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New implications for the origin of the IAB main group iron meteorites and the isotopic evolution of the noncarbonaceous (NC) reservoir
The origin of the IAB main group (MG) iron meteorites is explored through consideration of (182)W isotopic compositions, thermal modeling of (26)Al decay, and mass independent (nucleosynthetic) Mo isotopic compositions of planetesimals formed in the noncarbonaceous (NC) protosolar isotopic reservoir...
Gardado en:
| Publicado en: | Earth Planet Sci Lett |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
2020
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7709715/ https://ncbi.nlm.nih.gov/pubmed/33273744 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1016/j.epsl.2020.116248 |
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