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Seismic microzonation study in Doon valley, northwest Himalaya, India

  • Research Article
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Journal of the Geological Society of India

Abstract

Fundamental frequency map of site amplification at different sites in Doon valley, Uttarakhand, India is prepared from microtremor (ground ambient noise) using Horizontal to Vertical Spectral Ratio (HVSR) technique. The fan deposited alluvium filled synclinal valley of Doon lies between Main Boundary Thrust (MFT) and Himalayan Frontal Thrust (HFT) in the Himalayan active seismic belt and experienced many earthquakes in the past. The HVSR at different sites in the Doon valley ranges between the predominant frequencies 0.13 and 12.77 Hz. The HVSR in lower frequencies indicates that the site has either thick sediment covers or less compact rocks with fractures. Based on information on fundamental frequency and soft soil thickness, site classification map is generated. Results indicate that degree of compactness of rock types and presences of sediments vary significantly, which may play a major role in seismic hazard. The use of microtremor, therefore, constitutes an effective and inexpensive approach to site response and soft soil thickness estimation for preliminary microzonation.

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  1. Wadia Institute of Himalayan Geology, Dehradun, 248 001, India

    A. K. Mundepi

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Mundepi, A.K. Seismic microzonation study in Doon valley, northwest Himalaya, India. J Geol Soc India 81, 767–773 (2013). https://doi.org/10.1007/s12594-013-0101-z

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  • DOI: https://doi.org/10.1007/s12594-013-0101-z

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