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Seismic and gravity constraints on plate flexure and mantle rheology along the whole Hawaiian-Emperor seamount chain

Abstract:
The Hawaiian-Emperor seamount chain is a hotspot-generated intraplate volcanic chain that has yielded key constraints on the rigidity of Earth’s tectonic plates. However, previous studies have shown significant variability in the effective elastic thickness, Te, a proxy for the long-term strength of the lithosphere, along the chain. While low Te (10-20 km) at the Emperor Seamounts and high Te (17-37 km) at the Hawaiian Ridge are expected because of their differences in volcano and plate age, the change between them appears abrupt and occurs in the vicinity of the bend in the chain. To investigate this variability, we estimated Te along 3000 profiles - spaced 2 km apart along the chain - from gravity and flexure modeling, and calibrated using constraints from deep seismic experiments carried out in 2018 and 2019. Here we show that, contrary to previous predictions, Te changes gradually along the chain and that weak zones can exist within the interior of a large, otherwise rigid, plate and may, we speculate, facilitate the initiation of intra-oceanic subduction in response, for example, to changes in plate motion and eventually lead to their break-up.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41467-025-65442-3

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


Publisher:
Springer Nature
Journal:
Nature Communications More from this journal
Volume:
16
Issue:
1
Article number:
11013
Publication date:
2025-12-02
Acceptance date:
2025-10-14
DOI:
EISSN:
2041-1723


Language:
English
Keywords:
Pubs id:
2299842
Local pid:
pubs:2299842
Deposit date:
2025-10-15
ARK identifier:

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