The principles of metal concentration and deposition in magmatic and hydrothermal environments are examined. Natural and experimental data, including fluid inclusion, stable isotope, metal solubility, mineral stability, and metal partition behavior, are used to develop genetic models for ore deposits. Such models form the basis of mineral exploration strategies.
The principles of metal concentration and deposition in magmatic and hydrothermal environments are examined. Natural and experimental data, including fluid inclusion, stable isotope, metal solubility, mineral stability, and metal partition behavior, are used to develop genetic models for ore deposits. Such models form the basis of mineral exploration strategies.
