Fat Plumes May Reflect the Complex Rheology of the Lower Mantle

Abstract Recent tomographic imaging of the mantle below major hot spots shows slow seismic velocities extending down to the core‐mantle boundary, confirming the existence of mantle plumes. However, these plumes are much thicker than previously thought. Using new laboratory experiments and scaling la...

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Main Authors: A. Davaille, Ph. Carrez, P. Cordier
Format: Article
Language:English
Published: Wiley 2018-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2017GL076575
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author A. Davaille
Ph. Carrez
P. Cordier
author_facet A. Davaille
Ph. Carrez
P. Cordier
author_sort A. Davaille
collection DOAJ
description Abstract Recent tomographic imaging of the mantle below major hot spots shows slow seismic velocities extending down to the core‐mantle boundary, confirming the existence of mantle plumes. However, these plumes are much thicker than previously thought. Using new laboratory experiments and scaling laws, we show that thermal plumes developing in a visco‐plastic fluid present much larger diameters than plumes developing in a Newtonian fluid. Such a rheology requiring a yield stress is consistent with a lower mantle predominantly deforming by pure dislocation climb. Yield stress values between 1 and 10 MPa, implying dislocation densities between 108 and 1010 m−2, would be sufficient to reproduce the plumes morphology observed in tomographic images.
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series Geophysical Research Letters
spelling doaj-art-e81c2e0d44e54263a2bfff2f455293b02025-08-20T03:09:42ZengWileyGeophysical Research Letters0094-82761944-80072018-02-014531349135410.1002/2017GL076575Fat Plumes May Reflect the Complex Rheology of the Lower MantleA. Davaille0Ph. Carrez1P. Cordier2Laboratoire FAST CNRS/University of Paris‐Sud/University of Paris‐Saclay Orsay FranceUniversity of Lille, INRA, ENSCL, UMR 8207‐UMET‐Unite Materiaux et Transformations Lille FranceUniversity of Lille, INRA, ENSCL, UMR 8207‐UMET‐Unite Materiaux et Transformations Lille FranceAbstract Recent tomographic imaging of the mantle below major hot spots shows slow seismic velocities extending down to the core‐mantle boundary, confirming the existence of mantle plumes. However, these plumes are much thicker than previously thought. Using new laboratory experiments and scaling laws, we show that thermal plumes developing in a visco‐plastic fluid present much larger diameters than plumes developing in a Newtonian fluid. Such a rheology requiring a yield stress is consistent with a lower mantle predominantly deforming by pure dislocation climb. Yield stress values between 1 and 10 MPa, implying dislocation densities between 108 and 1010 m−2, would be sufficient to reproduce the plumes morphology observed in tomographic images.https://doi.org/10.1002/2017GL076575Mantle plumesnon‐Newtonian rheologydislocation climblower mantle convectiontomography imageslaboratory experiments
spellingShingle A. Davaille
Ph. Carrez
P. Cordier
Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
Geophysical Research Letters
Mantle plumes
non‐Newtonian rheology
dislocation climb
lower mantle convection
tomography images
laboratory experiments
title Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
title_full Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
title_fullStr Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
title_full_unstemmed Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
title_short Fat Plumes May Reflect the Complex Rheology of the Lower Mantle
title_sort fat plumes may reflect the complex rheology of the lower mantle
topic Mantle plumes
non‐Newtonian rheology
dislocation climb
lower mantle convection
tomography images
laboratory experiments
url https://doi.org/10.1002/2017GL076575
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