The Holbrook, Arizona, chondrite

Details The Holbrook, Arizona, chondrite The Holbrook, Arizona, chondrite

Jan 1961

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1961gecoa..21..276m&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 21, Issue 3-4, p. 276-283.

Mathematics

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Scientific paper

The Holbrook chondrite has been reanalysed, with the following results: Fe 7·18, Ni 1·09, Co 0·054, Cu 0·0096, FeS 7·94, SiO2 40·11, TiO2 0·14, Al2O3 1·90, Cr2O3 0·51, FeO 12·01, MnO 0·37, MgO 25·18, CaO 1·74, Na2O 0·93, K2O 0·10, P2O5 0·40, H2O 0·27, C 0·06 total 99·99. The mineralogical composition is olivine (Fo74), hypersthene (En76), plagioclase (An15), nickel-iron, troilite, chromite, and possibly apatite. The density of the meteorite is 3·56. A summary of the data on the abundances of Ba, Bi, Cs, Cu, In, Pb, Li, Hg, Rb, Se, Se, Sr, Te, Tl, Th, U, V, Y and Zr in this meteorite is included.

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