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Fluid and melt inclusions trapped in igneous rocks below the platinum-group element (PGE)-rich J-M reef in the Stillwater Complex, Montana provide a physiochemical record of a continuum of high P–T magmatic–hydrothermal and low P–T metamorphic events. Magmatic–hydrothermal volatiles ranged from NaCl-dominated halide melts (>82 wt % NaClequiv) to more complex Na–Ca–K–Fe–Mn–Ba–Si–Al–Cl brines (28–79...

Fluid and Halide Melt Inclusions of Magmatic Origin in the Ultramafic and Lower Banded Series, Stillwater Complex, Montana, USA