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The (142)Nd/(144)Nd variations in mantle-derived rocks provide constraints on the stirring rate of the mantle from the Hadean to the present
Early silicate differentiation events for the terrestrial planets can be traced with the short-lived (146)Sm-(142)Nd system (∼100-My half-life). Resulting early Earth-produced (142)Nd/(144)Nd variations are an excellent tracer of the rate of mantle mixing and thus a potential tracer of plate tectoni...
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| 出版年: | Proc Natl Acad Sci U S A |
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| 主要な著者: | , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2020
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7334517/ https://ncbi.nlm.nih.gov/pubmed/32541051 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2006950117 |
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