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HandWiki. Seismic Array. Encyclopedia. Available online: https://encyclopedia.pub/entry/27943 (accessed on 07 November 2026).
HandWiki. Seismic Array. Encyclopedia. Available at: https://encyclopedia.pub/entry/27943. Accessed November 07, 2026.
HandWiki. "Seismic Array" Encyclopedia, https://encyclopedia.pub/entry/27943 (accessed November 07, 2026).
HandWiki. (2022, September 29). Seismic Array. In Encyclopedia. https://encyclopedia.pub/entry/27943
HandWiki. "Seismic Array." Encyclopedia. Web. 29 September, 2022.

Seismic Array

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The content is sourced from: https://handwiki.org/wiki/Earth:Seismic_array

A seismic array is a system of linked seismometers arranged in a regular geometric pattern (cross, circle, rectangular etc.) to increase sensitivity to earthquake and explosion detection. A seismic array differs from a local network of seismic stations mainly by the techniques used for data analysis. The data from a seismic array is obtained using special digital signal processing techniques such as beamforming, which suppress noises and thus enhance the signal-to-noise ratio (SNR). The earliest seismic arrays were built in the 1950s in order to improve the detection of nuclear tests worldwide. Many of these deployed arrays were classified until the 1990s. Today they become part of the IMS as primary or auxiliary stations. Seismic arrays are not only used to monitor earthquakes and nuclear tests, but also used as a tool for investigating nature and source regions of microseisms as well as locating and tracking volcanic tremor and analyzing complex seismic wave-field properties in volcanic areas.

digital signal volcanic tremor seismic array

References

  1. Bormann, P (2012). New Manual of Seismological Observatory Practice (NMSOP-2). IASPEI. p. Chapter 9. 
  2. Muirhead, K. J., and Ram Datt (1976). The N-th root process applied to seismic array data. Geophysical Journal International, 47(1), 197-210.
  3. Schimmel, M., and Paulssen, H. (1997). Noise reduction and detection of weak, coherent signals through phase-weighted stacks. Geophysical Journal International, 130(2), 497-505.
  4. Kennett, B. L. N. (2000). Stacking three-component seismograms. Geophysical Journal International, 141(1), 263-269.
  5. Krüger, F., Weber, M., Scherbaum, F., and Schlittenhardt, J. (1993). Double beam analysis of anomalies in the core-mantle boundary region. Geophysical Research Letters, 20(14), 1475-1478.
  6. Capon, J. (1969). High-resolution frequency-wavenumber spectrum analysis. Proceedings of the IEEE, 57(8), 1408-1418.
  7. Kværna, T., and Doornbos, D. J. (1986). An integrated approach to slowness analysis with arrays and three-component stations. NORSAR Semiannual Technucal Summary, 1, 2-85.
  8. "NORSAR". Norsar.no. http://www.norsar.no/norsar/. Retrieved 2015-11-17. 
  9. Del Pezzo, E., and Giudicepietro, F. (2002). Plane wave fitting method for a plane, small aperture, short period seismic array: a MATHCAD program. Computers and Geosciences, 28(1), 59-64.
  10. "The Yellowknife Seismological Array". Can-ndc.nrcan.gc.ca. 2015-10-20. http://can-ndc.nrcan.gc.ca/yka/index-en.php. Retrieved 2015-11-17. 
  11. Frosch, R. A., and Green, P. E., Jr. (1966). The concept of a large aperture seismic array. Proceedings of the Royal Society of London A: Mathematical, Physical and Engineering Sciences (Vol. 290, No. 1422, pp. 368-384). The Royal Society.
  12. "GERES - Deutsche IMS-Station: Seismische Primärstation GERES (PS19)" (in de). BGR. 2000-08-12. http://www.bgr.bund.de/DE/Themen/Erdbeben-Gefaehrdungsanalysen/Seismologie/Kernwaffenteststopp/Ueberwachungsnetz/Deutsche-IMS-Stationen/GERES/geres_inhalt.html. Retrieved 2015-11-17. 
  13. "AS072, Spitsbergen, Norway: CTBTO Preparatory Commission". Ctbto.org. 2007-04-27. https://www.ctbto.org/verification-regime/featured-stations/types/auxiliary-seismic/as072-spitsbergen-norway/. Retrieved 2015-11-17. 
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