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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...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| 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 |