MERCURY-ANTIMONY ORE FORMATION OF JASPEROID-TYPE DEPOSITS IN CENTRAL ASIA

A mercury-antimony ore formation has been recognized and characterized as a result of persistent and purposeful investigations of the jasperoid type of mineralization, which is typical of the Central-Asian mercury-antimony province. Research into conditions of localization of mineralization, its mineralogo-geochemical, genetic features and practical significance of major useful components allowed the mercury-antimony ore formation to be differentiated and the following subformations to be distinguished: mercury, mercury-antimony-arsenic, mercury-antimony-arsenic with fluorine, antimony, antimony-mercury, antimony-arsenic with fluorine, and antimony-complex metals.

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