"Although there is a general tendency for high temperature magnetites to be high in titanium, this can by no means be used as a geological thermometer. Actually, the chemical composition of the ore-forming solutions influences, more directly and more radically, the titanium content of magnetites."
CITATION STYLE
Heier, K., & Buddington, A. F. (1956). Thermometric and petrogenetic significance of titaniferous magnetite; discussion and reply. American Journal of Science, 254(8), 506–515. https://doi.org/10.2475/ajs.254.8.506
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