دانشگاه علوم پزشکی شهید بهشتی
  • Register
  • Login
  • English
    • فارسی

Irtiqa Imini Pishgiri Masdumiyat (Safety Promotion and Injury Prevention)

  • Home
  • About
    • About the Journal
    • Indexing & Abstracting
    • Editorial Team
  • Issues
    • Current
    • Archives
  • Journal Policies
    • Article Processing Charge (APC)
    • Privacy Statement
    • Archiving
    • Open Access
  • Guidelines
    • for Authors
    • Authorship Criteria
    • Declaration
    • for Reviewers
  • Publication Ethics
  • Conference Proceedings
    • The 13th Student Scientific Conference of Innovation Health Sciences
    • The 9th Iranian Congress of Epidemiology
    • The fourth international conference and the fifth conference biennial Ergonomics of Iran
  • Contact
Advanced Search
  1. Home
  2. Archives
  3. Vol. 10 No. 1 (1401)
  4. Original article

Vol. 10 No. 1 (1401)

June 2022

Analysis of the Seismicity Parameters and Strong Ground Movement in Sarpol-e Zahab and its Related Crises

  • Zhamak Monazami-Tehrani
  • Ghazaleh Monazami-Tehrani
  • Arezou Dorostian
  • Bahram Akashe
  • Mahmoud Almasian

Irtiqa Imini Pishgiri Masdumiyat (Safety Promotion and Injury Prevention), Vol. 10 No. 1 (1401), 7 June 2022 , Page 95- 87
https://doi.org/10.22037/iipm.v10i1.36583 Published: 2022-08-01

  • View Article
  • Download
  • Cite
  • References
  • Statastics
  • Share

Abstract

Background and Objectives: The occurrence of natural disasters can be considered one of the most important concerns of human life, especially for the people of developing countries.  The existence of natural disasters in Iran has made Iran one of the top 10 countries in the world in terms of disasters.  Analysis of seismic data shows that almost every 5 years, on average, an earthquake with a magnitude of 7 (such as the Saravan and Sarpol-e-Zahab -Kermanshah earthquakes) occurs in Iran and has serious effects on human society. In this study, the parameters of strong ground motion in the Sarpol-e-Zahab area have been analyzed with a special focus on its crisis.

Material and methods: To evaluate the earthquake's return period in this fault system, two preliminary relationships of Gutenberg-Richter and the final distribution of the Kijku-Sellovel method have been used. In order to study seismicity and seismic hazard analysis, after checking the geology of the study area, the tectonics and seismicity of the region were studied. After that, a tectonic seismic model was prepared from this zone to determine the nature of seismicity better. Then, the seismic source database of the study area was defined and entered into EZ-frisk software for further analysis.

Results: The magnitude of the earthquakes based on the Gutenberg-Richter and Kijku-Sellovel methods has shown that the magnitude of the earthquake in the 475-year return period is 6.9Ms and 7.0Ms, subsequently. A magnitude of more than 7.8 is not expected in this region based on the Gutenberg-Richter method. On the other hand, the values of acceleration on the side where the fault slope is (northeast of the fault), have higher values than on the opposite side. In addition, the maximum acceleration of the earthquake in the position of the mountain frontal fault is estimated at 0.75 gals.

Conclusion: Therefore, considering the importance of the study area (geologically), the existence of active and important faults in this region, as well as political-security threats, the existence of spatial exchanges and links on both sides of the border, and the underdevelopment of study and planning in the field of crisis management of this region seems necessary. Also, according to the results of the earthquake return period in this region, raising the level of urban environment flexibility against the stresses caused by the crisis and minimizing the time of rehabilitation and resilience of cities are among the most important factors that should be considered in planning and managing cities.

How to cite this article: Monazami-Tehrani Z, Monazami-Tehrani GH, Drstian A, Akasheh B, Almasian M. Analysis of the Seismicity Parameters and Strong Ground Movement in Sarpol-e Zahab and its Related Crises. Irtiqa Imini Pishgiri Masdumiyat. 2022;10(1):80-6.

