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Metamorphic rocks are formed through the process of metamorphism, which alters the mineral composition, texture, and structure of parent rocks under temperature, pressure, and chemically active fluids. There are various types of metamorphism, including thermal, dynamic, geothermal, metasomatic, dynamothermal, and plutonic, each defined by the predominant conditions during formation. Common metamorphic rocks include gneiss, marble, and slate, each with distinct physical properties and uses in civil engineeri

Author

Bhawani Shankar

Language

EN