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Potassium isotopic heterogeneity in subducting oceanic plates
Oceanic crust and sediments are the primary K sinks for seawater, and they deliver considerable amounts of K to the mantle via subduction. Historically, these crustal components were not studied for K isotopes because of the lack of analytical precision to differentiate terrestrial variations. Here,...
Tallennettuna:
| Julkaisussa: | Sci Adv |
|---|---|
| Päätekijät: | , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
American Association for the Advancement of Science
2020
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7821876/ https://ncbi.nlm.nih.gov/pubmed/33268367 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.abb2472 |
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