Constraints on planetesimal accretion inferred from particle-size distribution in CO chondrites
Gabriel A. Pinto, Yves Marrocchi, Alessandro Morbidelli, S\'ebastien, Charnoz, Maria Eugenia Varela, Kevin Soto, Rodrigo Mart\'inez, Felipe, Olivares

TL;DR
This study analyzes particle-size distributions in CO chondrites to infer that planetesimals likely formed through gravitational collapse, with aerodynamic sorting during accretion influencing chondrule sizes.
Contribution
It provides evidence supporting gravitational collapse as the formation mechanism for planetesimals, based on particle-size distribution analysis and modeling of chondrule sorting.
Findings
Chondrule sizes increase with petrographic grade, indicating thermal metamorphism effects.
Aerodynamic sorting during accretion influenced chondrule distribution within parent bodies.
Modeling shows larger chondrules are more centrally concentrated, supporting gravitational collapse formation.
Abstract
The formation of planetesimals was a key step in the assemblage of planetary bodies, yet many aspects of their formation remain poorly constrained. Notably, the mechanism by which chondrules -- sub-millimetric spheroids that dominate primitive meteorites -- were incorporated into planetesimals remains poorly understood. Here we classify and analyze particle-size distributions in various CO carbonaceous chondrites found in the Atacama Desert. Our results show that the average circle-equivalent diameters of chondrules define a positive trend with the petrographic grade, which reflects the progressive role of thermal metamorphism within the CO parent body. We show that this relationship could not have been established by thermal metamorphism alone but rather by aerodynamic sorting during accretion. By modeling the self-gravitational contraction of clumps of chondrules, we show that (i) the…
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