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Coupled (182)W-(142)Nd constraint for early Earth differentiation
Recent high precision (142)Nd isotope measurements showed that global silicate differentiation may have occurred as early as 30–75 Myr after the Solar System formation [Bennett V, et al. (2007) Science 318:1907–1910]. This time scale is almost contemporaneous with Earth’s core formation at ∼30 Myr [...
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| Main Authors: | , , , , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
National Academy of Sciences
2010
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2890712/ https://ncbi.nlm.nih.gov/pubmed/20534492 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0913605107 |
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