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Cited by 211

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Superplumes from the Core-Mantle Boundary to the Lithosphere: Implications for Heat Flux

Romanowicz, Barbara, Gung, Yuancheng·2002·Science

Abstract

Three-dimensional modeling of upper-mantle anelastic structure reveals that thermal upwellings associated with the two superplumes, imaged by seismic elastic tomography at the base of the mantle, persist through the upper-mantle transition zone and are deflected horizontally beneath the lithosphere. This explains the unique transverse shear wave isotropy in the central Pacific. We infer that the two superplumes may play a major and stable role in supplying heat and horizontal flow to the low-viscosity asthenospheric channel, lubricating plate motions and feeding hot spots. We suggest that more heat may be carried through the core-mantle boundary than is accounted for by hot spot fluxes alone.

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Metadata

Authors
Romanowicz, B., & Gung, Y.
Venue
Science
Published
2002-04-19
Volume
296
Issue
5567
Pages
513-516
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1965567608
Cited by
211
References
1
FWCI
15.07
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Superplumes from the Core-Mantle Boundary to the Lithosphere: Implications for Heat Flux. https://app.cochat.ai/papers/10.1126/science.1069404
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Romanowicz, B., & Gung, Y. (2002). Superplumes from the Core-Mantle Boundary to the Lithosphere: Implications for Heat Flux. Science. https://doi.org/10.1126/science.1069404

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