Pressure solution is a common phenomenon in massive sulphide zinc-lead deposits of western Canada and may have been an important factor leading to the mobilizahon of ore-forming materials during diagenesis, deformatio...Pressure solution is a common phenomenon in massive sulphide zinc-lead deposits of western Canada and may have been an important factor leading to the mobilizahon of ore-forming materials during diagenesis, deformation and metamorphism of sedimentary ores. The control of ductile shear zones over gold mineralization could be explained in view of pressure solution of gold-bearing miner-als under shearing stress and the resultant mobilization of this metal.展开更多
文摘Pressure solution is a common phenomenon in massive sulphide zinc-lead deposits of western Canada and may have been an important factor leading to the mobilizahon of ore-forming materials during diagenesis, deformation and metamorphism of sedimentary ores. The control of ductile shear zones over gold mineralization could be explained in view of pressure solution of gold-bearing miner-als under shearing stress and the resultant mobilization of this metal.
