Dykes of the Mamsko-Chuyskaya muscovite province and their relationship with granites, which are the parent for pegmatites
Authors:
Abstract
In the geologic history of the province several periods of manifestation of bark magmatism are established. Of special interest are the so-called "intra-pegmatite" dikes of granites, accumulations of which are found in many pegmatite fields not only in the Mamsko-Chuyskaya province.
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References
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