Are some chondrule rims formed by impact processes? - Observations and experiments

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Chondrule, Hypervelocity Impact, Meteorite Craters, Meteoritic Microstructures, Regolith, Olivine, Petrography, Pyroxenes, Solar System Evolution

Scientific paper

The ability of high-speed impacts into a parent body regolith to account for the textures and compositions observed for rims on some chondrules is presently supported by both observational and experimental data. Experimental results obtained with a light-gas gun encompass recovered-grain characteristics ranging from fragmented projectile grains mixed with melted aerogel, demonstrating that rim-like thermal and mechanical alterations of projectiles may be due to a high-velocity encounter with a low density target. Irrespective of conclusions for other types of rims, granular and opaque rim characteristics seem inconsistent with nebular condensation.

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