Formation of large low shear velocity provinces through the decomposition of oxidized mantle

Large Low Shear Velocity Provinces (LLSVPs) in the lowermost mantle are key to understanding the chemical composition and thermal structure of the deep Earth, but their origins have long been debated. Bridgmanite, the most abundant lower-mantle mineral, can incorporate extensive amounts of iron (Fe)...

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Detalles Bibliográficos
Autores principales: Wang, Wenzhong, Liu, Jiachao, Zhu, Feng, Li, Mingming, Dorfman, Susannah M., Li, Jie, Wu, Zhongqing
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7997914/
https://www.ncbi.nlm.nih.gov/pubmed/33771990
http://dx.doi.org/10.1038/s41467-021-22185-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7997914/
https://www.ncbi.nlm.nih.gov/pubmed/33771990
http://dx.doi.org/10.1038/s41467-021-22185-1

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