A description of the meteorite which fell near Abee, Alberta, Canada

Mathematics – Logic

Scientific paper

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Scientific paper

id="ab1"The Abee meteorite, which fell at 54°13′N, 113°00′W, north of Edmonton, Alberta, on 9 June 1952, is described for the first time in this paper. The surface features and internal structures are those of a black polymict chondritic breccia. Chemical analyses have been made of the matrix and of the stony fragments, and these have been recalculated to give a mineralogical norm which corresponds with mineral identifications by X-ray diffraction. The stone consists mainly of enstatite and kamacitetaenite, with minor troilite, and accessory oldhamite, alabandite, α-cristobalite, and quartz. The metallurgical study of the nickel-iron of the meteorite indicates that relatively coarse grains of a kamacite-cohenite intergrowth resembling pearlite with marginal areas and islands of α-2-iron are the dominant phases present. Taenite is present only as an accessory constituent. The exterior of the fusion crust contains droplets of δ-iron and very fine-grained magnetite whereas the interior of the crust contains martensito grains produced by the heating and quenching of the kamacite.

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