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Determination of the homogeneous magnitude system magnitudes in seismological practice

Vaněk, J. (author)
Geophysical Institute, Czechoslovak Academy of Sciences
Kondorskaya, N.V. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
Fedorova, I.V. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
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Christoskov, L. (author)
Geophysical Institute, Bulgarian Academy of Sciences
Zakharova, A.I. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
Dineva, Savka (author)
Nosova, O.V. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
Kireev, I.A. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
Chepkunas, L.S. (author)
Institute of Physics of the Earth, Academy of Sciences, the U.S.S.R
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Geophysical Institute, Czechoslovak Academy of Sciences Institute of Physics of the Earth, Academy of Sciences, the US.S.R (creator_code:org_t)
Elsevier BV, 1985
1985
English.
In: Tectonophysics. - : Elsevier BV. - 0040-1951 .- 1879-3266. ; 118:3-4, s. 359-363
  • Journal article (peer-reviewed)
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  • Routine determination of network magnitudes by means of the Eurasian homogeneous magnitude system (HMS) is described and tested on a selection of recent shallow earthquakes. The HMS earthquake magnitudes appear to be more accurate and more reliable than the conventional earthquake magnitudes used in the present seismological practice. A preliminary investigation of correlations between magnitudes determined from different wave types shows a possible dependence of the correlation on the type of focal mechanism of earthquakes

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