Global geochemical fingerprinting of plume intensity suggests coupling with the supercontinent cycle
The links between plate tectonics and deep mantle structure remain unclear. Here, the authors demonstrate that transition elements (Ni, Cr, and Fe/Mn) in basaltic rocks can be used as a tool to trace plume-related magmatism through Earth history, and their results indicate the presence of a direct r...
Guardado en:
Autores principales: | Hamed Gamal EL Dien, Luc S. Doucet, Zheng-Xiang Li, Grant Cox, Ross Mitchell |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
|
Materias: | |
Acceso en línea: | https://doaj.org/article/1a347e4d867d4a32a0759d9fb84b3bbf |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Author Correction: Global geochemical fingerprinting of plume intensity suggests coupling with the supercontinent cycle
por: Hamed Gamal EL Dien, et al.
Publicado: (2020) -
Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation
por: Luc S. Doucet, et al.
Publicado: (2021) -
Geochemical constraints on the Hadean environment from mineral fingerprints of prokaryotes
por: Alexey A. Novoselov, et al.
Publicado: (2017) -
The evolution of basal mantle structure in response to supercontinent aggregation and dispersal
por: Xianzhi Cao, et al.
Publicado: (2021) -
Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
por: Crystal LaFlamme, et al.
Publicado: (2018)