期刊
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
卷 106, 期 2, 页码 799-805出版社
SEISMOLOGICAL SOC AMER
DOI: 10.1785/0120150179
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资金
- State of Utah
- National Institute for Occupational Health and Safety (NIOSH)
- NIOSH
Comparison of observed and synthetic radiation patterns suggests that Love waves generated by the 2007 Crandall Canyon Mine collapse (M-w 4.1) are the result of shear waves generated by a relatively large compensated linear vector dipole component at the source, whereas the Love waves associated with a 2013 Rudna Mine collapse (M-w 4.2) are minimal except where amplified by a deep sedimentary basin. We examine the source of the 19 March 2013 Rudna Mine, Poland, collapse with a full moment tensor inversion method, using the complete waveforms of regional-distance seismic data. The computed source is primarily composed of a dominant, and statistically significant, implosive component. The Rudna source is more similar to previous mine collapses than to double-couple tectonic earthquakes. Although source mechanisms are similar, there are clear differences in Love-wave amplitudes.
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