The metamorphic conditions characteristic of greenschist occur where the crust is thickened by continental collision or heated by rising magma.

Name: The metamorphic conditions characteristic of greenschist occur where the crust is thickened by continental collision or heated by rising magma.
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Greenschist facies metamorphism typically occurs at moderate temperatures and pressures, often associated with tectonic settings like continental collisions or areas with magmatic activity.

The Metamorphic Conditions Characteristic of Greenschist Occur Where the Crust