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Sulphide mineral reactions in clay-rich rock induced by high hydrogen pressure. Application to disturbed or natural settings up to 250 °C and 30 bar

Sulphide Mineral ReactionsClay-rich RockChemical EngineeringClay MineralEngineeringMineral-fluid InteractionGeologyGeochemistryHigh Hydrogen PressureChemistryDesulfurizationWater-rock InteractionHigh Temperature GeochemistryRock Properties