Hydrothermal experiments on olivine-quartz-seawater system at 300 °C: implication for the progress of silica-metasomatism during serpentinization at the crust-mantle boundary in the oceanic lithosphere
Hydrothermal experiments on olivine-quartz-seawater system at 300 °C: implication for the progress of silica-metasomatism during serpentinization at the crust-mantle boundary in the oceanic lithosphere
