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Homogeneous accretion of the Earth in the inner Solar System PRIMARY_TEXT

Nature Astronomy · 2026-03-27 · no page hash: the reader saw a rendering, not the bytes · created seq 19941

Link: https://www.nature.com/articles/s41550-026-02824-7 · read at 2026-09-29T01:44:03Z · held by reference: only the link, the quoted excerpts with their hashes, and the page hash when the reader had the bytes are stored

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Excerpt	Finding
Here we examine variations in ten nucleosynthetic isotope anomalies among planets and meteorite parent bodies to show that the linear extension of an array d...	verbatim — the passage is on the page, character for character
The Earth therefore formed exclusively from inner Solar System material whose composition did not vary over the course of accretion and was, on average, unli...	verbatim — the passage is on the page, character for character
The isotopic compositions of ε100Ru and ε48Ca ... constrain fCI to below 0.3 ± 0.1% or <0.1−0.03+0.05%, respectively ... ε48Ca constrains fCI to below 2 ± 0....	not found — this server looked at the page and did not find the passage

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Locator	Excerpt
QUOTE `{}`	Here we examine variations in ten nucleosynthetic isotope anomalies among planets and meteorite parent bodies to show that the linear extension of an array defined by non-carbonaceous bodies in any two isotopic anomalies always intersect...
QUOTE `{}`	The Earth therefore formed exclusively from inner Solar System material whose composition did not vary over the course of accretion and was, on average, unlike that of any chondrite.
QUOTE `{}`	The isotopic compositions of ε100Ru and ε48Ca ... constrain fCI to below 0.3 ± 0.1% or <0.1−0.03+0.05%, respectively ... ε48Ca constrains fCI to below 2 ± 0.2% in the BSE and, as a refractory lithophile element, in the bulk Earth.

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