Significance of Microchondrules of Olivine in Type I Carbonaceous Chondrites

Details Significance of Microchondrules of Olivine in Type I Carbonaceous Chondrites Significance of Microchondrules of Olivine in Type I Carbonaceous Chondrites

Jun 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968natur.218.1239m&link_type=abstract

Nature, Volume 218, Issue 5148, pp. 1239-1240 (1968).

Mathematics

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2

Scientific paper

THE identification of olivine1-3 in type I carbonaceous chondrites indicates their close genetical connexion with the rest of chondritic matter, which contains a high percentage of olivine. The discovery of interrelations between the ignition loss (IL) at 1,000° C in a nitrogen atmosphere and the statistical petrography of chondrules (ref. 4 and unpublished results) provides additional clues for the reconstruction of the cosmological history of chondrites.

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