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fractional crystallization

geology

Quick Summary

Fractional crystallization is a geological process where minerals crystallize from a magma at different temperatures. As a magma cools, early-formed minerals, which are typically denser, settle out. This removal of early crystals leaves the remaining liquid magma with a different chemical composition, leading to the formation of new minerals as cooling continues.1

This process is fundamental to understanding how different types of igneous rocks form from a single parent magma. For example, a basaltic magma can transform into rocks like granite through fractional crystallization, as early-formed minerals are separated from the melt. This process, along with assimilation, where magma incorporates surrounding rock, can explain the diversity of magmatic compositions observed in nature.12

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