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Estimating core-mantle boundary temperature from seismic shear velocity and attenuation

The temperature at Earth’s core-mantle boundary (CMB) is a key parameter to understand the dynamics of our planet’s interior. However, it remains poorly known, with current estimate ranging from about 3000 K to 4500 K and more. Here, we introduce a new approach based on joint measurements of seismic...

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Autors principals: Frédéric Deschamps, Laura Cobden
Format: Artigo
Idioma:Inglês
Publicat: Frontiers Media S.A. 2022-12-01
Col·lecció:Frontiers in Earth Science
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Accés en línia:https://www.frontiersin.org/articles/10.3389/feart.2022.1031507/full
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