HISTORY OF THE TECTONIC DEVELOPMENT OF THE ALPINE FOLDED REGION OF SOUTHEASTERN EUROPE AND ASIA MINOR - NEW DATA ON THE TECTONIC STRUCTURE AND HISTORY OF DEVELOPMENT OF THE ALPINE ZONE OF EUROPE |
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Abstract: | The pyrite-polymetallic deposits of the Rudnyy Altay, which occur in early geosynclinal sedimentary-volcanogenic sequences, are considered as polygenetic and polychronous. Their basic features and patterns of localization may be explained by the specific nature of the formation of the ore-surrounding volcanogenic associations and features of later redeposition of the ore material. —Authors. |
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