Global geochemical fingerprinting of plume intensity suggests coupling with the supercontinent cycle

Plate tectonics and mantle plumes are two of the most fundamental solid-Earth processes that have operated through much of Earth history. For the past 300 million years, mantle plumes are known to derive mostly from two large low shear velocity provinces (LLSVPs) above the core-mantle boundary, refe...

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Detalles Bibliográficos
Autores principales: Gamal EL Dien, Hamed, Doucet, Luc S., Li, Zheng-Xiang, Cox, Grant, Mitchell, Ross
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6872659/
https://www.ncbi.nlm.nih.gov/pubmed/31754134
http://dx.doi.org/10.1038/s41467-019-13300-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6872659/
https://www.ncbi.nlm.nih.gov/pubmed/31754134
http://dx.doi.org/10.1038/s41467-019-13300-4

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