НЕКОТОРЫЕ ЧЕРТЫ ТОПОМИНЕРАЛОГИИ ГРАНАТА КРИВОРОЖСКОГО БАССЕЙНА

Анотація

Localization of garnets within the slate strata of Kryvyj Rig ferruginous formation
was controlled by chemical and methamorphic factors. The probability of origin and the
abundance of garnets in slates were determined by aluminium and iron oxides relation.
The garnet became rock-forming mineral with transition from greenschist to epidote-
amphibolite facies of methamorphism of slates.