The Tillaberi meteorite - A chondrite corresponding to hypersthene L6 containing a remarkable inclusion

Details The Tillaberi meteorite - A chondrite corresponding to hypersthene L6 containing a remarkable inclusion The Tillaberi meteorite - A chondrite corresponding to hypersthene L6 containing a remarkable inclusion

Sep 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976metic..11..217m&link_type=abstract

Meteoritics, vol. 11, Sept. 30, 1976, p. 217-224. In French.

Mathematics

Logic

Chemical Analysis, Chondrites, Meteoritic Composition, Mineralogy, Petrology, Chemical Composition, Chromites, Feldspars, Inclusions, Kamacite, Olivine

Scientific paper

The meteorite investigated fell in the Republic of Niger in April 1970. A sample of the meteorite which had been sent to Paris was found to contain a lithic inclusion. The inclusion contains feldspar, rounded grains of olivine, and minute crystals of chromite. The mineralogical characteristics observed can be explained by assuming that a brief intense heating of the meteorite was followed by rapid cooling

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