pegmatitter
Pegmatite is a type of intrusive igneous rock characterized by its exceptionally large crystal size, often exceeding several centimeters or even meters in length. These coarse-grained rocks form from the slow crystallization of magma rich in volatiles such as water, boron, fluorine, and lithium, which lower the melting point of the magma and allow large crystals to develop. Pegmatites typically occur as dikes, veins, or irregular masses within or adjacent to other igneous rocks, particularly granites.
The formation of pegmatites is closely linked to the final stages of magma crystallization in plutonic environments.
Pegmatites are economically significant as sources of lithium, beryllium, tantalum, and rare earth elements. They also
The study of pegmatites contributes to understanding magmatic processes, mineralization, and the formation of economically valuable