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A 4,565-My-old andesite from an extinct chondritic protoplanet
The age of iron meteorites implies that accretion of protoplanets began during the first millions of years of the solar system. Due to the heat generated by (26)Al decay, many early protoplanets were fully differentiated with an igneous crust produced during the cooling of a magma ocean and the segr...
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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2021
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7980472/ https://ncbi.nlm.nih.gov/pubmed/33836612 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2026129118 |
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