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The continuous reaction series primarily involves the mineral groups of feldspars and amphiboles, which represent the gradual transition from mafic to felsic compositions. As magma cools, minerals crystallize in a specific order: olivine, pyroxene, amphibole, and biotite, followed by feldspars, muscovite, and quartz. This series illustrates the progressive change in mineral composition based on temperature and chemical environment during crystallization. The continuous nature of the series reflects the range of compositions within the feldspar and amphibole families, allowing for a spectrum of mineral types rather than distinct categories.

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7mo ago

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