Uranium Transport in F-Cl-Bearing Fluids and Hydrothermal Upgrading of U-Cu Ores in IOCG Deposits

<div>Equilibrium constants for the hydrolysis of UO<sub>2</sub>OH<sup>+</sup> and UO<sub>2</sub>(OH)<sub>2</sub>(aq).</div>

Geofluids

Figure 6: Uranium Transport in F-Cl-Bearing Fluids and Hydrothermal Upgrading of U-Cu Ores in IOCG Deposits 