Modeling Anisotropic Signature of Slab‐Induced Mantle Plumes From Thermochemical Piles in the Lowermost Mantle

Abstract Seismic anisotropy, observed in the lowermost mantle near Large Low‐Shear‐Velocity Provinces (LLSVPs), is likely caused by strong deformation from mantle flow interacting with these regions and/or plume formation. This study explores slab‐induced plume generation from LLSVPs under the assum...

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Bibliographic Details
Main Authors: Poulami Roy, Bernhard Steinberger, Manuele Faccenda, Michaël Pons
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2024GL113299
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