In general, the slower the cooling, the larger the crystals in the final rock. Because of this, we assume that coarse grained igneous rocks are "intrusive," in. Crystals in magma grow in a similar way as the melt cools. and the resulting rock is fine-grained, with crystals usually less than 1mm in size. Most aphanitic rocks are characterized by mineral grains less than Many fine-grained allotriomorphic-granular rocks are more simply termed sugary.
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