Modeling Anisotropic Signature of Slab‐Induced Mantle Plumes From Thermochemical Piles in the Lowermost Mantle Article Swipe
Poulami Roy
,
Bernhard Steinberger
,
Manuele Faccenda
,
Michaël Pons
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1029/2024gl113299
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1029/2024gl113299
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 assumption that LLSVPs are thermochemical piles and resulting flow behavior using 3‐D regional‐scale mantle convection models in ASPECT, coupled with mantle fabric simulations in ECOMAN. We tested various models with different LLSVP density and viscosity. The modeling of the crystallographic‐preferred orientation with predominant activity of the slip system [001](100) for Bridgmanite and [100](001) for post‐Perovskite reveals that substantial seismic anisotropy develops in the lowermost mantle, and specifically (a) at the margins of the rheologically stiffer LLSVP piles where deformation and upwelling of the surrounding mantle take place and fast horizontally polarized shear waves ( V sh ) transition to fast V sv and (b) within plume roots and conduits where vertically polarized shear waves ( V sv ) are faster.
Related Topics
Concepts
Geology
Mantle (geology)
Plume
Slab
Transition zone
Mantle wedge
Geophysics
Mantle convection
Anisotropy
Mantle plume
Seismic anisotropy
Shear (geology)
Upwelling
Petrology
Seismology
Lithosphere
Tectonics
Thermodynamics
Physics
Quantum mechanics
Oceanography
Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1029/2024gl113299
- https://onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2024GL113299
- OA Status
- gold
- Cited By
- 1
- References
- 88
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4410755513
All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W4410755513Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1029/2024gl113299Digital Object Identifier
- Title
-
Modeling Anisotropic Signature of Slab‐Induced Mantle Plumes From Thermochemical Piles in the Lowermost MantleWork title
- Type
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articleOpenAlex work type
- Language
-
enPrimary language
- Publication year
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2025Year of publication
- Publication date
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2025-05-26Full publication date if available
- Authors
-
Poulami Roy, Bernhard Steinberger, Manuele Faccenda, Michaël PonsList of authors in order
- Landing page
-
https://doi.org/10.1029/2024gl113299Publisher landing page
- PDF URL
-
https://onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2024GL113299Direct link to full text PDF
- Open access
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YesWhether a free full text is available
- OA status
-
goldOpen access status per OpenAlex
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https://onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2024GL113299Direct OA link when available
- Concepts
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Geology, Mantle (geology), Plume, Slab, Transition zone, Mantle wedge, Geophysics, Mantle convection, Anisotropy, Mantle plume, Seismic anisotropy, Shear (geology), Upwelling, Petrology, Seismology, Lithosphere, Tectonics, Thermodynamics, Physics, Quantum mechanics, OceanographyTop concepts (fields/topics) attached by OpenAlex
- Cited by
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1Total citation count in OpenAlex
- Citations by year (recent)
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2025: 1Per-year citation counts (last 5 years)
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88Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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