Origin of mineralizing fluids of the sediment-hosted Navachab gold mine, Namibia: Constraints from stable (O, H, C, S) isotopes

Earth and Planetary Sciences

• Peridotite 100%
• Fluid-Rock Interaction 100%
• Calcite 50%
• Dyke (Water management) 50%
• Metasedimentary Rock 50%
• Amphibolite 50%
• Granulite Facies 50%
• Clinopyroxene 50%
• Lamprophyre 50%
• Garnet 50%
• Isotopic Fractionation 50%
• Zincblende 50%
• Prograde Metamorphism 50%
• Geothermal Gradient 50%
• Aplite 50%
• Bismuth Tellurides 50%
• Arsenopyrite 50%
• Metapelite 50%
• Chalcopyrite 50%