Water Reservoirs in the Lower Mantle Beneath Northeastern Asia

Abstract Water in the mantle controls mantle convection and chemical transport processes within Earth's interior. However, whether the water in the lower mantle is primordial or recycled remains an open question. Here we report an electrical structure consisting of two stepped high‐conductivity anomalies crossing the 660‐km interface beneath northeastern Asia. The sheet‐like first‐step conductor locates in the mantle transition zone that can be best interpreted as hydrated stagnant Pacific slab, whereas the funnel‐like second‐step anomaly occurs in the uppermost lower mantle that is inferred to be a water reservoir replenished by the collapsed stagnant slab. The pivotal mechanism of this water transport process could be the dehydration reaction of dense hydrous magnesium silicates and the rehydration of stishovite and liebermannite in the transition zone. Our findings provide evidence for recycled lower‐mantle water reservoirs, and together with seismological and mineralogical studies, illustrate the deep‐mantle water plumbing system operated by cold slab subduction.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-04-11
DOI
https://doi.org/10.1029/2024gl114180
Citations
3
Primary Topic
Geological and Geophysical Studies
Type
article
Field-Weighted Citation Impact
7.04

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article

Water Reservoirs in the Lower Mantle Beneath Northeastern Asia

Yanhui Zhang, Geeth Manthilake, Aihua Weng, Junhao Guo et al.
3 citations
Geophysical Research Letters
Geological and Geophysical Studies
7.04
article

Water Reservoirs in the Lower Mantle Beneath Northeastern Asia

Yanhui Zhang, Geeth Manthilake, Aihua Weng, Junhao Guo, Shiwen Li, Zikun Zhou, Wen‐Liang Xu, Yabin Li
article en
3 citations

Abstract

Abstract Water in the mantle controls mantle convection and chemical transport processes within Earth's interior. However, whether the water in the lower mantle is primordial or recycled remains an open question. Here we report an electrical structure consisting of two stepped high‐conductivity anomalies crossing the 660‐km interface beneath northeastern Asia. The sheet‐like first‐step conductor locates in the mantle transition zone that can be best interpreted as hydrated stagnant Pacific slab, whereas the funnel‐like second‐step anomaly occurs in the uppermost lower mantle that is inferred to be a water reservoir replenished by the collapsed stagnant slab. The pivotal mechanism of this water transport process could be the dehydration reaction of dense hydrous magnesium silicates and the rehydration of stishovite and liebermannite in the transition zone. Our findings provide evidence for recycled lower‐mantle water reservoirs, and together with seismological and mineralogical studies, illustrate the deep‐mantle water plumbing system operated by cold slab subduction.

Geophysical Research LettersVol. 52(8)
Centre National de la Recherche Scientifique (FR), Jilin University (CN), Université Clermont Auvergne (FR), Observatoire de Physique du Globe de Clermont-Ferrand (FR), Laboratoire Magmas et Volcans (FR), Jilin Province Science and Technology Department (CN), Institut de Recherche pour le Développement (FR), Shijiazhuang Tiedao University (CN)
National Natural Science Foundation of China, Chinese Academy of Sciences, Jilin University, Istituto Nazionale di Geofisica e Vulcanologia, U.S. Geological Survey, Program for Jilin University Science and Technology Innovative Research Team, Institute of Geochemistry, Chinese Academy of Sciences
Openalex Percentile: Top 4%
Geological and Geophysical Studies
7.04
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