The Kyushu, Japan, chondrite

Details The Kyushu, Japan, chondrite The Kyushu, Japan, chondrite

Jan 1961

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1961gecoa..21..272m&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 21, Issue 3-4, p. 272-275.

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Scientific paper

The Kyushu chondrite has been analysed, with the following results: Fe 6·27, Ni 1·34, Co 0·046, FeS 5·89, SiO2 39·93, TiO2 0·14, Al2O3 1·86, Cr2O3 0·54, FeO 15·44, MnO 0·33, MgO 24·71, CaO 1·70, NaO 0·74, K2O 0·13, P2O5 0·31, H2O+0·27, C 0·03; total 99·67. The mineralogical composition is olivine (Fo74), hypersthene (En78), maskelynite, nickel-iron, troilite, chromite and possibly apatite. The density of the meteorite is 3·53.

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