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Accretion of the earliest inner Solar System planetesimals beyond the water snowline

Fe/Ni and Fe/Co ratios in iron meteorites indicate that the earliest inner Solar System planetesimals were oxidized and water-bearing, having formed beyond the point at which water condensed in the solar protoplanetary disk.

Damanveer S. Grewal
Nicole X. Nie
Paul D. Asimow
Research09 Jan 2024
Nature Astronomy

Volume: 8, P: 290-297
The UCLA Cosmochemistry Database

Bidong Zhang
Kerstin A. Lehnert
Juan D. Figueroa-Salazar
ResearchOpen Access07 Dec 2023
Scientific Data

Volume: 10, P: 1-6
A Global Building Occupant Behavior Database

Bing Dong
Yapan Liu
Xin Zhou
ResearchOpen Access28 Jun 2022
Scientific Data

Volume: 9, P: 1-15

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Accretion of the earliest inner Solar System planetesimals beyond the water snowline

The UCLA Cosmochemistry Database

A Global Building Occupant Behavior Database

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