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Geochemical analysis reveals crystallization from rest magma in granitoids of the Kalguty massif, indicating complex formation processes.
Exemplified by the Kalguty massif, the Gorny-Altai granite-leucogranite Mo-W-bearing orepetrogeochemical type was recognized and characterized petrochemically and geochemically. Crystallization from rest magma was shown to be the most probable process in the formation of leucocratic granites of the massif.
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Malikova et al. (1991) studied this question.
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