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I–Xe systematics of the impact plume produced chondrules from the CB carbonaceous chondrites: Implications for the half-life value of (129)I and absolute age normalization of (129)I–(129)Xe chronometer
It is inferred that magnesian non-porphyritic chondrules in the CB (Bencubbin-type) carbonaceous chondrites formed in an impact generated plume of gas and melt at 4562.49 ± 0.21 Ma (Bollard et al., 2015) and could be suitable for the absolute age normalization of relative chronometers. Here xenon is...
Guardat en:
| Publicat a: | Geochim Cosmochim Acta |
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| Autors principals: | , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
2016
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5688312/ https://ncbi.nlm.nih.gov/pubmed/29151614 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1016/j.gca.2016.01.012 |
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