Computer Science
Scientific paper
Jul 1954
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1954gecoa...6...27c&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 6, Issue 1, pp.27-34
Computer Science
4
Scientific paper
Measurements of the magnetic constants of chemically analyzed titaniferous magnetites from the Skaergaard intrusion indicate that FeTiO 3 is completely exsolved as lalmenite lamellae. Up to about 6% Fe 2 TiO 4 , however, may remain in solid solution, the amount appearing to be more closely related to the temperature of consolidation of the rock than to the total Fe 2 TiO 4 content of the mineral. The magnetic measurements provide a completely independent estimate of the Fe 2 O 4 contents of the samples, which show good agreement with values calculated from chemical analyses. The coexisting ilmenites show little variation in magnetic properties; in particular there is no close relationship between magnetic properties and content of Fe 2 O 3 .
Chevallier Raymond
Mathieu Suzanne
Vincent E. A.
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