“…Like those observations, the grains studied here consist of poorly crystallized graphite in intimate association with larger crystals of FeNi metal, in some cases with evidence for carbide at metal-C interfaces. These microstructures match those formed by catalytic reaction of C-bearing gases such as CO on metal surfaces to produce hydrocarbons, elemental carbon, and carbides (e.g., Fischer-Tropsch-type or FTT processes, Hindermann et al, 1993;Llorca and Casanova, 1998) and this appears to have played a role in forming the structures observed both in IDPs and in ordinary chondrites (Bradley et al, 1984;Brearley, 1990;Llorca and Casanova, 1998). The similarity of the graphite grains in the metalpoor lithology of GRA 95209 to these other materials indicates that they most likely formed by a similar process.…”