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- W2000596801 abstract "A structurally ordered cubic metal grain containing approximately 39 wt% Co, 61 wt% Fe, and less than 0.6 wt% Ni (approximately Fe3Co2) was found associated with troilite and pentlandite in the matrix of the Ningqiang carbonaceous chondrite. This mineral is similar to terrestrial wairauite. Experimental data in the Fe-Co system indicate that this CsCl-type Co-rich metal is stable below 700 C. Phase relations in the Fe-Co-Ni system show that Co cannot fractionate from Ni above 500 C. The dominant opaque minerals of awaruite, magnetite, and pentlandite in Ningqiang suggest relatively oxidizing conditions." @default.
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- W2000596801 date "1995-01-01" @default.
- W2000596801 modified "2023-09-22" @default.
- W2000596801 title "Cobalt-rich, nickel-poor metal (wairauite) in the Ningqiang carbonaceous chondrite" @default.
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- W2000596801 doi "https://doi.org/10.1111/j.1945-5100.1995.tb01217.x" @default.
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