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The document discusses the metamorphic process, defining it as the transformation of rocks in solid state due to changes in temperature and pressure, distinct from weathering. It outlines the limits of metamorphism, including diagenesis and anatexis, and emphasizes the roles of temperature, pressure, and chemically active fluids in driving metamorphic reactions. The synthesis section highlights how the analysis of mineral assemblages can reveal the pressure-temperature-time paths of metamorphic rocks, servi

Author

hemantnda764

Language

EN