Skip to main content
Log in

Retrospective Prediction of Location and Intensity for Two Large Crustal Earthquakes in Iran and India

  • Published:
Journal of Volcanology and Seismology Aims and scope Submit manuscript

Abstract

This paper reports results of mathematical modeling applied to the stress and strain in epicentral zones before and after the large earthquakes that occurred on June 22, 2002 in the Qazvin Province, northwestern Iran (Mw = 6.4) and the Gujarat, India earthquake of January 26, 2001 (M = 6.9). The modeling relied on a method for calculating stress and strain in a blocky elastic isotropic heterogeneous medium disturbed by a set of faults that are due to an external tectonic stress field. The boundary conditions were specified based on geological and seismological data. It has been shown that the epicenters of large crustal earthquakes occur in zones of high stress concentration at the ends of tectonic faults. Rupture occurs when the relationship between acting tectonic stresses satisfies the requirement σyyxx >3, thus connecting zones of high stress. The evolution of the aftershock process is controlled by the stress drop caused by a new rupture, while the resulting aftershock clusters are in spatial correlation with the stress drop zone. The new rupture propagates in the direction of dominant tectonic fault orientation in the region. We show a relationship to exist between rupture length and the possible retrospectively predicted location and magnitude of the earthquake depending on the elastic energy buildup and its possible release under specified structural tectonic conditions.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1.
Fig. 2.
Fig. 3.
Fig. 4.
Fig. 5.
Fig. 6.

Similar content being viewed by others

Notes

  1. A blind fault is understood in (Walker et al., 2005) as a fault that does not emerge at the surface.

  2. With due account of possible errors within ±5 km or more in epicenter location.

REFERENCES

  1. Alipoor, R., Hossein, A.S., and Ghamarian, S., Neotectonics of the Avaj region (NW Iran): left-lateral strike-slip and range-parallel reverse faults, Journal of Mountain Science, 2020, vol. 17, pp. 838–850. https://doi.org/10.1007/s11629-019-5688-0

    Article  Google Scholar 

  2. Benioff, Hugo, Mechanism and strain characteristics of the White Wolf fault as indicated by the aftershock sequence, California Division of Mines, Bull., 1955, vol. 171, pp. 199–202.

  3. Chester, F.M. and Chester, J.S., Ultracataclasite structure and friction processes of the Punchbowl fault, San Andreas system, California, Tectonophysics, 1998, vol. 295, nos. 1‒2, pp. 199–221. https://doi.org/10.1016/S0040-1951(98)00121-8

    Article  Google Scholar 

  4. Chester F.M., Evans, J.P., and Biegel, R.L., Internal structure and weakening mechanisms of the San Andreas fault, J. Geophys. Res., 1993, vol. 98, no. B1, pp. 771–786. https://doi.org/10.1029/92JB01866

    Article  Google Scholar 

  5. Chester, J.S., Chester, F.M., and Kronenberg, A.K., Fracture surface energy of the Punchbowl Fault, San Andreas system, Nature, 2005, vol. 437, pp. 133–136. https://doi.org/10.1038/nature03942

    Article  Google Scholar 

  6. Dinnik, A.N., Ustoichivost arok (The Stability of Arches), Moscow: OGIZ GOSTEKHIZDAT, 1946.

  7. Dowrick, D.J. and Rhoades, D.A., Relations between earthquake magnitude and fault rupture dimensions: How regionally variable are they?, Bull. Seismol. Soc. Amer., 2004, vol. 94, no. 3, pp. 776–788. https://doi.org/10.1785/0120030151

    Article  Google Scholar 

  8. Evans, J.P. and Chester, F.M., Fluid–rock interaction in faults of the San Andreas system: inference from San Gabriel fault rock geochemistry and microstructures, J. Geophys. Res., 1995, vol. 100, no. B7, pp. 13 007‒13 020. https://doi.org/10.1029/94JB02625

  9. Grown, E.T. and Hoek, E., Trends in relations between measured in situ stresses with depth, Intern. J. Rock Mech. Mining Sci., 1978, vol. 15, no. 4, pp. 211‒215.

    Article  Google Scholar 

  10. Gzovsky, M.V., A physical theory for the formation of tectonic ruptures, in Problemy tektonofiziki (Problems in Tectonophysics), Moscow: Gosgeolizdat, 1960, pp. 78‒89.

  11. Gzovsky, M.V., Osnovy tektonofiziki (Principles of Tectonophysics), Moscow: Nauka, 1975.

  12. Hamzehloo, H., Strong ground motion modelling of causative fault for the 2002 Avaj earthquake, Iran, Tectonophysics, 2005, vol. 409 nos. 1‒4, pp. 159–174. https://doi.org/10.1016/j.tecto.2005.08.016

    Article  Google Scholar 

  13. Kasahara, K., The nature of seismic origin as inferred from seismological and geodetic observations, Bull. Earthquake Res. Inst., Sept. 1957, vol. 35, part 3, 473–532.

