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Attenuation studies based on local earthquake Coda waves in the southern Indian peninsular shield

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Abstract

The Dharwar craton, Cuddapah basin and the Godavari graben characterise three diverse geological and tectonic settings in the peninsular shield of India. Owing to their contiguous proximity, they offer a unique opportunity to document differences, if any, in their seismic wave attenuation characteristics that might have a bearing on the seismogenic nature of the crust in a craton, basin and a rift-like graben structure. An attempt is made here to bring out these differences using constraints from coda-Q. We considered local earthquakes with epicentral distances ranging from␣14 to 150 km recorded at the digital broadband stations at Dharwar (DHD), Cuddapah (CUD) and Kothagudem (KGD) regions to derive the frequency-dependent coda-Q relations. Using the single scattering method, we obtained the frequency-dependent Q C relationship (Q C = Q 0 f n)for each of the three geological units separately: DHD: Q C = (730.62 ± 0.09)f (0.54 ± 0.01); CUD: Q C = (535.06 ± 0.13)f (0.59 ± 0.01) and KGD: Q C = (150.56 ± 0.08)f(0.91 ± 0.01). The Q C values obtained for all the three sub-regions show moderate to strong frequency dependence and essentially reflect the level of crustal heterogeneities to varying degrees.

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Acknowledegment

The authors are grateful to the Director, NGRI for his kind permission to publish this work.

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Correspondence to C. H. Patanjali Kumar.

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Kumar, C.P., Sarma, C.S.P., Shekar, M. et al. Attenuation studies based on local earthquake Coda waves in the southern Indian peninsular shield. Nat Hazards 40, 527–536 (2007). https://doi.org/10.1007/s11069-006-9017-x

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  • DOI: https://doi.org/10.1007/s11069-006-9017-x

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