Keywords:
  • Zagros Fault System
  • Earthquake recurrence interval Assessment
  • ZMAP Software
  • Upcoming Earthquake
  • pdf8 (فارسی)

How to Cite

1.
Monazami-Tehrani Z, Monazami-Tehrani G, Dorostian A, Akashe B, Almasian M. Analysis of the Seismicity Parameters and Strong Ground Movement in Sarpol-e Zahab and its Related Crises. Irtiqa Imini Pishgiri Masdumiyat [Internet]. 2022 Aug. 1 [cited 2026 Oct. 15];10(1):95-87. Available from: https://journals.sbmu.ac.ir/spip/article/view/36583
  • ACM
  • ACS
  • APA
  • ABNT
  • Chicago
  • Harvard
  • IEEE
  • MLA
  • Turabian
  • Vancouver
  • Endnote/Zotero/Mendeley (RIS)
  • BibTeX

References

. Zare M, Hashemi SA, Rahmani R. Seismic Hazard Analysis and Developping the Acceleration Zoning Maps in the Khark Island, Persian Gulf Iran. Journal of Natural Environmental Hazards. 2015 22;4(5):1-2.

Berberian M, Yeats RS. Patterns of historical earthquake rupture in the Iranian Plateau. Bulletin of the Seismological society of America. 1999;89(1):120-39.

Farahpour MM, Hessami K. Cretaceous sequence of deformation in the SE Zagros fold–thrust belt. Journal of the Geological Society. 2012;169(6):733-43.

Saura E, Vergés J, Homke S, Blanc E, Serra-Kiel J, Bernaola G, Casciello E, Fernández N, Romaire I, Casini G, Embry JC. Basin architecture and growth folding of the NW Zagros early foreland basin during the Late Cretaceous and early Tertiary. Journal of the Geological Society. 2011 Jan 1;168(1):235-50.

Agard P, Omrani J, Jolivet L, Whitechurch H, Vrielynck B, Spakman W, Monié P, Meyer B, Wortel R. Zagros orogeny: a subduction-dominated process. Geological Magazine. 2011 Nov;148(5-6):692-725.

Walpersdorf A, Hatzfeld D, Nankali H, Tavakoli F, Nilforoushan F, Tatar M, Vernant P, Chéry J, Masson F. Difference in the GPS deformation pattern of North and Central Zagros (Iran). Geophysical Journal International. 2006;167(3):1077-88.

Barzegari A, Ghorashi M, Nazari H, Shokri MA, Porkermani M. Evaluation of earthquake recurrence interval at Astara fault system based on seismic catalogs (NW of Iran). Scientific Quarterly Journal of Geosciences. 2016;25(98):83-92.

Harrison J, T Oberländer. Oberländer T. The Zagros streams: a new interpretation of transverse drainage in an orogenic zone. Syracuse University Press. 1967: 133- 80.

Eshaghi A, Pour-Mohammad Shahvar M, Farzanegan E, Mirzaei Alavijeh H. Source and strong ground motion parameters estimation of the November 12, 2017, Sarpol-e Zahab, Kermanshah earthquake using recorded accelerograms of Iran earthquake strong motion network. Iranian Journal of Geophysics. 2019;12(4):157-71.

Cornell CA. Engineering seismic risk analysis. Bulletin of the seismological society of America. 1968;58(5):1583-606.

Gutenberg B, Richter CF. Earthquake magnitude, intensity, energy, and acceleration: (Second paper). Bulletin of the seismological society of America. 1956;46(2):105-45.

Zare M. Relationships for Magnitude, intensity and pike horizontal acceleration base on Iranian Earthquakes. journal of seismology and engineering earthquake and research. 1995; 6:12-4.

