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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...

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Detalles Bibliográficos
Autores principales:	Borgeaud, Anselme F. E., Kawai, Kenji, Konishi, Kensuke, Geller, Robert J.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	American Association for the Advancement of Science 2017
Materias:	Research Articles
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

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