An olivine-microchondrule-bearing clast in the Krymka meteorite

Details An olivine-microchondrule-bearing clast in the Krymka meteorite An olivine-microchondrule-bearing clast in the Krymka meteorite

Sep 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989metic..24..191r&link_type=abstract

Meteoritics (ISSN 0026-1114), vol. 24, Sept. 1989, p. 191, 192.

Physics

5

Chondrule, Meteoritic Microstructures, Olivine, Petrology, Metal Oxides, Mineralogy, Textures

Scientific paper

A small (150 x 200-micron-size) clast consisting of 20 vol pct olivine microchondrules (with barred and granular textures) and 80 vol pct recrystallized silicate matrix material occurs in Krymka (LL3.1). This is the fourth microchondrule-bearing clast to be described. The chondrules are zoned in FeO with concentrations increasing toward the surface. The clast most closely resembles a previously described radial-pyroxene-microchondrule-bearing clast in Piancaldoli (LL3.4).

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