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Seismic doublets and multiplets at Polish coal and copper mines

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Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The following criteria for selection of doublets at Polish coal mines were accepted: the difference in magnitude (based on seismic moment) of two events not larger than 0.15, the distance between their hypocenters not greater than 150 m, and the time interval between their occurrence not longer than 10 days. Similarly, the criteria for seismic events at copper mines are: the difference in magnitude not exceeding 0.15, the distance not greater than 200 m, and the time interval not longer than 20 days. Seismic events from the Wujek and Ziemowit coal mines that oc-curred between 1993 and 1995, and seismic events from the Polkowice copper mine that occurred between 1994 and 1996 and from the Rudna copper mine that occurred between 1994 and 2004 were considered. Their source parameters and focal mechanisms were known in most cases from previous studies. Altogether 108 seismic pairs from coal mines and 118 pairs from copper mines were found, forming doublets, triplets and quadruplets, within the magnitude range from 0.7 to 3.5. The distance and time intervals between two events forming pairs are not dependent on magnitude of these events. The focal mechanism of seismic events forming pairs is similar in over 60 percent of pairs at coal mines and in about one third of pairs at copper mines. Spa-tial distributions of doublets in particular sections of coal and copper mines display dominant linear trends, characteristic for a given area, which are often in conformity with the direction of nodal planes determined by fault plane solution of one or both the events forming a doublet. In such cases, the rupture plane can be discriminated among the nodal planes.
Czasopismo
Rocznik
Strony
142--157
Opis fizyczny
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences ul. Księcia Janusza 64, 01-452 Warszawa, Poland, gibowicz@igf.edu.pl
Bibliografia
  • Augliera, P., M. Cattaneo and C. Eva, 1995, Seismic multiplets analysis and its implication in seismotectonics, Tectonophysics 248, 219-234.
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  • Domański, B., S.J. Gibowicz, and P. Wiejacz, 2002, Source time function of seismic events at Rudna copper mine, Poland, Pure Appl. Geophys. 159, 131-144.
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  • Gibowicz, S.J., 2001, Radiated energy scaling for seismic events induced by mining, Acta Geophys. Pol. 49, 95-111.
  • Gibowicz, S.J., and A. Kijko, 1994, An Introduction to Mining Seismology, Academic Press, San Diego.
  • Gibowicz, S.J., and S. Lasocki, 2005, Earthquake doublets and multiplets in the Fiji-Tonga-Kermadec region, Acta Geophys. Pol. 53, 239-274.
  • Gibowicz, S.J., B. Domański, B. Nita and P. Wiejacz, 2003, Source time function of seismic events at Polish coal mines derived by empirical Green's function approach, Acta Geophys. Pol. 51, 1-22.
  • Gibowicz, S.J., B.M. Domański and P. Wiejacz, 2006, Seismic doublets and multiplets in the Polish copper mines, Publs. Inst. Geophys. Pol. Acad. Sci. (in press).
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  • Moriya, H., K. Nakazato, H. Niitsuma and R. Baria, 2002, Detailed fracture system of the Soultz-sous-Forets HDR field evaluated using microseismic multiplet analysis, Pure Appl. Geophys. 159, 517-541.
  • Poupinet, G., W.L. Ellsworth and J. Frechet, 1984, Monitoring velocity variations in the crust using earthquake doublets: An application to the Calaveras Fault, California, J. Geophys. Res. 89, 5719-5731.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0014-0039
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