Effects of fluid-induced oxidation on the composition of Fe–Ti oxides in the Eastern Gabbro, Coldwell Complex, Canada: implications for the application of Fe–Ti oxides to petrogenesis and mineral exploration
Magnetite (mag)–ilmenite (ilm) intergrowths are more common than mag–ulvöspinel (usp) intergrowths in mafic–ultramafic Ni–Cu–PGE systems, yet the former has no known solid solution. The most accepted model for the formation of mag–ilm intergrowths in terrestrial environments is fluid-induced oxidati...
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Veröffentlicht in: | Mineralium deposita 2021-03, Vol.56 (3), p.601-618 |
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Format: | Artikel |
Sprache: | eng |
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