Iron Isotope Constraints on the Structure of the Early Solar System
The recent advent of nontraditional isotopic systems has revealed that meteorites display a fundamental isotopic dichotomy between noncarbonaceous (NC) and carbonaceous (C) groups, which represent material from the inner and outer solar system, respectively. On the basis of iron isotope anomalies, t...
Main Authors: | Yves Marrocchi, Maxime Piralla, François L. H. Tissot |
---|---|
Format: | Article |
Language: | English |
Published: |
IOP Publishing
2023-01-01
|
Series: | The Astrophysical Journal Letters |
Subjects: | |
Online Access: | https://doi.org/10.3847/2041-8213/acefd1 |
Similar Items
-
Large Carbonaceous Chondrite Parent Bodies Favored by Abundance–Volatility Modeling: A Possible Chemical Signature of Pebble Accretion
by: Jeremy W. Boyce, et al.
Published: (2024-01-01) -
Cavitating Bubbles in Condensing Gas as a Means of Forming Clumps, Chondrites, and Planetesimals
by: E. Chiang
Published: (2024-01-01) -
Impact Disruption of Bjurböle Porous Chondritic Projectile
by: Tomas Kohout, et al.
Published: (2024-01-01) -
Oxygen Isotopic Variations in the Calcium, Aluminum-rich Inclusion–forming Region Recorded by a Single Refractory Inclusion from the CO3.1 Carbonaceous Chondrite Dar al Gani 083
by: Samuel Ebert, et al.
Published: (2024-01-01) -
Outgassing of chondritic planets
by: Bukvic, Dushan Stephen
Published: (2010)