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Magnesium isotope geochemistry of the carbonate-silicate system in subduction zones
The lighter magnesium (Mg) isotopic signatures observed in intraplate basalts are commonly thought to result from deep carbonate recycling, provided that the sharp difference in Mg isotopic composition between surface carbonates and the normal mantle is preserved during plate subduction. However, de...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Oxford University Press
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9166541/ https://www.ncbi.nlm.nih.gov/pubmed/35673532 http://dx.doi.org/10.1093/nsr/nwac036 |