![]() Bull Seismol Soc Am 69:135–158Īnderson JG, Luco JE (1983) Consequences of slip rate constraints on earthquake occurrence relations. doi: 10.1029/2003TC001530Īmbraseys NN, Jackson JA, Melville CP (2002) Historical seismicity and tectonics: the case of the eastern mediterranean and the middle east, international handbook of earthquake and engineering seismology, V.81A, ISBN: 0-12-440652-1Īnderson J (1979) Estimating the seismicity from geological structure for seismic-risk studies. In: 11th Canadian Conference on Earthquake Engineering, 21–24 July, 2015, Victoria, Canada, Paper 93775Īllen M, Jackson J, Walker R (2004) Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates. At variance to previous models of the EMME region, we provide a homogeneous seismic source model representing a consistent basis for the next generation of seismic hazard models within the region.Īdams J, Halchuck S, Allen T, Rogers G (2015) Canada’s 5th Generation seismic hazard model for the 2015 National Building Code of Canada. Ultimately, alternative models of intrinsic uncertainties of data, procedures and models are considered when used for calculation of the seismic hazard. ![]() Recorded seismicity (both historical and instrumental) provides the input to estimate rates of earthquakes for area sources and background seismicity while geologic slip-rates are used to characterize fault-specific earthquake recurrences. A total of 234 area sources fully cross-border-harmonized are combined with 778 seismically active faults along with background-smoothed seismicity. The resulting seismogenic source model includes seismic sources defined by geological evidence and active tectonic findings correlated with measured seismicity patterns. We describe the development process of the model including the delineation of seismogenic sources and the description of methods and parameters of earthquake recurrence models, all representing the current state of knowledge and practice in seismic hazard assessment. We summarize multidisciplinary data (seismicity, geology, and tectonics) compiled and used to characterize the spatial and temporal distribution of earthquakes over the investigated region. ![]() Destructive earthquakes with great loss of life and property are frequent within this region, as exemplified by the recent events of Izmit (Turkey, 1999), Bam (Iran, 2003), Kashmir (Pakistan, 2005), Van (Turkey, 2011), and Hindu Kush (Afghanistan, 2015). The result covers eleven countries: Afghanistan, Armenia, Azerbaijan, Cyprus, Georgia, Iran, Jordan, Lebanon, Pakistan, Syria and Turkey, which span one of the seismically most active regions on Earth in response to complex interactions between four major tectonic plates i.e. The Earthquake Model of Middle East (EMME) project was carried out between 20 to provide a harmonized seismic hazard assessment without country border limitations. ![]()
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