Foreign inclusions in stony meteorites--I. Carbonaceous chondritic xenoliths in the Kapoeta howardite

Details Foreign inclusions in stony meteorites--I. Carbonaceous chondritic xenoliths in the Kapoeta howardite Foreign inclusions in stony meteorites--I. Carbonaceous chondritic xenoliths in the Kapoeta howardite

Aug 1973

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1973gecoa..37.1985w&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 37, Issue 8, pp.1985-1986

Physics

16

Scientific paper

Small, 1-3 millimeter-sized, black xenoliths containing chondrules and
chondrule fragments embedded in a fine-grained matrix are present in the
Kapoeta howardite. Forsteritic olivine, pentlandite and a nickel-rich
(0.3-2.8 wt. %) matrix indicate that these xenoliths are carbonaceous
ohondrite material.

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