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Abstrakty
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
Wydawca
Czasopismo
Rocznik
Tom
Strony
1462--1494
Opis fizyczny
Bibliogr. 43 poz.
Twórcy
autor
- International Institute of Earthquake Engineering and Seismology, Tehran, Iran
autor
- International Institute of Earthquake Engineering and Seismology, Tehran, Iran
autor
- 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.
- Ashkpour, M.S., and M. Mostafazadeh (2008), Source parameters of the Mw 5.8 Fin (South of Iran) earthquake of March 25, 2006, World Appl. Sci. J. 4, 1, 104- 115.
- Baker, C. (1993), Active seismicity and tectonics of Iran, Ph.D. Thesis, University of Cambridge, Cambridge.
- Baker, C., J. Jackson, and K. Priestley (1993), Earthquakes on the Kazerun line in the Zagros mountains of Iran: strike-slip faulting within a fold-and-thrust belt, Geophys. J. Int. 115, 1, 41-61, DOI: 10.1111/j.1365-246X.1993. tb05587.x.
- 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.
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- GCMT (2015), Global Centroid Moment Tensor (GCMT) catalog, Harvard University Seismology Department, available from: http://www.Globalcmt.org/ CMT.search.html.
- Gulia, L., S. Wiemer, and M. Wyss (2012), Catalog artifacts and quality controls, Community Online Resource for Statistical Seismicity Analysis, DOI: 10.5078/corssa-93722864, available from: http://www.corssa.org.
- 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.
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- 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.
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- 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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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-1b3a3afc-32d6-467d-9e52-93c8113ca69c