Abstract
The chrome spinels vary in composition depending on their occurrences in olivine, plagioclase and glass. The variations result from changes of melt composition during crystallization and competition between olivine and plagioclase with spinels for Al and Mg.-K.A.R.
Cite
CITATION STYLE
APA
Furuta, T., & Tokuyama, H. (1983). Chromian spinels in Costa Rica basalts, Deep Sea Drilling Project site 505 - a preliminary interpretation of electron microprobe analyses. Initial Reports of the D.S.D.P., 69, 805–810. https://doi.org/10.2973/dsdp.proc.69.153.1983
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