NON-PEGMATITIC DEPOSITS OF BERYLLIUM: MINERALOGY, GEOLOGY, PHASE EQUILIBRIA AND ORIGIN

dc.contributor.author	Barton M.D.
dc.contributor.author	Young S.
dc.date.accessioned	2021-10-16T08:29:58Z
dc.date.available	2021-10-16T08:29:58Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=28509074
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2002, 50, С. 5, 591-691
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/30715
dc.description.abstract	Non-pegmatitic occurrences of Be minerals constitute a diverse set of geologic environments of considerable mineralogical and petrological interest; they currently provide the majority of the world’s Be ore and emeralds and they contain the greatest resource of these commodities. Of the approximately 100 Be minerals known (see Chapter 1 by Grew; Appendix A1), most occur in hydrothermal deposits or non-pegmatitic igneous rocks, where their distribution varies systematically with the setting and origin (Table 11, Fig. 11). Beryllium minerals are best known from geologic systems associated with felsic magmatism. They also occur in a variety...
dc.title	NON-PEGMATITIC DEPOSITS OF BERYLLIUM: MINERALOGY, GEOLOGY, PHASE EQUILIBRIA AND ORIGIN
dc.type	Статья

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