A correlation between ultra-low basal velocities in the mantle and hot spots

Q. Williams, J. Revenaugh, Edward Garnero

Research output: Contribution to journalArticle

130 Citations (Scopus)

Abstract

The statitical correlation between the locations of hot spots at the surface at Earth and the distribution of ultra-low-velocity zones at the base of the mantle has about a 1 percent chance of arising randomly. This correlation is more significant than that between hot spots and negative velocity anomalies in tomographic models of deep mantle compressional and shear velocity. This correlation is consistent with the notion that many hot spots originate in a low-velocity, probably partially molten layer at the core-mantle boundary and undergo little lateral deflection on ascent.

Original languageEnglish (US)
Pages (from-to)546-549
Number of pages4
JournalScience
Volume281
Issue number5376
DOIs
StatePublished - Jul 24 1998
Externally publishedYes

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mantle
low velocity zone
core-mantle boundary
deflection
anomaly
distribution

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Cite this

A correlation between ultra-low basal velocities in the mantle and hot spots. / Williams, Q.; Revenaugh, J.; Garnero, Edward.

In: Science, Vol. 281, No. 5376, 24.07.1998, p. 546-549.

Research output: Contribution to journalArticle

Williams, Q. ; Revenaugh, J. ; Garnero, Edward. / A correlation between ultra-low basal velocities in the mantle and hot spots. In: Science. 1998 ; Vol. 281, No. 5376. pp. 546-549.
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