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Ultra-low-velocity anomaly inside the Pacific Slab near the 410-km discontinuity
The upper boundary of the mantle transition zone, known as the “410-km discontinuity”, is attributed to the phase transformation of the mineral olivine (α) to wadsleyite (β olivine). Here we present observations of triplicated P-waves from dense seismic arrays that constrain the structure of the sub...
| 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/PMC10155659/ https://www.ncbi.nlm.nih.gov/pubmed/37193082 http://dx.doi.org/10.1038/s43247-023-00756-y |