On the theory of pegmatite genesis
Authors:
Abstract
Such minerals as muscovite, feldspars, ores of a number of valuable metals - lithium, beryllium, partly niobium, tantalum, elements of the rare earth group, etc., are mostly extracted from pegmatite deposits. The industrial significance of pegmatite bodies is constantly increasing. Pegmatites, in addition, are often receptacles of many rare minerals, and in some cases serve as natural museums of beautiful crystals, which attracts the special attention of mineralogists. The peculiarity of the genesis of pegmatites has long been of interest to petrologists and geochemists. In the phenomena of pegmatite formation, researchers encounter perhaps the most complex process of mineral formation, with which one can perhaps compare only the process of skarn formation. When studying pegmatites, the interests of petrologists and mineralogists are closely intertwined. In pegmatites, phenomena that indicate the general features of various processes of mineral formation and transformation of the rocks that make up the veins are manifested with such exceptional clarity and on such, often, enormous scales that in other types of deposits they are generally unknown or are discovered in a much less clear form.
Область исследования:
Geology
Funding:
None
References
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