Abstract Earthquake, explosion, and a nuclear test data are compared with forward modeling and band-pass filtered surface wave amplitude data for exploring methodologies to improve earthquake–explosion discrimination. The proposed discrimination method is based on the solutions of a double integral transformation in the wavenumber and frequency domains. Recorded explosion data on June 26, 2001 (39.212°N, 125.383°E) and October 30, 2001 (38.748°N, 125.267°E), a nuclear test on October 9, 2006 (41.275°N, 129.095°E), and two earthquakes on April 14, 2002 (39.207°N, 125.686°E) and June 7, 2002 (38.703°N, 125.638°E), all in North Korea, are used to discriminate between explosions and earthquakes by seismic wave analysis and numerical modeling. The explosion signal is characterized by first P waves with higher energy than that of S waves. Rg waves are clearly dominant at 0.05–0.5 Hz in the explosion data but not in the earthquake data. This feature is attributed to the dominant P waves in the explosion and their coupling with the SH components.
Cho ,Kwang-Hyun . Discriminating between explosions and earthquakes[J]. APPLIED GEOPHYSICS, 2014, 11(4): 429-436.
[1]
Bonner, J., Russell, L., Harkrider, D., Reiter, D., and Herrmann, R., 2006, Development of a time-domain variable period surface wave magnitude measurement procedure for application at regional and teleseismic f America, 96, 678-696.
[2]
Bonner, J., Stroujkova, A., and Anderson, D. N., 2011, Improving earthquake and explosion discrimination by using Love and Rayleigh wave magnitudes, in “2011 Monitoring Research Review: Ground-Based Nuclear Explosion Monitoring Technologies” sponsored by the Air Force Research Laboratory.
[3]
Cho, K. H., and Lee, K., 2006, Dispersion of Rayleigh waves in the Korean Peninsula: Journal of the Korean Geophysical Society, 9, 231-240.
[4]
Cho, K. H., Herrmann, R. B., Ammon, C. J., and Lee, K., 2007, Imaging the upper crust of the Korean Peninsula by surface wave tomography: Bulletin of the Seismological Society of America, 97, 198-207, doi: 10.1785/0120060096.
[5]
Cho, K. H., Lee, S.-H., and Kang, I. -B., 2011a, Crustal structure of the Korean Peninsula using surface wave dispersion and numerical modeling: Pure and Applied Geophysics, 168, 1587-1598, doi: 10.1007/s00024-011-0262-x.
[6]
Cho, K. -H., Chen, H. W., Kang, I. -B., and Lee, S. -H., 2011b, Crust and upper mantle structures of the region between Korea and Taiwan by surface wave dispersion study: Geoscience Journal, 15, 71-81, doi: 10.1007/s12303-011-0009-9.
[7]
Cho, Kwang Hyun, 2014, Discovery of a surface-wave velocity anomaly in the West Sea of South Korea:Exploration Geophysics, 45, 86-93.
[8]
Chun, K. -Y., Wu, Y., and Henderson, G. A., 2011, Magnitude estimation and source discrimination: A close look at the 2006 and 2009 North Korean underground nuclear explosions : Bulletin of the Seismological Society of America, 101, 1315-1329.
[9]
Hong, T. -K., Baag, C. -E., Choi, H., and Sheen, D. -H, 2008, Regional seismic observations of the 9 October 2006 underground nuclear explosion in North Korea and the influence of crustal structure on regional phases: Journal of Geophysical Research, 113, B03305, doi: 10.1029/2007JB004950.
[10]
Hong, T. -K. and Rhie, J., 2009, Regional source scaling of the 9 October 2006 underground nuclear explosion in North Korea: Bulletin of the Seismological Society of America, 99, 2523-2540.
[11]
Howard J. P., and Steven, R. T., 2008, Effects of shock-induced tensile failure on mb-Ms discrimination: Contrasts between historic nuclear explosions and the North Korean test of 9 October 2006, Geophysical Research Letters: 35, L14301, doi: 10.1029/2008GL034211.
[12]
Hudson, J. A., 1969, A quantitative evaluation of seismic signals at teleseismic distances II. Body waves and surface waves from an extended source: Geophys. J., 18, 353-370.
[13]
Kafka, A. L., 1990, Rg as a depth discriminant for earthquakes and explosions - a case study in New England: Bulletin of the Seismological Society of America, 80, 373-394.
[14]
Kremenetskaya, E., Asming, V., Jevtjugina, Z., and Ringdal, F., 2002, Study of regional surface waves and frequency-dependent Ms:mb discrimination in the European Arctic: Pure and Applied Geophysics, 159, 721-733.
[15]
Saikia, C. K., 1992, Numerical Study of Quarry Generated Rg as a Discriminant for Earthquakes and Explosions - Modeling of Rg in Southwestern New England: Journal of Geophysical Research, 97, 11,057-11,072.
[16]
Walter, W. R., Matzel, E., Pasyanos, M., Harris, D. B., Gok, R., Ford, S. R., 2007, Empirical observations of earthquake-explosion discrimination using P/S ratios and implications for the sources of explosion S-waves: “MRR2007-29th Research Review on Nuclear Explosion Monitoring Technologies” sponsored by the Air Force Research Laboratory.
[17]
Yoo, H. J., Herrmann, R. B., Cho, K. H., and Lee, K., 2007, Imaging the three-dimensional crust of the Korean Peninsula by joint inversion of surface-wave dispersion and teleseismic receiver functions: Bulletin of the Seismological Society of America, 97, 1002-1011, doi: 10.1785/0120060134.