Nowroozi AA. Empirical relations between magnitudes and fault parameters for earthquakes in Iran. Bulletin of the Seismological Society of America. 1985;75(5):1327-38.

El Adnani M, Yétongnon K, Benslimane D. A multiple layered functional data model to support multiple representations and interoperability of GIS: application to urban management systems. InProceedings of the 9th ACM international symposium on Advances in geographic information systems. 2001; 70-5.

Weichert DH. Estimation of the earthquake recurrence parameters for unequal observation periods for different magnitudes. Bulletin of the Seismological Society of America. 1980;70(4):1337-46.

Kijko A, Sellevoll MA. Estimation of earthquake hazard parameters from incomplete data files. Part II. Incorporation of magnitude heterogeneity. Bulletin of the Seismological Society of America. 1992;82(1):120-34.

Adibi A, Zarifi F. The role and status of passive defense with a view to the geography of Khuzestan Province. Quarterly journal of disciplinary knowledge of Khuzestan. 2013. 5: 119-46.

Berberian M. Earthquakes and coseismic surface faulting on the Iranian Plateau. Elsevier; 2014.

Douglas J. Ground motion prediction equations 1964–2019. University of Strathclyde, August. 2019:81-94.

Douglas J. Ground-motion prediction equations 1964-2010. Pacific Earthquake Engineering Research Center; 2011.

Shoja–Taheri J, Naserieh S, Hadi G. A test of the applicability of NGA models to the strong ground-motion data in the Iranian plateau. Journal of Earthquake Engineering. 2010 Jan 6;14(2):278-92.

Campbell KW, Bozorgnia Y. NGA ground motion model for the geometric mean horizontal component of PGA, PGV, PGD and 5% damped linear elastic response spectra for periods ranging from 0.01 to 10 s. Earthquake spectra. 2008;24(1):139-71.

Idriss IM. An NGA empirical model for estimating the horizontal spectral values generated by shallow crustal earthquakes. Earthquake spectra. 2008;24(1):217-42.

Abrahamson N, Silva W. Summary of the Abrahamson & Silva NGA ground-motion relations. Earthquake spectra. 2008;24(1):67-97.

Chiou BJ, Youngs RR. An NGA model for the average horizontal component of peak ground motion and response spectra. Earthquake spectra. 2008;24(1):173-215.

Mahsuli M, Rahimi H, Bakhshi A. Probabilistic seismic hazard analysis of Iran using reliability methods. Bulletin of Earthquake Engineering. 2019 Mar;17(3):1117-43.

Zare M. Seismic hazard zoning in Iran: a state-of-the-art on the studies during four decades. Journal of Seismology and Earthquake Engineering. 2017 Jul 1;19(2):71-101.

Nayeri M, Shieh E, Rezaei M, Saeidi Rezvani N. Managing neighborhood resilience in earthquake encountered in urban exhausted tissues with FAHP method (Case studyL Abdolabad, Tehran). Geography (Regional Planning). 2018 May 22;8(2):21-38.

Rezaei MR, Rafieian M, Hosseini SM. Measurement and evaluation of physical resilience of urban communities against earthquake (Case study: Tehran neighborhoods). Human Geography Research. 2015 Dec 22;47(4):609-23.

  • Abstract Viewed: 361 times
  • pdf8 (فارسی) Downloaded: 202 times

Download Statastics

  • Linkedin
  • Twitter
  • Facebook
  • Google Plus
  • Telegram

Developed By

Open Journal Systems

Language

  • فارسی
  • English

Information

  • For Readers
  • For Authors
  • For Librarians
  • Home
  • Archives
  • Submissions
  • About the Journal
  • Editorial Team
  • Contact

Creative Commons License

This journal is distributed under the terms of CC BY-NC 4.0.

ISSN-Online: 2383-1901| ISSN-Print: 2345-2455

                      https://goo.gl/maps/Q5TCJTUWtv7nqhe1A

Powered by OJSPlus