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