К МИНЕРАЛОГИИ КРИОГЕННЫХ ЗОН ОКИСЛЕНИЯ РУДНЫХ МЕСТОРОЖДЕНИЙ ЮГО-ВОСТОКА ГОРНОГО АЛТАЯ

Abstract

Oxidation zones of ore deposits are considered for the mountainous part of the Mountain Altai. Their structure is compared with zonality of cryogenic areas. Rozenite and siderotile, characteristic sulfate minerals, are described for the first time.