Development of Faults and Prediction of Earthquakes in the Himalayas

  • A. K. Dubey Department of Petroleum Engineering, Graphic Era Deemed to be University, Dehradun, India
Keywords: Faults and faulting, Himalayan thrusts, Oil trap, Seismicity, Superimposed deformation


Recurrence period of high magnitude earthquakes in the Himalayas may be of the order of hundreds of years but a large number of smaller earthquakes occur every day. The low intensity earthquakes are not felt by human beings but recorded in sensitive instruments called seismometers. It is not possible to get rid of these earthquakes because the mountain building activity is still going on. Continuous compression and formation of faults in the region is caused by northward movement of the Indian plate. Some of the larger faults extend from Kashmir to Arunachal Pradesh. Strain build up in the region results in displacement along these faults that cause earthquakes. Types of these faults, mechanism of their formation and problems in predicting earthquakes in the region are discussed.


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Davis, G. H., Reynolds, S. J., & Kluth, C. F. (2011). Structural geology of rocks and regions. John Wiley & Sons.

Dubey, A. K. (2014). Understanding an orogenic belt: structural evolution of the Himalaya. Springer.

Gansser, A. (1964). Geology of the Himalayas. Interscience, New York, 289 pp.

Kandpal, G. C., Joshi, K. C., Joshi, D. D., Singh, B. K., & Singh, J. (2006). Signature of quaternarytectonics in a part of Dehra Dun valley, Uttaranchal. Journal Geological Society of India, 67, 147-150.

Rautela, P. & Sati, D. (1996). Recent crustal adjustments in Dehra Dun valley, western Uttar Pradesh, India. Current Science, 71, 776-780.

Srivastava, D. C. & John, G. (1999). Deformation in the Himalayan frontal fault zone : Evidence from small scale structures in Mohand-Khara area, NW Himalaya. Gondwana Research Group Memoir, Osaka, Japan, 6, 273-284.

Valdiya, K. S., Joshi, D. D., Sanwal, R., & Tandon, S. K., (1984). Geomorphic development across the active main boundary thrust: an example from the Nainital hills in Kumaun Himalaya. Journal Geological Society of India, 25(12), 761-774.

Yeats, R.S. &Thakur, V. C. (1998). Reassessment of earthquake hazard based on a fault-bend fold model of the Himalayan plate-boundary fault. Current Science, 74(3), 230-233