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Mantle–slab interaction and redox mechanism of diamond formation
Subduction tectonics imposes an important role in the evolution of the interior of the Earth and its global carbon cycle; however, the mechanism of the mantle–slab interaction remains unclear. Here, we demonstrate the results of high-pressure redox-gradient experiments on the interactions between Mg...
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| Autori principali: | , , , , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2013
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3870714/ https://ncbi.nlm.nih.gov/pubmed/24297876 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1313340110 |
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