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pure and applied geophysics

, Volume 82, Issue 1, pp 26–28 | Cite as

Geographical distribution of magnitude differences of 2° distant stations

  • U. Walzer
Article

Summary

The surface wave magnitudes determined at one seismic station are dependent of azimuthal receiving characteristics of this station.

Keywords

Geographical Distribution Surface Wave Seismic Station Distant Station Magnitude Difference 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. [1]
    A. Zátopek etJ. Vaněk,Les magnitudes de Praha et leur relation avec les ‘revised values’ de Pasadena, Publ. Bureau Centr. Séism. Int., Trav. sc.,A18 (1952), 137–152.Google Scholar
  2. [2]
    N. Panner,Die Ableitung der Magnitudengleichung für Oberflächenwellen für die seismische Station Collmberg, Stud. geophys. et geod.3 (1959), 242–254.Google Scholar
  3. [3]
    U. Walzer,Untersuchung der Azimutabhängigkeit von Erdbebenmagnituden, Freiberger Forschungsh.C194 (1966), 33–91.Google Scholar
  4. [4]
    J. Vaněk undJ. Stelzner,Einheitliche Bestimmung von Erdbebenmagnituden für mitteleuropäische Stationen, Trav. Inst. Geoph. Acad. Tchécosl. Sc., No. 136 (1960).Google Scholar

Copyright information

© Birkhäuser Verlag 1970

Authors and Affiliations

  • U. Walzer
    • 1
  1. 1.Zentralinstitut Physik der ErdeDeutsche Akademie der Wissenschaften zu BerlinJena

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