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K isotopes as a tracer of seafloor hydrothermal alteration
At ocean spreading ridges, circulation of seawater through rock at elevated temperatures alters the chemical and isotopic composition of oceanic crust. Samples obtained from drilling into ocean floor and from ophiolites have demonstrated that certain isotope systems, such as (18)O/(16)O and (87)Sr/(...
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| Publicado no: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5338375/ https://ncbi.nlm.nih.gov/pubmed/28174267 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1609228114 |
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