Flow rates and reaction rates in the Galapagos Rise spreading center hydrothermal system as inferred from (228)Ra/(226)Ra in vesicomyid clam shells
The (228)Ra/(226)Ra ratios in a previously dated vesicomyid clam shell were used to determine that seawater was in contact with mid-oceanic-ridge basalt glass for 22-45 years prior to arrival to the surface at 350°C at the Galapagos Rise Spreading Center. The minimum rate of reaction for the 45-year...
Збережено в:
| Опубліковано в:: | Proc Natl Acad Sci U S A |
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| Автори: | , |
| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
National Academy of Sciences
1986
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| Предмети: | |
| Онлайн доступ: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC386478/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16593746/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.83.17.6241 |
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