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   <subfield code="a">Lapse time and frequency-dependent attenuation characteristics of coda waves in the Northwestern Himalayas</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[S. Mukhopadhyay, C. Tyagi]</subfield>
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   <subfield code="a">We analyzed the local earthquakes waveform recorded on a broadband seismic network in the northwestern Himalayan Region to compute lapse time and frequency dependence of coda Q (Q c). The observed Q c values increase with increasing lapse time at all frequency bands. The increase in Q c values with lapse time is attributed to an increase in Q c with depth. This implies that attenuation decreases with increasing depth. The approximate radius of medium contributing to coda generation varies from 55 to 130km. By comparing the Q c values with those from other regions of the world, we find that they are similar to those obtained from tectonically active regions. The estimated Q c values show a frequency-dependent relationship, Q c = Q 0 f n , where Q 0 is Q c at 1Hz and n represents degree of frequency dependence. They represent the level of heterogeneity and tectonic activity in an area. Our results show that northwest Himalayas are highly heterogeneous and tectonically very active. Q 0 increases from 113 ± 7 to 243 ± 10 and n decreases from 1.01 ± 0.05 to 0.85 ± 0.03 when lapse time increases from 30 to 70s. As larger time window sees the effect of deeper part of the Earth, it is concluded that Q 0 increases and n decreases with increasing depth; i.e., heterogeneity decreases with depth in the study area.</subfield>
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   <subfield code="a">lapse time</subfield>
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   <subfield code="a">attenuation characteristics</subfield>
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   <subfield code="a">Mukhopadhyay</subfield>
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   <subfield code="t">Journal of Seismology</subfield>
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