CORDIS Project
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This project aims to improve the understanding of mantle convection by modeling the rheological properties of Earth's mantle phases. It employs multiscale modeling to link atomic-scale mechanisms to macroscopic behavior, focusing on key minerals.
Understanding mantle convection is essential to understand the thermal and chemical evolution of the Earth and to constrain the forces driving plate tectonics.
The rheological properties of the mantle are traditionally inverted from surface geophysical data.
Radial profiles of the viscosity are thus available but a lot of uncertainties remain.A more detailed model of mantle rheology could be obtained from the knowledge of the constitutive flow laws of mantle phases. A lot of progresses have been…
Partner organizations (coordinator is shown above), with normalized type and CORDIS activity type. Guests see up to 4 partners.
France, VILLENEUVE D'ASCQ
Type: University / higher education
Activity type: Higher or Secondary Education Establishments
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