Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere

Decompressional melting of asthenosphere under spreading centers has been accepted to produce oceanic lithospheric mantle with vertical compositional variations, but these gradients are much smaller than those observed from ophiolites, which clearly require additional causes. Here we conduct high-de...

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Detalles Bibliográficos
Autores principales: Xiong, Qing, Dai, Hong-Kun, Zheng, Jian-Ping, Griffin, William L., Zheng, Hong-Da, Wang, Li, Reilly, Suzanne Y. O’
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9663536/
https://www.ncbi.nlm.nih.gov/pubmed/36376287
http://dx.doi.org/10.1038/s41467-022-34781-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9663536/
https://www.ncbi.nlm.nih.gov/pubmed/36376287
http://dx.doi.org/10.1038/s41467-022-34781-w

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