Загрузка...
No significant boron in the hydrated mantle of most subducting slabs
Boron has become the principle proxy for the release of seawater-derived fluids into arc volcanics, linked to cross-arc variations in boron content and isotopic ratio. Because all ocean floor serpentinites so far analysed are strongly enriched in boron, it is generally assumed that if the uppermost...
Сохранить в:
| Опубликовано в: : | Nat Commun |
|---|---|
| Главные авторы: | , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group UK
2018
|
| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6214984/ https://ncbi.nlm.nih.gov/pubmed/30389930 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07064-6 |
| Метки: |
Добавить метку
Нет меток, Требуется 1-ая метка записи!
|