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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...
| Autores principales: | , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2023
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| Materias: | |
| 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 |