Amoeboid olivine aggregates and related objects in carbonaceous chondrites: records of nebular and asteroid processes
By A. Krot, M. Petaev, S. Russell, S. Itoh, T. Fagan, H. Yurimoto, L. Chizmadia, M. Weisberg, M. Komatsu, A. A. Ul'yanov and 1 more. 2004
148 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atomic and Molecular Physics, and Optics, Geophysics
View Paper: https://www.semanticscholar.org/paper/4f51f1c2cd7689926ac481a92cd87b9ed7e4d530
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Citations in the corpus
- Redox Conditions in the Solar Nebula: Observational, Experimental, and Theoretical Constraints (2008, background): “The lowest XFa reported in AOAs in Acfer 094 is ~0.002 (Krot et al. 2004a).”
- The Effect of Jupiter's Formation on the Distribution of Refractory Elements and Inclusions in Meteorites (2017, background): “Explaining these CAIs and explaining the distribution of mass is why we choose a single CAI radius of 2.5 mm. AOAs: Chondrites also contain varying portions of another type of refractory inclusion, amoeboid olivine aggregates, or AOAs (Grossman & Steel 1976; Krot et al. 2004).”
- Chondrules and the Protoplanetary Disk (2011, background): “…1999); oxygen isotopic analysis of secondary fayalite, magnetite, and Ca-rich pyroxene (e.g., Choi et al. 2000); and thermodynamic analysis (Krot et al. 2004a, Fedkin & Grossman 2006) all indicate that asteroidal fluid-assisted metamorphism at temperatures above ∼200◦C was the cause of…”