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Earthquake Potential in the Zagros Region, Iran

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Seismic strain and b value are used to quantify seismic potential in the Zagros region (Iran). Small b values (0.69 and 0.69) are related to large seismic moment rates (9.96×1017 and 4.12×1017) in southern zones of the Zagros, indicating more frequent large earthquakes. Medium to large b values (0.72 and 0.92) are related to small seismic moment rates (2.94×1016 and 6.80×1016) in middle zones of the Zagros, indicating less frequent large earthquakes. Small b value (0.64) is related to medium seismic moment rate (1.38×1017) in middle to northern zone of the Zagros, indicating frequent large earthquakes. Large b value (0.87) is related to large seismic moment rate (2.29×1017) in northwestern zone, indicating more frequent large earthquakes. Recurrence intervals of large earthquakes (M > 6) are short in southern (10 and 14 years) and northwestern (13 years) zones, while the recurrence intervals are long in the middle (46 and 114 years) and middle to northern (25 years) zones.
Słowa kluczowe
Czasopismo
Rocznik
Strony
1462--1494
Opis fizyczny
Bibliogr. 43 poz.
Twórcy
  • International Institute of Earthquake Engineering and Seismology, Tehran, Iran
  • International Institute of Earthquake Engineering and Seismology, Tehran, Iran
  • Department of Physics, Persian Gulf University, Bushehr, Iran
Bibliografia
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  • Alavi, M. (1994), Tectonics of the Zagros orogenic belt of Iran: New data and interpretations, Tectonophysics 229, 3-4, 211-238, DOI: 10.1016/0040-1951(94) 90030-2.
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  • Berberian, M. (1995), Master blind thrust faults hidden under the Zagros folds: Active basement tectonics and surface morphotectonics, Tectonophysics 241, 3-4, 193-224, DOI: 10.1016/0040-1951(94)00185-C.
  • Ekstrom, G., and P. England (1989), Seismic strain rates in regions of distributed continental deformation, J. Geophys. Res. 94, B8, 10231-10257, DOI: 10.1029/JB094iB08p10231.
  • Frohlich, C., and S. Davis (1993), Teleseismic b values: or, much ado about 1.0, J. Geophys. Res. 98, B1, 631-644, DOI: 10.1029/92JB01891.
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  • Gutenberg, B., and C.F. Richter (1944), Frequency of earthquakes in California, Bull. Seismol. Soc. Am. 34, 4, 185-188.
  • Gutenberg, B., and C.F. Richter (1954), Seismicity of the Earth and Related Phenomena, Princeton University Press.
  • Hanks, T.C., and H. Kanamori (1979), A moment magnitude scale, J. Geophys. Res. 84, 2348-2350.
  • Heaton, T.H., and H. Kanamori (1984), Seismic potential associated with subduction in the northwestern United States, Bull. Seismol. Soc. Am. 74, 3, 933-941.
  • Jackson, J., and D. McKenzie (1988), The relationship between plate motions and seismic moment tensors and the rates of active deformation in the Mediterranean and Middle East, Geophys. J. Int. 93, 1, 45-73, DOI: 10.1111/ j.1365-246X.1988.tb01387.x.
  • Jackson, J., J. Haines, and W. Holt (1995), The accommodation of Arabia-Eurasia plate convergence in Iran, J. Geophys. Res. 100, B8, 15205-15219, DOI: 10.1029/95JB01294.
  • Kadinsky-Cade, K., and M. Barazangi (1982), Seismotectonics of southern Iran: the Oman Line, Tectonics 1, 5, 389-412, DOI: 10.1029/TC001i005p00389.
  • Kijko, A., and M.A. Sellevoll (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, 3, 645-654.
  • Maggi, A., J.A. Jackson, K. Priestley, and C. Baker (2000), A re-assessment of focal depth distributions in Southern Iran, the Tien Shan and Northern India: do earthquakes really occur in the continental mantle? Geophys. J. Int. 143, 3, 629-661, DOI: 10.1046/j.1365-246X.2000.00254.x.
  • Masson, F., J. Chery, D. Hatzfeld, J. Martinod, P. Vernant, F. Tavakoli, and M. Ghafory-Ashtiani (2005), Seismic versus a seismic deformation in Iran inferred from earthquakes and geodetic data, Geophys. J. Int. 160, 1, 217-226, DOI: 10.1111/j.1365-246X.2004.02465.x.
  • McQuarrie, N. (2004), Crustal-scale geometry of the Zagros fold-thrust belt, Iran, J. Struct. Geol. 26, 3, 519-535, DOI: 10.1016/j.jsg.2003.08.009.
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  • Mostafazadeh, M.,O. Alptekin, and A.O. Oncel (2000), Body waveform modeling of five moderately earthquakes in the Zagros fold thrust belt, J.S.E.E. 2, 3, 1- 10.
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  • Shahvar, M.P., M. Zare, and S. Castellaro (2013), A unified seismic catalog for the Iranian Plateau (1900-2011), Seism. Res. Lett. 84, 2, 233-249, DOI: 10.1785/0220120144.
  • Talebian, M., and J. Jackson (2004), A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran, Geophys. J. Int. 156, 3, 506-526, DOI: 10.1111/j.1365-246X.2004.02092.x.
  • Tsapanos, T.M. (1990), b values of two tectonic parts in the Circum-Pacific belt, Pure Appl. Geophys. 134, 2, 229-242, DOI: 10.1007/BF00876999.
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  • Vernant, P., F. Nilforoushan, D. Hatzfeld, M.R. Abbassi, C. Vigny, F. Masson, H. Nankali, J. Martinod, A. Ashtiani, R. Bayer, F. Tavakoli, and J. Chery (2004), Present-day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman, Geophys. J. Int. 157, 1, 381-398, DOI: 10.1111/j.1365-246X.2004.02222.x.
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  • Walpersdorf, A., D. Hatzfeld, H. Nankali, F. Tavakoli, F. Nilforoushan, M. Tatar, P. Vernant, J. Chery, and F. Masson (2006), Difference in the GPS deformation pattern of North and Central Zagros (Iran), Geophys. J. Int. 167, 3, 1077-1088, DOI: 10.1111/j.1365-246X.2006.03147.x.
  • Ward, S. (1994), A multidisciplinary approach to seismic hazard in southern California, Bull. Seismol. Soc. Am. 84, 5, 1293-1309. Wiemer, S. (2001), A software package to analyze seismicity: ZMAP, Seism. Res. Lett. 72, 373-382, DOI: 10.1785/gssrl.72.3.373.
  • Wiemer, S., and M. Wyss (2000), Minimum magnitude of complete reporting in earthquake catalogs: examples from Alaska, the Western United States, and Japan, Bull. Seismol. Soc. Am. 90, 4, 859-869, DOI: 10.1785/0119990114.
  • Wiemer, S., S.R. McNutt, and M. Wyss (1998), Temporal and three dimensional spatial analysis of the frequency-magnitude distribution near Long Valley caldera, California, Geophys. J. Int. 134, 2, 409-421, DOI: 10.1046/j.1365- 246x.1998.00561.x.
  • Woessner, J., and S. Wiemer (2005), Assessing the quality of earthquake catalogues: Estimating the magnitude of completeness and its uncertainty, Bull. Seismol. Soc. Am. 95, 2, 684-698, DOI: 10.1785/0120040007.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-1b3a3afc-32d6-467d-9e52-93c8113ca69c
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