Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/3333
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dc.contributor.authorMitra, S-
dc.contributor.authorPriestley, K-
dc.contributor.authorGaur, V. K-
dc.contributor.authorRai, S. S-
dc.date.accessioned2008-09-02T14:44:33Z-
dc.date.available2008-09-02T14:44:33Z-
dc.date.issued2006-08-
dc.identifier.citationBulletin of the Seismological Society of America; Vol. 96, No. 4A, pp. 1551 - 1559en
dc.identifier.issn0037-1106-
dc.identifier.urihttp://hdl.handle.net/2248/3333-
dc.description.abstractWe 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.isoenen
dc.publisherThe Seismological Society of Americaen
dc.relation.urihttp://dx.doi.org/10.1785/0120050116en
dc.subjectShear-Wave Speed Structureen
dc.subjectPhase-Velocity Dispersionen
dc.titleShear-Wave Structure of the South Indian Lithosphere from Rayleigh Wave Phase-Velocity Measurementsen
dc.typeArticleen
Appears in Collections:IIAP Publications

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