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This document summarizes metamorphism, the process by which pre-existing rocks undergo physical and chemical changes due to increases in temperature and/or pressure. Metamorphism results in the formation of new minerals and textures. Common metamorphic processes include recrystallization, phase changes, and reactions forming new minerals. Increasing temperature and pressure can drive these changes. The document also describes different types of metamorphic rocks including foliated rocks like slate, schist a

Author

Helen Chen

Language

EN