Late-stage anhydrite-gypsum-siderite-dolomite-calcite assemblages record the transition from a deep to a shallow hydrothermal system in the Schwarzwald mining district, SW Germany
Keywords: رگهای هیدروترمال; Erosion; Hydrothermal veins; U-Pb age dating of carbonates; Fluid evolution; Mixing; Upper Rhine Graben; Uplift; Carbonates; Sulphates;