A reaction in which chemical constituentsof a rock are rearranged to form a new mineral assemblage, but no materialis added to or lost from the rock as a whole. Applied generally to diageneticor metamorphic environments.
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A reaction in which chemical constituentsof a rock are rearranged to form a new mineral assemblage, but no materialis added to or lost from the rock as a whole. Applied generally to diageneticor metamorphic environments.