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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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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Hyung, Eugenia, Jacobsen, Stein B.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2020
Assuntos:
Acesso em linha: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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