Impact-generated hydrothermal circulation and metasomatism of the rochechouart astrobleme: mineralogy and major and trace element distribution
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
10.6 Metamorphic Hydrothermal Processes and Metasomatism
A hydrothermal model for metasomatism of neoarchean Algoma-Type banded iron formation to massive hematite ore at the Soudan Mine, NE Minnesota
Kinetics of silica metasomatism during serpentinization revealed by hydrothermal experiments on olivine-quartz-seawater system at 300 ∘C