Abstract

The Shillong Plateau is an earthquake-prone region in the northeastern India. Based on regional seismotectonic studies, we present here a deterministic seismic hazard assessment (DSHA) and maps of peak horizontal accelerations (PHA) for three largely populated districts – the East Khasi hills, the Ri-Bhoi, and the West Garo hills – within the Shillong Plateau. The hazard analysis methodology is based on the analysis of 72 earthquake sources (active faults) located within 500 km seismotectonic region around the plateau. Using an average sample log-likelihood approach, suitable ground motion prediction equations (GMPEs) are identified. As a variation in hypocentral distances can affect the ranks (or weights) of selected GMPEs, DSHA is performed separately for the three selected districts. Analyses show that the northern part of the East Khasi hills, eastern part of Ri-Bhoi district and the West Garo hills districts exhibit the highest PHA value of 0.46 g at site class A (hard rocks). In addition, response spectra for the Shillong city, Nongpoh, and Tura indicate that the maximum spectral acceleration reaches 0.67 g, 0.77 g, and 0.64 g at 0.1 s, respectively. These assessments indicate that the Barapani, Oldham, and Dauki faults influence significantly the seismic hazard in the studied region.

Highlights

  • The northeastern region of India (NE-India) is located between two plate boundaries: the Indian-Burmese plate boundary from the east and the Indian-Eurasian plate boundary from the north

  • deterministic seismic hazard assessment (DSHA) is performed for the three districts – East Khasi hills, Ri-Bhoi, and West Garo hills – within the Shillong Plateau

  • We have obtained that the peak horizontal accelerations (PHA) values range from 0.27 g to 0.46 g within these districts

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Summary

Introduction

The northeastern region of India (NE-India) is located between two plate boundaries: the Indian-Burmese plate boundary from the east and the Indian-Eurasian plate boundary from the north. During the 1897 Assam EQ (marked as 18 in Figure 2), GEOMATICS, NATURAL HAZARDS AND RISK many buildings were significantly damaged or destroyed in the Shillong city, and in Cherrapunji located in the East Khasi hills district. A deterministic (scenario-based) seismic hazard analysis (DSHA) is presented in this paper for three selected districts within SP – East Khasi hills, Ri-Bhoi, and West Garo hills – where the most populated cities – the Shillong city, Cherrapunji, Nongpoh, and Tura – are located. Numerous faults located within and around the SP have been identified, and a seismotectonic map of the SP has been developed by Baro and Kumar (2017) This map (Figure 2) covers major part of northeast India, portion of the eastern Himalayas, plains of Bengal and Bangladesh within a circle of 500 km radius with its center located at the geographical point (25.63N, 91.25E).

MCT Arun F95 Purnea F1–2 F3–4 F10–12 F13–14 F15–16 F5–6
Conclusion
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