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Seismic Evidence for Partial Melt at the Base of Earth's Mantle

Williams, Quentin, Garnero, Edward J.·1996·Science

Abstract

The presence of an intermittent layer at the base of Earth's mantle with a maximum thickness near 40 kilometers and a compressional wave velocity depressed by ∼10 percent compared with that of the overlying mantle is most simply explained as the result of partial melt at this depth. Both the sharp upper boundary of this layer (<10 kilometers wide) and the apparent correlation with deep mantle upwelling are consistent with the presence of liquid in the lowermost mantle, implying that the bottom of the thermal boundary layer at the base of the mantle may lie above its eutectic temperature. Such a partially molten zone would be expected to have enhanced thermal and chemical transport properties and may provide constraints on the geotherm and lateral variations in lowermost mantle temperature or mineralogy.

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Metadata

Authors
Williams, Q., & Garnero, E. J.
Venue
Science
Published
1996-09-13
Volume
273
Issue
5281
Pages
1528-1530
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2075877487
Cited by
596
References
0
FWCI
21.61
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Seismic Evidence for Partial Melt at the Base of Earth's Mantle. https://app.cochat.ai/papers/10.1126/science.273.5281.1528
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Williams, Q., & Garnero, E. J. (1996). Seismic Evidence for Partial Melt at the Base of Earth's Mantle. Science. https://doi.org/10.1126/science.273.5281.1528

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.