Abstract
This paper aims to describe a probabilistic frequency analysis procedure to develop seismic hazard maps of Kopet Dagh region in north and northeast of Iran which with mostly shallow earthquakes is a high active seismic area. The existence of Khangiran super gas reservoir increases the importance of this region. By application of the probabilistic methodology of Cornell, an extensive numerical analysis based on several deterministic and probabilistic indices, the frequency content of ground motions recorded during seismic events were carried out by EZFRISK computer code, Matlab programming environment, and generated graphical user interface C# computer code. In this paper, definition of a seismotectonic model of the whole region based on geologic, tectonics, and seismic information the potential seismic sources introduced and their seismic characteristics were determined. Among the different applied attenuation relationships, the proposed one by Ambraseys et al. (J Earthq Eng Struct Dyn 25(4):371–400, 1996) was considered and the results are expressed in a series of contour maps of expected PGA for 63 % probability. The elimination of fore and aftershocks and also put some abilities such as capability for result exporting in several format which can be defined by user for other mathematical generic curve fitting tools were carried out by a generated code in Matlab programming environment. Obtained hazard maps indicated that maximum accelerations will be occurred in northwest-central trend which has a well matching with Quchan-Robat and Esfarayen-Robat Gharabil faults. The relevant frequency analysis showed that form 0.1 to 10 Hz, PGA directly increased by frequency and then up to 20 Hz with a sharpen shape, decreased by frequency increasing. The trend continues by gradual reduction up to 100 Hz. Maximum acceleration will be occurred in the basement in frequency content of 10 Hz.
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References
Algermissen ST, Perkins DM (1976) A probabilistic estimate of maximum acceleration in rock in the contiguous United States. USGS open file report 76–416, p 45
Ambraseys N, Melville CP (1982) A history of Persian earthquakes. Cambridge University Press, p. 219
Ambraseys N, Simpson K (1996) Prediction of vertical response spectra in Europe. J Earthq Eng Struct Dyn 25(4):401–412
Ambraseys N, Simpson K, Bommer J (1996) Prediction of horizontal response spectra in Europe. J Earthq Eng Struct Dyn 25(4):371–400
Berberian M (1981) Active faulting and tectonics of Iran, in Zagros, Hindu Kush, Himalaya geodynamic evolution. In: Gupta HK, Delany FM (eds) Geodyn Ser Am Geophys Un 3:33–69
Berberian M (1994) Natural hazard and the first earthquake catalogue of Iran, historical hazards in Iran prior to 1900. Int Inst Earthq Eng Seismol 1:603p
Berberian M, Qorashi M, Arzhangravesh B, Mohajer-Ashjai A (1985) Recent tectonics, seismotectonics, and earthquake- fault hazard study of the greater Tehran Region. Geol Surv Iran 56, 316s, (in Farsi)
Bommer JJ, Abrahamson NA (2006) Why do modern probabilistic seismic-hazard analyses often lead to increased hazard estimates? Bull Seismol Soc Am 96(6):1967–1977
Bozorgnia Y, Bertero VV (2004) Earthquake engineering: from engineering seismology to performance-based engineering. CRC Press, Boca Raton
CMT (2006) Centroid Moment Tensor catalogue, Harvard University. Department of geological Sciences, available online at: http://www.seismology.harvard.edu/CMTsearch.html
Cornell CA (1968) Engineering seismic risk analysis. Bull Seismol Soc Am 58:1583–1606
Das S, Guptha ID, Guptha VK (2006) A probabilistic seismic hazard analysis of Northeast India. Earthq Spectr 22(1):1–27
Gao M (1988) Discussion on annual occurrence rates. Dev World Seismol 1:1–5 (in Chinese)
Gardner J, Knopoff K (1974) Is the sequence of earthquakes in Southern California, with aftershock remove Poissonian? Bull Seismol Soc Am 64:1363–1367
Gutenberg B, Richter CF (1944) Frequency of earthquakes in California. Bull Seismol Soc Am 34:185–188
Jackson JA, McKenzie DP (1984) Active tectonics of the Alpine-Himalayan Belt between Turkey and Pakistan. Geophys J R Astron Soc 77:185–26440
