Earthquake hazard zoning using Analytical Hierarchy Process (AHP) and fuzzy logic (study area: Southern Khorasan Province)

Document Type : Original Article

Authors

1 MSc Student, University of Birjand

2 Professor, University of Birjand,

3 Assistant Professor, University Birjand,

Abstract

Southern-khorasan Province is located in east of Iran and northern part of Sistan Suture Zone. Active faults and different earthquake occurrences imply high seismic potential in this province. In this zonation, several factors such as seismic moment, seismic is acceleration, is fractures, distance from fault, alluvial depth and erosion province maps are used. Hazard zonation shows more than 40% of Province is located in very high to high risk classes, 16% in medium risk class and 40.6% in low to very low risk classes. The results of zoningmapshowsmost riskofoccurrence ofearthquakes are coinciding with environs of Ardekol(city Haji Abad), Dasht- e- bayaz(Nimblock, Qayen), the eastern part ofthe Doroneh (Ferdows, Tabas), Giv(Birjand), Sedeh(Sedeh, Ariancity), Naiband(Tabas, Khuor), Ferdows  (Ferdows, Sarayan), Esfandiar(Boshrooyeh) andthenfaultShah Abad(Sarbisheh, Darmiyan, Asadiyeh), Sahl Abad(Darmiyan, Asadiyeh), Abgarm(Gazik), Pourang(Sarbisheh, Darmiyan, Gazik), Nozad (Sarbishe, Darmiyan, Asadiye), Kalmard(Tabas, Khuor) andsouth of Birjand faults(Birjand). The comparison of AHP method and fuzzy logic shows that zoning map prepared by fuzzy logic has more coinciding with reality and in the meantime operators OR (community), Product (Multiplication algebraic) and Sum (sum) were fuzzy coincides with reality. Among them the OR fuzzy (community) has the best matching seismic areas.

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References
Ambraseys, N.N, Melill, C.P., 1982, A history of Persian earthquakes. Cambridge University press, Cambridge, UK, p.236.
Berberian, M., 1979. Earthquake faulting and bedding thrust associated with the Tabas- e- Golshan (Iran) Earthquake of September 16, 1978. Bulletin of the seismological Society of America, 69, p. 1861- 1887.
Campbell, A.N., 1982, Recognition of a Hidden Mineral deposit by an Artificial Intelligence Program, Science, V. 217(3), p. 927- 929.
Chung, C.F., and Fabbri, A.G., 1993, the Representation of Geosciences Information for Data Integration, Nonrenewable Resources, V. 2(2), p. 122- 139.
Champati-ray, P.K., Dimri, S., Lakhera, R.C., and Sati, S., 2007, Fuzzy- based method for landslide hazard assessment in active seismic zone of Himalaya, Landslides, 4: p. 101-111.
Gooijer, J., Hyndman, R., 2006, 25 Years of Time Series Forecasting, International Journal of Forecasting, No. 2. p. 443- 473.
Mojarad, M., Hossein, M., Zare, M., Morshedy, A.H., Pishahang, M.H., 2014, Modeling of the seimotectonic provinces of Iran using the self- organizing map algorithm. Computers & Geosciences, V. 67. p. 150- 162.
Mohajer- Ashjai, A., Nowroozi, A.A., 1978, Observed and probable intensity zoning if Iran, Tectonophysics. 49, p. 149- 160.
Mohager, G.A., Pierce, G.R., 1963, Qazvin, Iran earthquake. Bull. Am. Assoc. Petrol. Geol., 47 (10), p. 1878- 1883.
Nowroozi, A.A., 1971, Seismotectonics of the Persian plateau, Eastern Turkey, Caucasus, and Hindukush region, Bull, Seismol, Soc.Am. 61. p. 317- 341.
Nowroozi, A.A., 1972, Focal mechanism of earthquakes in Persia, Turkey, West Pakistan and Afghanistan and plate tectonic of Middle East. Bull. Seismol. Soc. 46. p. 74- 96.
King Stephanie, A., Kiremdndgian, A., 1995, law lincho, Basoz Nersini, Earthquake Damage and loos Estimation through Gis, proceeding of Earthquake Engineering Spain, p. 325- 401.
Schwartz, D., Coopersmith, K.J., 1984, fault Behavior and Characteristic Earthquakes: Examples from the Wasatch and San Andreas Fault, J. Geophys. Res. 89, p. 5681- 5698.
Tirrule, R., Bell, L.R., Griffins, R.J., and Camp, V.E., 1983, The Sistan Suture zone of eastern Iran. G.S.A V. 94.., p. 134- 150.
Turcotte, D.L., 1992, Feractals and Chaos in Geology and Geophysics (Cambridge University Press, Cambridge), p.17.
Walker, R.T., Jackson, J., 2004, Active tectonic and late Cenozoic strain distribution in central and eastern Iran. Tectonics 23, PC5010. P.1-24.
Wells, D.L. and Coppersmith, K.J., 1994, New empirical relationship among magnitude, rupture length, rupture area and surface displacement, Bull. Seism. Soc. AM., 84, p. 974- 1002.
Zadeh, L.A., 1965, Fuzzy Sets, Information and Cintrol, No, 8, p. 339.
Zadeh, L.A., 1973, Outline of Approach to Analysis of Complex System and Decision Process, IEEE Trans on System Man and Cybernetic, SMC. 1, p. 28- 44