Cargando…
Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
The Ontong Java and Manihiki oceanic plateaus are believed to have formed through high-degree melting of a mantle plume head. Boninite-like, low-Ti basement rocks at Manihiki, however, imply a more complex magma genesis compared with Ontong Java basement lavas that can be generated by ∼30% melting o...
Autores principales: | Golowin, Roman, Portnyagin, Maxim, Hoernle, Kaj, Hauff, Folkmar, Gurenko, Andrey, Garbe-Schönberg, Dieter, Werner, Reinhard, Turner, Simon |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2017
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5309764/ https://www.ncbi.nlm.nih.gov/pubmed/28181497 http://dx.doi.org/10.1038/ncomms14322 |
Ejemplares similares
-
How and when plume zonation appeared during the 132 Myr evolution of the Tristan Hotspot
por: Hoernle, Kaj, et al.
Publicado: (2015) -
Evidence for compositionally distinct upper mantle plumelets since the early history of the Tristan-Gough hotspot
por: Homrighausen, Stephan, et al.
Publicado: (2023) -
Interrelation of the stagnant slab, Ontong Java Plateau, and intraplate volcanism as inferred from seismic tomography
por: Obayashi, Masayuki, et al.
Publicado: (2021) -
Boron isotopes in boninites document rapid changes in slab inputs during subduction initiation
por: Li, Hong-Yan, et al.
Publicado: (2022) -
Intraplate volcanism triggered by bursts in slab flux
por: Mather, Ben R., et al.
Publicado: (2020)