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Heavy oxygen recycled into the lithospheric mantle
Magmas in volcanic arcs have geochemical and isotopic signatures that can be related to mantle metasomatism due to fluids and melts released by the down-going oceanic crust and overlying sediments, which modify the chemistry and mineralogy of the mantle wedge. However, the effectiveness of subductio...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6584624/ https://ncbi.nlm.nih.gov/pubmed/31217538 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-45031-3 |
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