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Tracing magmatic–hydrothermal processes in IOCG systems: The Shabdiz iron deposit, Iran
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DOI：10.1016/j.gexplo.2026.108098.png)
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Abstract
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• First integrated field, petrography, chemistry & FI study of Shabdiz Fe deposit • Magnetite textures and TiVCoNiGa track evolving hydrothermal stages. • Fluid evolution from hot, low-fO2 magmatic to cooler oxidized basinal waters • NaCl- and CaCl2-rich inclusions indicate mixing of basin and magmatic fluids. • New IOCG genetic model for SSZ links redox-T to magnetite/sulfide deposition.
Keywords:
Iron mineralization
Magnetite
IOCG
SaSZ
Iran
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