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This document discusses metamorphism, describing it as the mineralogical and structural changes that occur in solid rocks subjected to changes in pressure, temperature, and chemical environments. It outlines the main types of metamorphism including contact, regional, cataclastic, shock, burial, and hydrothermal metamorphism. Grades of metamorphism increase with greater temperature and pressure. The agents that drive metamorphic changes are heat, pressure, and fluids, which can cause minerals to transform or
- Author
- Bhargav Arandhara
- Language
- EN