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The Shatsky Rise oceanic plateau formed through plume–ridge interaction
(2023). The Shatsky Rise oceanic plateau formed through plume–ridge interaction. Nature Geoscience 16(11): 944-945. https://dx.doi.org/10.1038/s41561-023-01289-x
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, meer
Is gerelateerd aan:
Zhang, X.; Brown, E.L.; Zhang, J.; Lin, J.; Bao, X.; Sager, W.W. (2023). Magmatism of Shatsky Rise controlled by plume–ridge interaction. Nature Geoscience 16(11): 1061-1069. https://dx.doi.org/10.1038/s41561-023-01286-0, meer
Peer reviewed article  
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Abstract
    There are two competing hypotheses for the origin of oceanic plateaus: plume versus plate. Thermodynamic modelling of magmatism at Shatsky Rise, in the Pacific Ocean, now suggests that neither mechanism is adequate on its own and in fact plume–ridge interaction is required to explain the formation of this ocean plateau.
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