    Google Scholar 

  14. Kocharyan, G.G., Geomekhanika razlomov (Fault Geomechanics), Moscow: GEOS, 2016.

  15. Morozov, V.N. and Manevich, A.I., Modeling the state of stress and strain in the epicentral area of the January 26, 2001 M 6.9, India earthquake, Geofiz. Issled., 2016, vol. 17, no. 4, pp. 23‒36. https://doi.org/10.21455/gr2016.4-2

    Article  Google Scholar 

  16. Morozov, V.N. and Manevich, A.I., The mechanism responsible for the rupture during the January 17, 1995 M 6.9 Hansin-Avazi, Kobe, Japan earthquake, Dokl. Akad. Nauk, Nauki o Zemle, 2021, vol. 499, no. 2, pp. 151–158. https://doi.org/10.21455/gr2016.4-2

  17. Morozov, V.N., Kaftan, V.I., Tatarinov, V.N., Kolesnikov, I.Yu., Manevich, A.I., and Melnikov, A.Yu., Numerical modeling of stress and strain and the results of GPS monitoring of the epicentral zone of the August 24, 2014 Napa, California earthquake, Geotektonika, 2018a, no. 5, pp. 90–102. https://doi.org/10.1134/S0016853X18040069

  18. Morozov, V.N., Tatarinov, V.N., Kolesnikov, I.Yu., and Manevich, A.I., Modeling the state of stess and strain in the epicentral zone of the large Iranian earthquake of December 26, 2003, Mw = 6.6), Fizika Zemli, 2018b, no. 4, pp. 68‒78. https://doi.org/10.1134/S0002333718040087

  19. Morozov, V.N., Tatarinov, V.N., and Manevich, A.I., Simulating the state of stress and strain in the epicentral zone of a large earthquake in Turkey (Izmit, 1999, M 7.4), J. Volcanol. Seismol., 2020, vol. 14, no. 2, pp. 105–114. https://doi.org/10.31857/S0203030620020042

    Article  Google Scholar 

  20. Ponomarev, V.S., Energonasyshchennost geologicheskoi sredy (The Energy Saturation in the Geologic Medium), Moscow: Nauka, 2008.

  21. Sadovsky, M.A. and Pisarenko, V.F., Seismicheskii protsess v blokovoi srede (The Seismic Process in a Blocky Medium), Moscow: Nauka, 1991.

  22. Schulz, S.E. and Evans, J.P., Mesoscopic structure of the Punchbowl fault Southern California and the geological and geophysical structure of active faults, J. Struct. Geol., 2000, vol. 22, no. 7, pp. 913–930. https://doi.org/10.1016/S0191-8141(00)00019-5

    Article  Google Scholar 

  23. Selin, K.V., The variation in original horizontal stresses over depth in a massif in various regions worldwide, Gorn. Inf.-Anal. Byul., 2008, no. 10, pp. 297‒301.

  24. Sherman, S.I., Seminsky, S.A., Bornyakov, S.A., Buddo, V.Yu., Lobatskaya, R.M., Adamovich, A.N., Truskov, V.A., and Babichev, A.A., Razlomoobrazovanie v litosfere: zony sdviga (Fault Generation in the Lithosphere: Shear Zones), Novosibirsk: Nauka, 1992.

  25. Walker, R.T., Bergman, E., Jackson, J., Ghorashi, M., and Talebian, M., The 2002 June 22 Changureh (Avaj) earthquake in Qazvin province, northwest Iran: epicentral relocation, source parameters, surface deformation and geomorphology, Geophys. J. Int., 2002, vol. 160, no. 2, pp. 707–720. https://doi.org/10.1111/j.1365-246x.2005.02516.x

    Article  Google Scholar 

  26. Western Iran–M 6.5, Earthquake Hazard Program USGS. URL: https://earthquake.usgs.gov/earthquakes/eventpage/usp000b6pk/executive (14.04.2022)

  27. Wells, D.L. and Coppersmith, K.J., New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement, Bull. Seismol. Soc. Amer., 1994, vol. 84, no. 4, pp. 975–1002.

    Google Scholar 

  28. Zabrodin, V.Yu., Rybas, O.V., and Gilmanova, G.Z., Razlomnaya tektonika materikovoi chasti Dalnego vostoka Rossii (The Fault Tectonics of the Continental Far East of Russia), Vladivostok: Dalnauka, 2015.

  29. Zubkov, A.V., A law governing the formation of natural state of stress in the crust, Litosfera, 2016, no. 5, pp. 146‒151.

Download references

ACKNOWLEDGMENTS

We used equipment and materials supplied by the Analytical Center of Geomagnetic Data, Geophysical Center, Russian Academy of Sciences (http://ckp.gcras.ru/).

Funding

This work was supported through a government assignment of the RAS Geophysical Center approved by the Ministry of Education and Science of Russia.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to A. I. Manevich.

Ethics declarations

The authors declare that they have no conflicts of interest.

Additional information

Translated by A. Petrosyan

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Morozov, V.N., Manevich, A.I. & Tatarinov, V.N. Retrospective Prediction of Location and Intensity for Two Large Crustal Earthquakes in Iran and India. J. Volcanolog. Seismol. 17, 219–227 (2023). https://doi.org/10.1134/S074204632370015X

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S074204632370015X

Keywords:

Navigation