In 1969, numerous fragments were found in a shallow depression during nickel exploration in Western Australia. They were not recognized as meteoritic until 1971, when a single large mass with ablation characteristics, along with smaller fragments totaling 24 kg, was found 400 m from the first find. Although originally described as petrologic type 5, all current research concludes that Yilmia is a type 6. The Van SchmusWood (1967) scheme for petrographic type has been modified for enstatite chondrites, establishing both a textural type (37), reflecting peak metamorphic temperature, and a mineralogical type (αδ), pertaining to the cooling history (Zhang and Sears, 1996; Quirico et al., 2011). Under this classification scheme, Yilmia has thermometers that indicate a classification of EL6β. A rapid cooling phase was initiated consistent with 30,000°C/day (Kissin, 1989).
Planetary-type noble gases, including Ar, Kr, and Xe, have been identified in Yilmia, the carrier of which is thought to be a nanometer-sized phase designated phase "Q" (for quintessence). Noble gases are adsorbed at low nebular pressures onto this phase, or precursors of this phase, likely consisting of rare graphite grains, kerogen, or carbon blacks. An alternate scenario, proposed by Matsuda et al. (2010), argues that an amorphous phase of carbon experienced implantation through ion irradiation of planetary noble gases (the "plasma model") and now constitutes the carrier of phase Q. These Q-gases are released through oxidation processes resulting in a rearrangement of the carbon structure.
The higher incidence of impact shock events for EL chondrites is attested by the higher prevalence of impact-melt breccias among the more metamorphosed members, as well as by the occurrence of abundant silica in the form of tridymite, cristobalite, and sinoite, the latter mineral known to crystallize from an impact melt. Following the impact-shock events, most EL6 chondrites experienced an extended period of annealing to shock stage S1, which was followed by a period of less severe impact-shock events resulting in a shock stage of S2 (Rubin et al., 2009).
While taenite is uncommon in other E chondrites, it is present in Yilmia. The photo above shows a 1.25 g partial slice of this terrestrially weathered, low-metal, enstatite chondrite.