Solid Earth
Solid Earth
SE
Articles | Volume 12, issue 2
Articles | Volume 12, issue 2
https://doi.org/10.5194/se-12-421-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-421-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 12, issue 2
Research article
 | 
22 Feb 2021
Research article |  | 22 Feb 2021

Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans

Daniela Paz Bolrão, Maxim D. Ballmer, Adrien Morison, Antoine B. Rozel, Patrick Sanan, Stéphane Labrosse, and Paul J. Tackley

Viewed

Total article views: 3,827 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,657 1,033 137 3,827 154 209
  • HTML: 2,657
  • PDF: 1,033
  • XML: 137
  • Total: 3,827
  • BibTeX: 154
  • EndNote: 209
Views and downloads (calculated since 17 Apr 2020)
Cumulative views and downloads (calculated since 17 Apr 2020)

Viewed (geographical distribution)

Total article views: 3,827 (including HTML, PDF, and XML) Thereof 3,478 with geography defined and 349 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 11 May 2026
Download
Short summary
We use numerical models to investigate the thermo-chemical evolution of a solid mantle during a magma ocean stage. When applied to the Earth, our study shows that the solid mantle and a magma ocean tend toward chemical equilibration before crystallisation of this magma ocean. Our findings suggest that a very strong chemical stratification of the solid mantle is unlikely to occur (as predicted by previous studies), which may explain why the Earth’s mantle is rather homogeneous in composition.
Read more
Share