Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1551-2020
https://doi.org/10.5194/se-11-1551-2020
Research article
 | 
26 Aug 2020
Research article |  | 26 Aug 2020

Increased density of large low-velocity provinces recovered by seismologically constrained gravity inversion

Wolfgang Szwillus, Jörg Ebbing, and Bernhard Steinberger

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Wolfgang Szwillus on behalf of the Authors (10 Jun 2020)
ED: Referee Nomination & Report Request started (26 Jun 2020) by Taras Gerya
RR by Anonymous Referee #1 (30 Jun 2020)
RR by Anonymous Referee #2 (02 Jul 2020)
ED: Publish as is (02 Jul 2020) by Taras Gerya
ED: Publish subject to technical corrections (03 Jul 2020) by Susanne Buiter (Executive editor)
AR by Wolfgang Szwillus on behalf of the Authors (10 Jul 2020)  Manuscript 
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Short summary
At the bottom of the mantle (2850 km depth) two large volumes of reduced seismic velocity exist underneath Africa and the Pacific. Their reduced velocity can be explained by an increased temperature or a different chemical composition. We use the gravity field to determine the density distribution inside the Earth's mantle and find that it favors a distinct chemical composition over a purely thermal cause.