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Seismological mapping of fine structure near the base of the Earth's mantle

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Seismological mapping of fine structure near the base of the Earth's mantle; 1993; Article; Journal; Nature; Vidale, J. E.; Benz, H. M.

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THE Earth's core-mantle boundary (CMB) juxtaposes liquid iron and crystalline silicates, and is a region of large vertical thermal gradients. The D??? region, which extends up to 200-300 km above the CMB, often has elevated shear-wave velocity and suggestions of lateral variations in structure1. Recent improvements in our ability to assemble and analyse records from regional seismic networks have allowed us to examine long profiles of travel times, amplitudes and waveforms from more than a thousand short-period seismometers2. We observe, across Canada and the United States, P waves that have grazed the CMB from the powerful nuclear test in Lop Nor, China, on 21 May 1992. First-arrival travel times and large secondary arrivals are consistent [...]

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local-index unknown 70018380
local-pk unknown 70018380
series unknown Nature

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journalNature
parts
typevolume
value361
typeissue
value6412
languageEnglish
citationTypeArticle

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