References (in Persian)
Ambersz, Nicholas, Melville, Charles., (1991), Translated by Abolhassan Reddeh, Agah Publishing Institute. [In Persian]
Hasanzadeh, Bahram., Rahimi, Behnam., Mirzaei, Noorbakhsh., (2015), Seismotectonic investigation of the Central Kopeh Dagh range using Seismicity parameters and fractal dimension by specific attention to Bakharden–Quchan fault zone, Tectonics Journal, , Vol.1, No. 1. [In Persian]
Talebian, Morteza, (2012), Comparison of seismic, geodetic and geologic moment rates in Eastern Alborz and Kopeh Dagh, Scientific Quarterly Journal, Geosciences, Vol.22, No.86. , pp.183-192. [In Persian]
References (in English)
Berberian, M., (1994) , Natural Hazards and the first earthquake catalogue of Iran, Vol. 1: Historical Hazards in Iran Prior to 1900, International Institute of Earthquake Engineering and Seismology, Tehran, 603 p. in English & 66 p. in Persian.
Campbell, K.W., ( 1981) , Near source attenuation of peak horizontal acceleration, Bull. Seism. Soc. Am. 71, pp. 2039-2070.
Donovan,N.,(1973) , Earthquake hazards for building practices for disaster mitigation,building Science Series 46,Nat. Bur. of Standards,U.S. Dept. of Commerce, Washington.D.C, pp.82-110.
Esteva,L.,(1970), Seismic risk and design criteria for nuclear power plants, R.J.Jansen(ed),MT Press, Cambridge, Mass. p 142-182.
Hollingsworth, J., Jackson, J., Walker, R., Gheitanchi, M., Bolourch, M., (2006) ,Strike-slip faulting, rotation, and along-strike elongation in the Kopeh-Dagh Mountains, NE Iran. UGeophys. J. Int.U 166, pp. 1161–1177.
International Institute of Earthquake Engineering and Seismology (IIEES), http://www.iiees.ac.ir
Jackson, J., Priestley, K., Allen, M. , Berberian, M., )2002( , Active tectonics of the South caspian Basin, Geophys. J. Int. 148 , pp. 214-245.
Lyberis, N., and Manby, G., (1999) , Oblique to orthogonal convergence across the Turan block in the post-Miocene, American Association of Petroleum Geologists Bulletin, v. 83, pp. 1135–1160.
McKenzie, D. P .,( 1972) ,Active tectonics of the Mediterranean region, Geophysical Journal of the Royal Astronomical Society 30, pp. 109-185.
McKenzie, D .,(1978) , Some remarks on the development of sedimentary basins, Earth and Planetary Science Letters, 40, pp. 25-32.
Mohajer-Ashjai, A. & Nowroozi, A.A., (1987), Observed and probable intensity zoning of Iran, Tectonophysics, Vol.49, pp. 21-30.
Nowroozi, A.A., (1985), Empirical relations between magnitudes and fault parameters for earthquake in Iran, Bull Seis. Soc. Am., Vol. 75 (5) , pp.1327-1338.
Nowroozi, A.A, Ahmadi, G.,( 1986), Analysis of earthquake risk in Iran based on seismotectonic provinces, Tectonophysic, volume: 122.
Shabanian, E., Bellier, O., Abbassi, M. R., Siame, L., Arnaud, N. & Cocheme´, J. J.,(2009), New tectonic configuration in NE Iran: Active strikeslip Faulting between the Kopeh Dagh And Binalud mountains, Tectonics, 28: TC5002.
Slemmons, D.b., (1982), Determination of design earthquake magnitude for micrizonation. Proc. 3rd Int. Earthquake Micro. Conf., VI , pp. 119-130.
Tchalenko, J. S., )1975(, Seismicity and structure of the Kopet Dagh (Iran,U.S.S.R.), Royal Society, London, PTRMAD v. 278, n. 1275, pp. 1-28 .
Trifunac, M.D, and Brady, A.G., ( 1975), On the correlation of seismic intensity scales with peaks an recorded strong motion, Bull. Seism. Soc. Am., 65, pp. 139-173.
Wells, D.L. and Coppersmith, K.J., (1994), New empirical relationship among magnitude, rupture length, rupture area and surface displacement, Bull. Seism. Soc. AM., Vol. 84, No. 4, pp.974-1002.