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Abstract
Ground motions are estimated at 55 sites in Delhi, the capital of India from four postulated earthquakes (three regional M ^sub w^â[euro][per thousand]=â[euro][per thousand]7.5, 8.0, and 8.5 and one local). The procedure consists of (1) synthesis of ground motion at a hard reference site (NDI) and (2) estimation of ground motion at other sites in the city via known transfer functions and application of the random vibration theory. This work provides a more extensive coverage than earlier studies (e.g., Singh et al., Bull Seism Soc Am 92:555â[euro]"569, 2002 ; Bansal et al., J Seismol 13:89â[euro]"105, 2009 ). The Indian code response spectra corresponding to Delhi (zone IV) are found to be conservative at hard soil sites for all postulated earthquakes but found to be deficient for M ^sub w^â[euro][per thousand]=â[euro][per thousand]8.0 and 8.5 earthquakes at soft soil sites. Spectral acceleration maps at four different natural periods are strongly influenced by the shallow geological and soil conditions. Three pockets of high acceleration values are seen. These pockets seem to coincide with the contacts of (a) Aravalli quartzite and recent Yamuna alluvium (towards the East), (b) Aravalli quartzite and older quaternary alluvium (towards the South), and (c) older quaternary alluvium and recent Yamuna alluvium (towards the North).[PUBLICATION ABSTRACT]