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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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Bibliografski detalji
Izdano u:Proc Natl Acad Sci U S A
Glavni autori: Hyung, Eugenia, Jacobsen, Stein B.
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2020
Teme:
Online pristup: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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