Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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Tectonic Implications of the Earthquakes in the Indian Subcontinent


Affiliations
1 Department of Applied Geology, Dr. H.S. Gour University, Sagar - 470 003, India
     

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The Bhuj earthquake (26 January 2001) in India and the Ghori earthquake (8 October 2005) in Pakistan, both occurred close to the Indian-Iranian plate boundary related to the activity along the intracontinental Chaman transform fault. It is suggested that the seismic activity along NNW to NNE trending weak zones or faults is more intense in the sub-continent than along the WNW trending zones, since the stress along the former is less compressive but more of the shear or translational type. The devastative Koyna (1967) and Latur (1993) earthquakes both occurred along faults or weak zones that were close to the meridional rather than the equatorial trend. The Indian plate is moving to the north or NNE or NNW, along a rotational trajectory and hence the force tends to be more compressive along the equatorial weak zones. In contrast, it tends to be less compressive and more of the shear or translational along the weak zones that are close to meridional trend. The seismic activity is therefore more intense along the weak zones with NNW to NNE trend than along the ENE to EW trending zones.

Keywords

Earthquakes, Seismicity, Meridional Trend, Equatorial Trend, Regmatic Fracture Pattern, Bhuj Earthquake, Ghori Earthquake.
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  • BENDICK, R., BILHEM, R., FIELDING, E., GAUR, V.K., HOUGH, S., KIER, G., KULKARNI, M.N. MARTIN, S., MUELLER, K. and MUKUL, M. (2001) The January 26, 2001 "Republic Day", Earthquake, India, Seism. Res. Lett., v.72(3), pp.328-335.

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  • WEBSITES: asc-india.org; cires.colorado.edu; earthquake.bgs.ac.uk; earthquake.usgs.gov; Geotimes.org.


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  • Tectonic Implications of the Earthquakes in the Indian Subcontinent

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Authors

Manish K. Purohit
Department of Applied Geology, Dr. H.S. Gour University, Sagar - 470 003, India
K. K. Prajapati
Department of Applied Geology, Dr. H.S. Gour University, Sagar - 470 003, India

Abstract


The Bhuj earthquake (26 January 2001) in India and the Ghori earthquake (8 October 2005) in Pakistan, both occurred close to the Indian-Iranian plate boundary related to the activity along the intracontinental Chaman transform fault. It is suggested that the seismic activity along NNW to NNE trending weak zones or faults is more intense in the sub-continent than along the WNW trending zones, since the stress along the former is less compressive but more of the shear or translational type. The devastative Koyna (1967) and Latur (1993) earthquakes both occurred along faults or weak zones that were close to the meridional rather than the equatorial trend. The Indian plate is moving to the north or NNE or NNW, along a rotational trajectory and hence the force tends to be more compressive along the equatorial weak zones. In contrast, it tends to be less compressive and more of the shear or translational along the weak zones that are close to meridional trend. The seismic activity is therefore more intense along the weak zones with NNW to NNE trend than along the ENE to EW trending zones.

Keywords


Earthquakes, Seismicity, Meridional Trend, Equatorial Trend, Regmatic Fracture Pattern, Bhuj Earthquake, Ghori Earthquake.

References