STRUCTURAL POSITION OF GOLD ORE DEPOSITS IN THE INTRUSIVE VOLCANOGENIC FRAMING OF THE PRECAMBRIAN GONZHA SALIENT (UPPER AMUR REGION)

Boriskina N.G.; Khomich V.G.

dc.contributor.author	Boriskina N.G.
dc.contributor.author	Khomich V.G.
dc.date.accessioned	2024-11-09T08:38:08Z
dc.date.available	2024-11-09T08:38:08Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526123
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 526-529
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46403
dc.description.abstract	Recent geological–geophysical studies of gold ore districts in the Russian Far East specified the essential role of Precambrian massifs, salients, blocks, deep faults, and protomagmatic chambers in distribution of noble metal deposits. However, additional information on position and major factors determining localization of explored deposits is needed to predict new objects in known ore districts and select the most promising ore occurrences. The analysis of geological data on the Gonzha area from this standpoint revealed that gold deposits in this area are associated with necks, stocks, sills, and paleovents located at the margins of volcanoplutonic granitoid massifs surrounding the local Precambrian salient.
dc.subject	Gonzha area
dc.subject	Precambrian
dc.title	STRUCTURAL POSITION OF GOLD ORE DEPOSITS IN THE INTRUSIVE VOLCANOGENIC FRAMING OF THE PRECAMBRIAN GONZHA SALIENT (UPPER AMUR REGION)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040040
dc.subject.age	Precambrian
dc.subject.age	Докембрий