Kijko A, Sellevoll MA (1989) Estimation of earthquake hazard parameters from incomplete data files. Part I: utilization of extreme and complete catalogs with different threshold magnitudes. Bull Seismol Soc Am 79:645–654
Kijko A, Sellevoll MA (1992) Estimation of earthquake hazard parameters from incomplete data files. Part II. Incorporating magnitude heterogeneity. Bull Seismol Soc Am 82:120–134
Klügel J-U (2007a) Error inflation in probabilistic seismic hazard analysis. Eng Geol 90:186–192
Klügel J-U (2007b) Comment on “Why do modern probabilistic seismic hazard analyses often lead to increased hazard estimates?” by Julian J. Bommer and Norman A. Abrahamson. Bull Seismol Soc Am 97:2198–2207
Kossobokov VG (2006) Testing earthquake prediction methods: the West Pacific short-term forecast of earthquakes with magnitude MwHRV>=5.8. Tectonophysics 413:25–31
Lombardi AM, Akinci A, Malagnini L, Mueller CS (2005) Uncertainty analysis for seismic hazard in Northern and Central Italy. Ann Geophys 48:853–865
Main IG (1996) Statistical physics, seismogenesis and seismic hazard. Rev Geophys 34:433–462
Main IG, Li L, McCloskey J, Naylor M (2008) Effect of the Sumatran mega-earthquake on the global magnitude cut-off and event rate. Nat Geosci 1:142. doi:10.1038/ngeo141
McGuire RK (1976) FORTRAN computer program for seismic risk analysis. US Geol Surv, Open File Rep No. 76–67
McGuire RK (1978) FRISK—a computer program for seismic risk analysis. US Department of Interior. Geol Surv Open File Rep 78–1007
Mirzaei N (1997) Seismic zoning of Iran. PhD dissertation, Institute of Geophysics. State Seismological Bureau, Beijing, 139pp
Mirzaei N, Kazemian J, Karluti E, Shabani E (2000) Seisrisk iii+ manual. Geophysic Institute of Tehran University
Mona L (2005) Seismic hazard assessment of North Western Himalayan fold and Thrust Belt Pakistan. Chapter 6 of PhD Dissertation. Quid e Azam University, Islamabad
National Geodatabase of Iran (www.ngdir.ir)
Orozova IM, Suhadolc P (1999) A deterministic-probabilistic approach for seismic hazard assessment. Tectonophysics 312:191–202
Peruzza L, Slejko D, Bragato PL (2000) The Umbria-Marche case: some suggestions for the Italian seismic zonation. Soil Dyn Earthq Eng 20:361–371
Reiter L (1990) Earthquake hazard analysis: issues and insights. Columbia Univ. Press, New York
Richter CH (1958) Elementary seismology. W.H. Freeman, New York
Shi Z, Zhang Y (1996) Seismic intensity zoning mapof China. In: Achievements of seismic hazard prevention and reduction in China. Seismological Press, Beijing, pp 143–164
Shi Z, Yan J, Gao M (1992) Researchon the principle and methodology of Seismic zonation—result of the trial in North China. Acta Seismol Sin 5:305–314
Stepp JC (1973) Analysis of completeness of the earthquake sample in the Puget sound area. In: Contribution to seismic zoning, NOAA Tech. Report, ERL 267-ESL30, Washington, D.C.
Tchalenko JS (1975) Seismicity and structure of the Kopet Dagh (Iran, USSR). Phil Trans R Soc 278:1–25
Todorovska MI, Gupta ID, Gupta VK, Lee VW, Trifunac MD (1995) Selected topics in probabilistic seismic hazard analysis. Report No. CE95-08. Dept. of Civil Eng., Univ. of Southern California, Los Angeles
Trifonov VG (1978) Late quaternary tectonic movements of Western and Central Asia. Bull Geol Soc Am 89:1059–1072
Trifunac MD (1990) A microzonation method based on uniform risk spectra. Soil Dyn Earthq Eng 9(1):34–43
Turcotte DL (1992) Fractals and chaos in geology and geophysics. Cambridge Univ. Press, New York
Wang Z (2005) Discussion—Klügel, J.-U. 2005 problems in the application of the SSHAC probability method for assessing earthquake hazards at Swiss nuclear power plants. Eng Geol 78:285–307
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Esmaeilabadi, R., Abasszadeh Shahri, A., Behzadafshar, K. et al. Frequency content analysis of the probable earthquake in Kopet Dagh region—Northeast of Iran. Arab J Geosci 8, 3833–3844 (2015). https://doi.org/10.1007/s12517-014-1446-3
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DOI: https://doi.org/10.1007/s12517-014-1446-3