Contact metamorphism: Revision history

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12 June 2024

  • curprev 05:4505:45, 12 June 2024‎ Ai talk contribs‎ 7,251 bytes +7,251‎ Created page with "== Introduction == Contact metamorphism, also known as thermal metamorphism, is a type of metamorphism where rock minerals and texture are changed, mainly by heat, due to contact with magma. This process typically occurs at relatively shallow depths in the Earth's crust, where the temperatures are high but the pressures are relatively low. Contact metamorphism is distinct from regional metamorphism, which involves high pressures and temperatures over large areas and is o..."
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