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Shear-Wave Structure of the South Indian Lithosphere from Rayleigh Wave Phase-Velocity Measurements

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dc.contributor.author Mitra, S
dc.contributor.author Priestley, K
dc.contributor.author Gaur, V. K
dc.contributor.author Rai, S. S
dc.date.accessioned 2008-09-02T14:44:33Z
dc.date.available 2008-09-02T14:44:33Z
dc.date.issued 2006-08
dc.identifier.citation Bulletin of the Seismological Society of America; Vol. 96, No. 4A, pp. 1551 - 1559 en
dc.identifier.issn 0037-1106
dc.identifier.uri http://hdl.handle.net/2248/3333
dc.description.abstract We investigate the upper mantle shear-wave speed structure beneath the south Indian shield by measuring and modeling fundamental mode Rayleigh wave phase-velocity dispersion. Observed phase velocities for the south Indian shield closely match those observed for the Canadian shield. We constrain the south Indian crust using published receiver function results and invert the dispersion data for upper mantle shear-wave structure. The 155-km-thick seismic lithosphere of the south Indian shield is composed of a 35 km-thick, two-layer crust and a 120-km-thick, high-velocity upper mantle lid. Beneath the Moho the average Sn wave speed is 4.7 km sec–1. Both Sn travel times data and the dispersion data suggest a positive sub-Moho shear-wave speed gradient. Beneath the seismic lithosphere there is a low- velocity layer where the shear-wave speed drops to 4.4 km sec–1. en
dc.language.iso en en
dc.publisher The Seismological Society of America en
dc.relation.uri http://dx.doi.org/10.1785/0120050116 en
dc.subject Shear-Wave Speed Structure en
dc.subject Phase-Velocity Dispersion en
dc.title Shear-Wave Structure of the South Indian Lithosphere from Rayleigh Wave Phase-Velocity Measurements en
dc.type Article en


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