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Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif

The chemical compositions of the residues of the mantle melting that produces mid-ocean ridge basalt can be altered by fluid–rock interactions at spreading ridges and, possibly, during seawater penetration along bending-related faults in plates approaching trenches. This chemically modified rock, if...

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Detalles Bibliográficos
Autores principales: Ranaweera, Lalindra V., Ota, Tsutomu, Moriguti, Takuya, Tanaka, Ryoji, Nakamura, Eizo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6026181/
https://www.ncbi.nlm.nih.gov/pubmed/29959384
http://dx.doi.org/10.1038/s41598-018-28219-x

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