Skip to main content
Log in

Estimation of seismic hazard in Gujarat region, India

  • Original Paper
  • Published:
Natural Hazards Aims and scope Submit manuscript

Abstract

The seismic hazard in the Gujarat region has been evaluated. The scenario hazard maps showing the spatial distribution of various parameters like peak ground acceleration, characteristics site frequency and spectral acceleration for different periods have been presented. These parameters have been extracted from the simulated earthquake strong ground motions. The expected damage to buildings from future large earthquakes in Gujarat region has been estimated. It has been observed that the seismic hazard of Kachchh region is more in comparison with Saurashtra and mainland. All the cities of Kachchh can expect peak acceleration in excess of 500 cm/s2 at surface in case of future large earthquakes from major faults in Kachchh region. The cities of Saurashtra can expect accelerations of less than 200 cm/s2 at surface. The mainland Gujarat is having the lowest seismic hazard as compared with other two regions of Gujarat. The expected accelerations are less than 50 cm/s2 at most of the places. The single- and double-story buildings in Kachchh region are at highest risk as they can expect large accelerations corresponding to natural periods of such small structures. Such structures are relatively safe in mainland region. The buildings of 3–4 stories and tall structures that exist mostly in cities of Saurashtra and mainland can expect accelerations in excess of 100 cm/s2 during a large earthquake in Kachchh region. It has been found that a total of 0.11 million buildings in Rajkot taluka of Saurashtra are vulnerable to total damage. In Kachchh region, 0.37 million buildings are vulnerable. Most vulnerable talukas are Bhuj, Anjar, Rapar, Bhachau, and Mandvi in Kachchh district and Rajkot, Junagadh, Jamnagar, Surendernagar and Porbandar in Saurashtra. In mainland region, buildings in Bharuch taluka are more vulnerable due to proximity to active Narmada-Son geo-fracture. The scenario hazard maps presented in this study for moderate as well as large earthquakes in the region may be used to augment the information available in the probabilistic seismic hazard maps of the region.

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
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12

Similar content being viewed by others

References

  • Aki K (1967) Scaling law of seismic spectrum. J Geophys Res 72:1217–1231

    Article  Google Scholar 

  • Anderson J, Hough S (1984) A model for the shape of the Fourier amplitude spectrum of acceleration at high frequencies. Bull Seismol Soc Am 74:1969–1993

    Google Scholar 

  • Arya AS (2000) Non-engineered construction in developing countries—an approach toward earthquake risk prediction. Proceedings of 12WCEE. Paper no 2824

  • Atkinson GM, Boore DM (1995) Ground motion relations for Eastern North America. Bull Seismol Soc Am 85:17–30

    Google Scholar 

  • Beresnev IA, Atkinson GM (1997) Modelling finite fault radiation from the ωn spectrum. Bull Seismol Soc Am 87:67–84

    Google Scholar 

  • BIS (2002) IS 1893 (Part 1)—2002: Indian standard criteria for earthquake resistant design of structures, part 1—general provisions and buildings. Bureau of Indian Standards, New Delhi

    Google Scholar 

  • Biswas SK (1980) Structure of Kutch-Kathiawar region, W India. Proceedings of 3rd Indian Geological Congress, Pune, pp 255–272

  • Biswas SK (1987) Regional tectonic framework, structure and evolution of the western marginal basins of India. Tectonophysics 135:307–327

    Article  Google Scholar 

  • Biswas SK (2005) A review of structure and tectonics of Kutch basin, western India, with special reference to earthquake. Curr Sci 88:1592–1600

    Google Scholar 

  • Bodin P, Horton S (2004) Source parameters and tectonic implications of aftershocks of the Mw7.6 Bhuj earthquake of January 26, 2001. Bull Seismol Soc Am 94:818–827

    Article  Google Scholar 

  • Bodin P, Malagnini L, Akinci A (2004) Ground-motion scaling in the Kachchh Basin, India, deduced from aftershocks of the 2001 Mw 7.6 Bhuj earthquake. Bull Seismol Soc Am 94:1658–1669

    Article  Google Scholar 

  • Boore D (1983) Stochastic simulation of high-frequency ground motions based on seismological models of the radiated spectra. Bull Seismol Soc Am 73:1865–1894

    Google Scholar 

  • Brune JN (1970) Tectonic stress and the spectra of seismic shear waves from earthquakes. J Geophys Res 75:4997–5009

    Article  Google Scholar 

  • Brune JN (1971) Seismic sources, fault plane studies and tectonics. EOS 52:178–187

    Article  Google Scholar 

  • Chopra S, Kumar D, Rastogi BK (2010) Attenuation of high frequency P and S waves in the Gujarat region, India. Pure Appl Geophys. doi:10.1007/s00024-010-0143-8

