Fragmentary structure of petmatite veins and prediction of muscovite bearing capacity
Authors:
Abstract
Examples of the most typical pegmatite veins of the North Baikal region, located in granitoid bodies and represented by combinations of converged different-structured zones, which have a rootless bar-shape of a certain spatial orientation of sizes, are considered. Prospective mica saturation is associated mainly with large-block (pegmatoid) zones, the separation of which from the "background" of other structures and the correct geometrization are of great practical importance.
Область исследования:
(Archived) Without section
Funding:
None
References
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