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Korotev, Randy L. (1987) The nature of the meteoritic components of Apollo 16 soil, as inferred from correlations of iron, cobalt, iridium, and gold with nickel. Journal of Geophysical Research: Solid Earth, 92. doi:10.1029/jb092ib04p0e447

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Reference TypeJournal (article/letter/editorial)
TitleThe nature of the meteoritic components of Apollo 16 soil, as inferred from correlations of iron, cobalt, iridium, and gold with nickel
JournalJournal of Geophysical Research: Solid Earth
AuthorsKorotev, Randy L.Author
Year1987 (March 30)Volume92
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/jb092ib04p0e447Search in ResearchGate
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Mindat Ref. ID906103Long-form Identifiermindat:1:5:906103:7
GUID0
Full ReferenceKorotev, Randy L. (1987) The nature of the meteoritic components of Apollo 16 soil, as inferred from correlations of iron, cobalt, iridium, and gold with nickel. Journal of Geophysical Research: Solid Earth, 92. doi:10.1029/jb092ib04p0e447
Plain TextKorotev, Randy L. (1987) The nature of the meteoritic components of Apollo 16 soil, as inferred from correlations of iron, cobalt, iridium, and gold with nickel. Journal of Geophysical Research: Solid Earth, 92. doi:10.1029/jb092ib04p0e447
In(1987) Journal of Geophysical Research: Solid Earth Vol. 92. American Geophysical Union (AGU)


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