TECTONIC POSITION OF THE ALSHAR AU-AS-SB-TL DEPOSIT, MACEDONIA

dc.contributor.author	Kochneva N.T.
dc.contributor.author	Volkov A.V.
dc.contributor.author	Serafimovski T.
dc.contributor.author	Tasev G.
dc.contributor.author	Tomson I.N.
dc.date.accessioned	2024-10-23T07:15:56Z
dc.date.available	2024-10-23T07:15:56Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13510860
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 175-178
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46142
dc.description.abstract	The territory of Macedonia experienced long-term geological evolution. Its majority is occupied by the Serbian–Macedonian and Pelagonia crystalline massifs, separated by the Mesozoic Vardarian riftogenic graben. Macedonia is located in the Serbian–Macedonian part of the Eurasian Tethys metallogenic belt. Mineralization related to the Cenozoic activation in this area is expressed in the formation of volcanoplutonic associations in the dispersed spreading environment. The activation spanned the Serbian–Macedonian Massif and part of the Vardarian riftogenic zone. Superimposed structures of this period occur as narrow NW-trending grabenlike depressions complicated by local ring structures of the chamber type.
dc.title	TECTONIC POSITION OF THE ALSHAR AU-AS-SB-TL DEPOSIT, MACEDONIA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020036

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