Material composition and internal structure of granite-pegmatite bodies of the Mamsko-Chuyskaya mica province
Authors:
Abstract
In the Mamsko-Chuyskaya mica province many deposits are confined to the bodies of the so-called giganto-migmatites, representing a system of layer-by-layer and secant pegmatite deposits, so they were studied by many geologists. One of the first researchers was N.V. Petrovskaya who called these bodies giganto-migmatites. In subsequent years, all geologists unanimously noted that more than half of the pegmatite varieties involved in the structure of giganto-migmatites are granitic rocks. They were named granite-pegmatites.
Область исследования:
(Archived) Geology and metallogeny
References
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