About the theory of pegmatite genesis

V. D. Nikitin

Vol 30 Iss. 2

Pages:

44-117

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RUS

Article

Geology

About the theory of pegmatite genesis

Authors:

V. D. Nikitin

Date submitted:

1954-08-12

Date accepted:

1954-10-12

Date published:

1955-07-16

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 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

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About the theory of pegmatite genesis

Abstract

References

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