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Information Journal Paper

Title

INTENSITY-MAGNITUDE RELATIONSHIP AND INTENSITY ATTENUATION LAW IN IRAN

Pages

  26-33

Abstract

 This paper is devoted to explore the relationship between EARTHQUAKE intensity in the epicenter and its MAGNITUDE as well as the INTENSITY ATTENUATION LAWS of the IRANian EARTHQUAKEs. For this purpose, available data, reports, seismotectonic and isoseismalmaps, related to 21 destructive EARTHQUAKEs in a period of 1957 to 1998, were studied.The results show that the intensity-magnitude relationships and the INTENSITY ATTENUATION LAWS are strongly dependent on the site geology that specifies local effects. Therefore, the sites have been classified, according to site geology, into two groups, hard sites and soft sites. The intensity-magnitude and intensity attenuation versus the distance from the EARTHQUAKE sources (surface refaulting of the causative fault (s)) were determined and introduced for each of the two site groups. Finally, the obtained laws were compared with some other laws offered by other researchers.

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    APA: Copy

    RAMAZI, H.R., & HORMOZINEZHAD, M.R.. (2005). INTENSITY-MAGNITUDE RELATIONSHIP AND INTENSITY ATTENUATION LAW IN IRAN. GEOSCIENCES, 15(57), 26-33. SID. https://sid.ir/paper/31649/en

    Vancouver: Copy

    RAMAZI H.R., HORMOZINEZHAD M.R.. INTENSITY-MAGNITUDE RELATIONSHIP AND INTENSITY ATTENUATION LAW IN IRAN. GEOSCIENCES[Internet]. 2005;15(57):26-33. Available from: https://sid.ir/paper/31649/en

    IEEE: Copy

    H.R. RAMAZI, and M.R. HORMOZINEZHAD, “INTENSITY-MAGNITUDE RELATIONSHIP AND INTENSITY ATTENUATION LAW IN IRAN,” GEOSCIENCES, vol. 15, no. 57, pp. 26–33, 2005, [Online]. Available: https://sid.ir/paper/31649/en

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