SPATIAL DISTRIBUTION AND FORMATION CONDITIONS OF AU-BEARING PORPHYRY CU-MO DEPOSITS IN THE NORTHEAST OF RUSSIA

Volkov A.V.; Sidorov A.A.; Prokof'ev V.Yu.; Savva N.E.; Egorov V.N.; Shapovalov V.S.; Kolova E.E.

dc.contributor.author	Volkov A.V.
dc.contributor.author	Sidorov A.A.
dc.contributor.author	Prokof'ev V.Yu.
dc.contributor.author	Savva N.E.
dc.contributor.author	Egorov V.N.
dc.contributor.author	Shapovalov V.S.
dc.contributor.author	Kolova E.E.
dc.date.accessioned	2024-12-22T03:47:50Z
dc.date.available	2024-12-22T03:47:50Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518422
dc.identifier.citation	Geology of Ore Deposits, 2006, 48, 6, 448-472
dc.identifier.issn	1075-7015
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47046
dc.description.abstract	By analogy with other metallogenic belts of the Circum-Pacific ring, the metallogenic belts in the Northeast of Russia are promising for discovery of large and superlarge porphyry-type Au-Cu-Mo deposits. The spatial distribution of these deposits is controlled by intrusive domes in Middle Paleozoic, Late Jurassic-Early Cretaceous, and Late Cretaceous volcanic belts. New data on formation conditions and sources of ore matter are presented in this paper with respect to the deposits of the Baim and Koni-P'yagina ore districts of the Oloi and Uda-Murgal metallogenic belts. Some aspects of a geological and genetic model of the porphyry copper ore-magmatic system are discussed. © Pleiades Publishing, Inc. 2006.
dc.subject	Cretaceous
dc.subject	Jurassic
dc.title	SPATIAL DISTRIBUTION AND FORMATION CONDITIONS OF AU-BEARING PORPHYRY CU-MO DEPOSITS IN THE NORTHEAST OF RUSSIA
dc.type	Статья
dc.identifier.doi	10.1134/S107570150606002X
dc.subject.age	Mesozoic::Cretaceous
dc.subject.age	Мезозой::Меловая
dc.subject.age	Mesozoic::Jurassic
dc.subject.age	Мезозой::Юрская