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Possibility of formation of considerable part of albitites in Anzass iron-deposit as result of metasomatic transformation of enclosing rocks represented by paraschists; process is accompanied by introduction of sodium and aluminum and by removal of silica.
Possibility of formation of considerable part of albitites in Anzass iron-deposit as result of metasomatic transformation of enclosing rocks represented by paraschists; process is accompanied by introduction of sodium and aluminum and by removal of silica.
Origin of Anzass albitites
O proiskhozhdenii Anzasskikh al'bititov
Pavlov, D.I. (author)
1961
7 pages
2 Plates
Article (Journal)
Russian
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