Dr. Alan Rubin, UCLA, has analyzed the West, TX meteorite as an L6 chondrite:
W0, S3, L6 olivine
Fa: 24.2±0.2 (n=12)low-Ca pyx Fs20.5±0.7 Wo1.6±0.2 (n=12)
kamacite has an average composition of Fe 93.1 Ni 5.8 Co 0.83 (n=4) taenite has an average composition of Fe 69.6 Ni 30.3 Co 0.30 (n=9) Taenite is much more abundant than kamacite. Many plagioclase grains exceed 50 µm in size. Some metal grains have irregular grains of troilite inside them. Metallic Cu is present in metal grains. There are some thin metal- and sulfide-bearing shock veins. The rock exhibits signficant silicate darkening.
The "Ash Creek" (Doug Dawn`s proposed name for the meteorite) meteorite sample was collected by Doug Dawn, Dima, Rob McCafferty, and Sergey and sent to Dr. Rubin for analysis.
The data from Dr. Rubin`s classification analysis will be sent to the Meteorite NOMCOM for approval and a final naming will be approved.
Record timing for meteorite recovery and analysis; congratulations to all that worked on this!!!
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