Messengers from the deep: Fossil wadsleyite-chromite microstructures from the Mantle Transition Zone

Investigations of the Mantle Transition Zone (MTZ; 410–660 km deep) by deformation experiments and geophysical methods suggest that the MTZ has distinct rheological properties, but their exact cause is still unclear due to the lack of natural samples. Here we present the first direct evidence for cr...

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Detalles Bibliográficos
Autores principales: Satsukawa, Takako, Griffin, William L., Piazolo, Sandra, O’Reilly, Suzanne Y.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4643243/
https://www.ncbi.nlm.nih.gov/pubmed/26563583
http://dx.doi.org/10.1038/srep16484

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4643243/
https://www.ncbi.nlm.nih.gov/pubmed/26563583
http://dx.doi.org/10.1038/srep16484

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