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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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| Опубликовано в: : | Proc Natl Acad Sci U S A |
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| Главные авторы: | , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
National Academy of Sciences
2017
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| Предметы: | |
| Online-ссылка: | 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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