Low-velocity anomaly in the Coral Sea associated with subducting slabs and the Woodlark rift
Abstract Classical plume models offer insights into intraplate volcanism and seamount chain formation by assuming a cylindrical upwelling of hot materials from the core-mantle boundary. The interaction of mantle plumes with ridges or subducting slabs disrupts typical plate tectonics, leading to dist...
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| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-03-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-025-02166-8 |
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