Spurious low velocity zones in joint inversions of surface waves and receiver functions
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DOI: 10.1093/gji/ggz345
Abstract: Low-velocity layers within the crust can indicate the presence of melt and lithologic differences with implications for crustal composition and formation. Seismic wave conversions and reverberations across the base of the crust or intracrustal discontinuities,… read more here.
Keywords: low velocity; velocity; receiver functions; spurious low ... See more keywords