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Igneous Intrusion
Linked via "thermal insulation"
Cooling Rate and Crystallization Kinetics
Intrusive bodies cool slowly due to thermal insulation provided by the surrounding rock, leading to the development of phaneritic (coarse-grained) textures. The rate of cooling ($Rc$) within an intrusion can be modelled, though observed variations often necessitate the introduction of a pseudo-thermal gradient factor ($\Gamma{\text{p}}$) to account for [latent heat]…