Earth’s evolving geodynamic regime recorded by titanium isotopes

Earth’s mantle has a two-layered structure, with the upper and lower mantle domains separated by a seismic discontinuity at about 660 km (refs. (1,2)). The extent of mass transfer between these mantle domains throughout Earth’s history is, however, poorly understood. Continental crust extraction res...

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Detalles Bibliográficos
Autores principales: Deng, Zhengbin, Schiller, Martin, Jackson, Matthew G., Millet, Marc-Alban, Pan, Lu, Nikolajsen, Katrine, Saji, Nikitha S., Huang, Dongyang, Bizzarro, Martin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10482698/
https://www.ncbi.nlm.nih.gov/pubmed/37495699
http://dx.doi.org/10.1038/s41586-023-06304-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10482698/
https://www.ncbi.nlm.nih.gov/pubmed/37495699
http://dx.doi.org/10.1038/s41586-023-06304-0

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