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Q C -estimates of Kachchh Basin in western India have been obtained in a high frequency range from 1.5 to 24.0 Hz using the aftershock data of Bhuj earthquake of January 26, 2001 recorded within an epicentral distance of 80 km. The decay of coda waves of 30 sec window from 186 seismograms has been analysed in four lapse time windows, adopting the single backscattering model. The study shows that Q c is a function of frequency and increases as frequency increases. The frequency dependent Q c relations obtained for four lapse-time windows are: Q c =82 f 1.17 (20-50 sec), Q c =106 f 1.11 (30-60 sec), Q c =126f 1.03 (40-70 sec) and Q c =122f 1.02 (50-80 sec). These empirical relations represent the average attenuation properties of a zone covering the surface area of about 11,000, 20,000, 28,000 and 38,000 square km and a depth extent of about 60, 80, 95, 110 km, respectively. With increasing window length, the degree of frequency dependence, n, decreases marginally from 1.17 to 1.02, whereas Q 0 increases significantly from 82 to 122. At lower frequencies up to 6 Hz, Q c )1 of Kachchh Basin is in agreement with other regions of the world, whereas at higher frequencies from 12 to 24 Hz it is found to be low. Figure 1 Map showing epicenters of aftershocks of Bhuj earthquake used in the Q c analysis, tectonic features in the Kachchh Basin and the locations of recording stations.

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A 1D velocity model of the Tehri region in the Garhwal Himalaya is estimated from the travel-time inversion of 145 well-located local events having 1177 P and 1090 S arrivals. The velocity model consists of six layers up to 24 km depth, with P-and S-wave velocities ranging from 4.42 to 6:78 km=s and 2.41 to 3:71 km=s, respectively. The depth of the Moho, estimated using travel-time curves of crustal phases, is about 46 km. A low-velocity layer deciphered between 12 and 14 km depths is ascribed to fractured basement thrust representing the upper surface of the Indian plate. Using the proposed velocity model, 1457 events are relocated. About 70% of the locatable events occur in the Inner Lesser Himalaya between the Main Central thrust (MCT) and the Srinagar thrust. The postulated depth of the basement thrust in the vicinity of the MCT is about 10-12 km. The depth distribution of events delineates the geometry of the seismically active Main Himalayan thrust (MHT) below a 300-km-long segment of the MCT. The MHT is composed of two shallow-dipping fracture zones that seem to represent seismically active thrust zones dipping in opposite directions. Two seismicity zones, at 10 and 15 km depths with a 5 km vertical separation, define a flat-ramp-flat type structure of the MHT in the vicinity of the MCT. The postulated front of the underthrusting Indian plate is at a depth of about 15-18 km. The lower-flat seismicity zone bifurcates into two, indicating further slicing of the lower-flat zone. The postulated thickness of the brittle part of the underthrusting Indian crust is about 20 km in the vicinity of the MCT.

A software (EQK_SRC_PARA) has been developed to estimate spectral parameters of earthquake source spectrum, namely: low frequency displacement spectral level (Ω 0 ), corner frequency above which spectrum decays with a rate of 2 (f c ), the cut-off frequency above which the spectrum again decays (f max ) and the rate of decay above f max (N). A Brune's source model [1,2] that yield a fall-off of 2 beyond corner frequency is considered with high cut-off frequency factor presented by Boore [3] that fits well for frequencies greater than f max . The software EQK_SRC_PARA is written in MATLAB and uses input data in Sesame ASCII Format (SAF) format. The obtained spectral parameters have been used to estimate source parameters (e.g., seismic moment, source dimension and stress drop etc.) and to develop scaling laws for the study region. The cut-off frequency "f max " can also be studied and interpreted to confirm about its origin.