CORDIS Project
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This project explores the influence of volatile components in magmas on the formation of iron oxide deposits, particularly in low-Titanium systems. Through experimental studies, it aims to understand the processes that lead to the concentration of economically important elements in these geological formations.
The formation of magmatic iron oxide deposit is closely related to the role of volatiles in magmas, especially in low-Ti magmatic systems (Kiruna-type).
Volatiles have strong effect on phase equilibria, saturation of Fe-Ti oxides, and liquid immiscibility.
They also control the magmatic-hydrothermal transition with implications for the remobilization of some strategic elements (P, Au, Cu, REE) by fluids.
Volatiles are thus key components for the relation between Kiruna-type ores and Iron Oxides…
GOTTFRIED WILHELM LEIBNIZ UNIVERSITAET HANNOVER
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