|Crystallization · Crystal growth
Recrystallization · Seed crystal
Protocrystalline · Single crystal
|Nucleation · Crystal
Crystal structure · Solid
|Methods and technology|
|Boules · Bridgman-Stockbarger
Czochralski process · Fractional crystalliz. · Frac. freezing · Hydroth. synthesis · LHPG · Iodide process
|This article does not cite any references or sources. (March 2010)|
In geology, solid-state recrystallization is a metamorphic process that occurs under situations of intense temperature and pressure where grains, atoms or molecules of a rock or mineral are packed closer together, creating a new crystal structure. The basic composition remains the same. This process can be illustrated by observing how snow recrystallizes to ice without melting.
As opposed to metasomatism, which is a chemical change caused by metamorphism, recrystallization is a physical process. However, recrystallization can occur when a local migration of chemicals results in the chemical change of the rock or mineral with no external addition of materials.