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- W2093794703 abstract "Abstract— We describe a previously unreported meteorite found in Axtell, Texas, in 1943. Based on the mineralogical composition and texture of its matrix and the sizes and abundance of chondrules, we classify it as a CV3 carbonaceous chondrite. The dominant opaque phase in the chondrules is magnetite, and that in refractory inclusions is Ni-rich NiFe metal (awaruite). Axtell, therefore, belongs to the oxidized subgroup of CV3 chondrites, although unlike Allende it escaped strong sulfidation. The meteorite bears a strong textural resemblance to Allende, and its chondrule population and matrix appear to be quite similar to those of Allende, but its refractory inclusions, thermoluminescence properties, and cosmogenic 60Co abundances are not. Our data are consistent with a terrestrial age for Axtell of ∼100 years and a metamorphic grade slightly lower than that of Allende." @default.
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- W2093794703 date "1995-01-01" @default.
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- W2093794703 title "Axtell, a new CV3 chondrite find from Texas" @default.
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- W2093794703 doi "https://doi.org/10.1111/j.1945-5100.1995.tb01210.x" @default.
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