Basalts in the Lance carbonaceous chondrite

Details Basalts in the Lance carbonaceous chondrite Basalts in the Lance carbonaceous chondrite

Feb 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980znata..35..180k&link_type=abstract

Zeitschrift für Naturforschung, Teil a, vol. 35 a, Feb. 1980, p. 180-190.

Computer Science

10

Basalt, Carbonaceous Chondrites, Mineralogy, Petrology, Electron Microscopy, Melting, Meteoritic Microstructures, X Ray Analysis

Scientific paper

Three lithic fragments of the Lance carbonaceous chondrite which are thought to be of igneous origin and of basaltic parentage, consisting of large enstatite grains, are examined. Microprobe analyses are performed using an ARL-SEMQ automated electron microprobe, operating at 15kV acceleration potential and about 15nA sample current. Investigations indicate that: (1) the fragments are of igneous origin, and (2) the original melt was of basaltic composition, crystallizing the primary mineral association ol plus en plus plag plus low-Fe augite

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