  • Chopra S, Kumar D, Rastogi BK, Choudhury P, Yadav RBS (2011a) Deterministic seismic scenario in Gujarat, India. Natural Hazards. doi:10.1007/s11069-011-0027-y

  • Chopra S, Kumar D, Rastogi BK, Choudhury P, Yadav RBS (2011b) Estimation of site amplification functions in Gujarat region, India, Natural Hazards. doi:10.1007/s11069-012-0116-6

  • GSI (2000) Seismotectonics Atlas of India and its environs. Geological Survey of India publications, p 87

  • Gupta HK, Rao PC, Rastogi BK, Sarkar D (2001a) The deadliest intraplate earthquake: perspectives. Science 291:2101–2102

    Article  Google Scholar 

  • Gupta HK, Harinarayana T, Kousalya M, Mishra DC, Mohan I, Rao NP, Raju PS, Rastogi BK, Reddy PR, Sarkar D (2001b) Bhuj earthquake of 26 January 2001. J Geol Soc India 57:275–278

    Google Scholar 

  • Iyengar RN, Raghukanth STG (2003) Attenuation of strong ground motion and site specific seismicity in Peninsular India. Proceedings of national seminar on seismic design of nuclear power plants, 21–22 February 2003, SERC Chennai, Allied Publ. Pvt. Ltd. N. Delhi

  • Kramer SL (1995) Geotechnical earthquake engineering. Prentice Hall, New Jersey

    Google Scholar 

  • Mandal P, Johnston A (2006) Estimation of source parameters for the aftershocks of the 2001 Mw 7.7 Bhuj earthquake, India. Pure Appl Geophys 163:1537–1560

    Article  Google Scholar 

  • Merh SS (1995) Geology of Gujarat. Geol Soc Ind, p 222

  • Motazedian D, Atkinson GM (2005) Stochastic finite-fault modeling based on dynamic corner frequency. Bull Seismol Soc Am 95:995–1010

    Article  Google Scholar 

  • Murakami H (2001) Outline of damage survey, A comprehensive survey of the 26 January 2001 earthquake (Mw7.7) in the state of Gujarat, India, Report by the Research Team Supported by the Grant-in-Aid for Specially Promoted Research Provided by the Japanese Ministry of Education, Culture, Sports, Science and Technology in the fiscal year of 2000 (Grant No. 12800019), Sato et al. pp 51–55

  • Rajendran CP, Rajendran K (2001) Characteristics of deformation and past seismicity associated with the 1819 Kutch earthquake, north western India. Bull Seismol Soc Am 91:407–426

    Article  Google Scholar 

  • Rastogi BK, Gupta HK, Mandal P, Satyanarayana HVS, Kousalya M, Raghavan R, Jain R, Sarma ANS, Kumar N, Satyamurthy C (2001) The deadliest stable continental region earthquake occurred near Bhuj on 26 January 2001. J Seismol 5:609–615

    Article  Google Scholar 

  • Reiter L (1990) Earthquake hazard analysis—issues and insights. Columbia University Press, New York

    Google Scholar 

  • Senoi RS (1991) Engineering Geology studies of some major Dam projects and reservoirs in the Narmada valley, M.P. SEG J

  • Singh SK, Bansal BK, Bhattacharya SN, Pacheco JF, Dattatrayam RS, Ordaz M, Suresh G, Kamal, Hough SE (2003) Estimation of ground motion for Bhuj (26 January 2001; Mw 7.6) and for future earthquakes in India. Bull Seismol Soc Am 93:353–370

    Article  Google Scholar 

  • Talwani P, Gangopadhyay A (2001) Tectonic framework of the Kachchh earthquake of 26 January 2001. Seism Res Lett 72:336–345

    Article  Google Scholar 

  • Wells DL, Coppersmith KJ (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Am 84:974–1002

    Google Scholar 

  • Yadav RBS, Tripathi JN, Rastogi BK, Chopra S (2008) Probabilistic assessment of earthquake hazard in Gujarat and adjoining region, India. Pure Appl Geophys 165:1813–1833

    Article  Google Scholar 

Download references

Acknowledgments

The authors are grateful to their respective organizations for support. The study was supported by the Ministry of Earth Sciences, Government of India, and Science and Technology Department, Government of Gujarat.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Sumer Chopra.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Chopra, S., Kumar, D., Rastogi, B.K. et al. Estimation of seismic hazard in Gujarat region, India. Nat Hazards 65, 1157–1178 (2013). https://doi.org/10.1007/s11069-012-0117-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11069-012-0117-5

Keywords

Navigation