To On the genesis of crystal-bearing the Ural crustalenose pegmatites of the Urals
Abstract
Pegmatite fields confined to the zone of development of Hercynian granitoid intrusions on the eastern slope of the Urals have been studied, as is known, for a very long time. To a large extent, these pegmatites are among those natural objects on which the classical theory of the genesis of pegmatite formations was built ...
Область исследования:
(Archived) Without section
Funding:
None
References
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