NEW CONCEPT OF THE GEODYNAMIC NATURE OF THE DEVONIAN ORE-BEARING BASALT-RHYOLITE FORMATION IN RUDNYI ALTAI

dc.contributor.author	Promyslova M.Yu.
dc.date.accessioned	2022-07-18T05:29:12Z
dc.date.available	2022-07-18T05:29:12Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13450084
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1209-1211
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38225
dc.description.abstract	It can be assumed that orebearing volcanosedimentary sequences of Rudnyi Altai began to form since the Emsian at the transition from the axial rift of the Ob-Zaisan ocean spreading to the continental rift of the Altai-Mongol block. Devonian riftogenesis was manifested only in Rudnyi Altai, neighboring areas of Gornyi Altai, and the entire central part of the Altai-Sayan fold system. This process involved a vast (over 2000-km-long and up to 200-km-wide) region [4] comparable in size to the Basin and Range Province in the western United States.
dc.subject	Devonian
dc.title	NEW CONCEPT OF THE GEODYNAMIC NATURE OF THE DEVONIAN ORE-BEARING BASALT-RHYOLITE FORMATION IN RUDNYI ALTAI
dc.type	Статья
dc.subject.age	Paleozoic::Devonian
dc.subject.age	Палеозой::Девонская	ru

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