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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...

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Bibliografski detalji
Izdano u:Earth Planet Sci Lett
Glavni autori: Hilton, Connor D., Walker, Richard J.
Format: Artigo
Jezik:Inglês
Izdano: 2020
Teme:
Online pristup: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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