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Condensation Time of the Solar Nebula from Extinct (129)I in Primitive Meteorites
Mineral separates from five carbonaceous chondrites were dated by extinct 16 million year (129)I, in an attempt to establish the condensation time of the solar nebula. Two Fe(3)O(4) or Fe(3)O(4)-FeS samples from the Murchison and Orgueil meteorites are older than any other material dated thus far, a...
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| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
1975
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC432285/ https://ncbi.nlm.nih.gov/pubmed/16592213 |
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