Recrystallization (geology)

In geology, solid-state recrystallization is a metamorphic process that occurs under high temperatures and pressures where atoms of minerals are reorganized by diffusion and/or dislocation glide. During this process, the physical structure of the minerals is altered while the composition remains unchanged.^[1][2] This is in contrast to metasomatism, which is the chemical alteration of a rock by hydrothermal and other fluids.

Crystallization
Fundamentals
Crystal Crystal structure Nucleation
Concepts
Crystallization Crystal growth Recrystallization Seed crystal Protocrystalline Single crystal
Methods and technology
Boules Bridgman–Stockbarger method Van Arkel–de Boer process Czochralski method Epitaxy Flux method Fractional crystallization Fractional freezing Hydrothermal synthesis Kyropoulos method Laser-heated pedestal growth Micro-pulling-down Shaping processes in crystal growth Skull crucible Verneuil method Zone melting
v t e

Solid-state recrystallization can be illustrated by observing how snow recrystallizes to ice. When snow is subjected to varying temperatures and pressures, individual snowflakes undergo a physical transformation but their composition remains the same. Limestone is a sedimentary rock that undergoes metamorphic recrystallization to form marble, and clays can recrystallize to muscovite mica.

References

1. "Metamorphic rock | Definition, Formation, & Facts | Britannica". www.britannica.com. 2024-10-07. Retrieved 2024-11-22.
2. Drury, Martyn R.; Urai, Janos L. (1990). "Deformation-related recrystallization processes". Tectonophysics. 172 (3–4): 235–253. doi:10.1016/0040-1951(90)90033-5.