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Imaging paleoslabs in the D″ layer beneath Central America and the Caribbean using seismic waveform inversion
D″ (Dee double prime), the lowermost layer of the Earth’s mantle, is the thermal boundary layer (TBL) of mantle convection immediately above the Earth’s liquid outer core. As the origin of upwelling of hot material and the destination of paleoslabs (downwelling cold slab remnants), D″ plays a major...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5710186/ https://www.ncbi.nlm.nih.gov/pubmed/29209659 http://dx.doi.org/10.1126/sciadv.1602700 |