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Source time function of seismic events at Polish coal mines derived by empirical Green's function approach

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The empirical Gren's function deconvolution techniques in the frequency and time domains were applied to retrieve the source time functions from the records of P waves of 25 seismic events that occurred in 1994 and 1995 at Wujek coal mine and of 5 events that occurred in 1994 at Ziemowit coal mine. The selected events were located within the underground seismic networks composed at Wujek mine 14 vertical sensors, situated at a depth between 300 and 740 m and within the mining area of about 8 km2. the network at Ziemowit mine was composed of 16 vertical seismometers located at a depth between 430 and 620 m in the southern part of the mine. Moment magnitude of selected events ranged from 1.1 to 2.2. the records of several smaller events from the same area and with the similar source mechanism, with moment magnitude ranging from 0.3 to 1.7 , were accepted as empirical Green's functions. Both applied methods, the spectral division and the projected Landweber deconvolution, provided consistent and stable results. The relative source time functions of 6 events at Wujek mine and of 3 events at Ziemowit mine indicate that the rupture source propagated unilaterally, either along or perpendicularly to the longwall extension where the events were originated. The rupture velocity ranged from 0.4 to 0.8 of the S-wave velocity, which is distinctly lower than its typical value reported from natural earthquakes.
Rocznik
Strony
1--22
Opis fizyczny
Bibliogr. 21 poz.
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa
Bibliografia
  • 1. Ben-Menahem, A., 1962, Radiation of seismic body waves from a finite moving source in the Earth, J. Geophys. Res. 67, 345-350.
  • 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. 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.
  • 5. Dębski, W., and B. Domański, 2002, An application of the pseudo-spectral technique to retrieving source time function, Acta Geophys. Pol. 50, 207-221.
  • 6. Domański, B., and S. J. Gibowicz, 1999, Determination of source time function of mining-induced seismic events by the empirical Green's function approach, Publs. Inst. GeoI. phys., Polish Acad. Sci. M-22 (310), 5-14.
  • 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 Geophys. 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, 2002, Source time function of seismic events Rudna copper mine, Poland, Pure Appl. Geophys. 159, 131-144.
  • 10. Gibowicz, S.J., and B. Domański, 2001, New results of source time function studies by empirical Green 's function approach for seismic events at Rudna copper mine, Publs. Geophys. Pol. Acad. Sci. M-27 (352), 63-78 (in Polish).
  • 11. Gibowicz, S.J., and A. Kijko, 1994, An Introduction to Mining Seismology, Academic San Diego.
  • 12. Gibowicz, S.J., B. Domański and P. Wiejacz, 1997, Seismic moment and source size of seismic events in mines, KBN Report No 9 S601 008 06, 136 p., Warszawa (in Polish).
  • 13. Hanks, T.C., and H. Kanamori, 1979, A moment magnitude scale, J. Geophys. Res. 84, 2348-2350.
  • 14. Hartzell, S.H., 1978, Earthquake after shocks as Green's functions, Geophys. Res. Lett. 5, 1-5.
  • 15. 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.
  • 16. 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.
  • 17. 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, Geophys. J. Int. 137,651-662.
  • 18. Li, Y., and C.H. Thurber, 1988, Source properties of two microearthquakes at Kilauea Volcano, Hawaii, Bull. Seism. Soc. Am. 78, 1123-1132.
  • 19. Li, Y., C. Doli Jr and M.N. Toksöz, 1995, Source characterization and fault plane determinations for MbLg = 1.2 to 4.4 earthquakes in the Charlevoix seismic zone, Quebec, Canada, Bull. Seism. Soc. Am. 85, 1604-1621.
  • 20. Mueller, C.S., 1985, Source pulse enhancement by deconvolution of an empirical Green's function, Geophys. Res. Lett. 12, 33-36.
  • 21. 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-BSL7-0007-0024
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