S.E., J.M. Lees and F. Monastero, 1999, Attenuation and source properties at the Coso geothermal area, California, Bull. Seism. Soc. Am. 89, 1606-1619.
  • 18. Jost, M.L., T. Busselberg, O. Jost and H.-P. Harjes, 1998, Source parameters of injection-induced microearthquakes at the KTB deep drilling site, Germany, Bull. Seism. Soc. Am. 88, 815-832.
  • 19. Lanza, V., D. Spallarossa, M. Cattaneo, D. Bindi and P. Augliera, 1999, Source parameters of small events using constrained deconvolution with empirical Green's functions, Geo¬phys. J. Int. 137, 651-662.
  • 20. Li, Y., C. Doll Jr. and M.N. Toksoz, 1995, Source characterization and fault plane determinations for MmLg = 1.2 to 4.4 earthquakes in the Charlevoix seismic zone, Quebec, Canada, Bull. Seism. Soc. Am. 85, 1604-1621.
  • 21. Mueller, C.S., 1985, Source pulse enhancement by deconvolution of an empirical Green's function, Geophys. Res. Lett. 12, 33-36.
  • 22. Shi, J., W.-Y. Kim and P.G. Richards, 1998, The comer frequencies and stress drops of intra-plate earthquakes in the northeastern United States, Bull. Seism. Soc. Am. 88, 531-542.
  • 23. Urbancic, T.I., C.-I. Trifu and P.R. Young, 1993, Stress release estimates, scaling behaviour, and source complexities of microseismic events. In: R.P. Young (ed.), "Rockbursts and Seismicity in Mines", pp. 255-260, Balkema, Rotterdam.
  • 24. Wiejacz, P., 1992, Calculation of seismic moment tensor for mine tremors from the Legnica-Głogów Copper Basin, Acta Geophys. Pol. 40, 103-122.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0007-0052
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