LATE PALEOZOIC FAULTS OF THE ALTAI REGION, CENTRAL ASIA: TECTONIC PATTERN AND MODEL OF FORMATION
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dc.contributor.author | Buslov M.M. | |
dc.contributor.author | Smirnova L.V. | |
dc.contributor.author | Safonova I.Yu | |
dc.contributor.author | Semakov N.N. | |
dc.contributor.author | Kiryanova A.P. | |
dc.contributor.author | Watanabe T. | |
dc.contributor.author | Fujiwara Y. | |
dc.contributor.author | Iwata K. | |
dc.date.accessioned | 2022-09-28T05:54:13Z | |
dc.date.available | 2022-09-28T05:54:13Z | |
dc.date.issued | 2004 | |
dc.identifier | https://elibrary.ru/item.asp?id=13461542 | |
dc.identifier.citation | Journal of Asian Earth Sciences, 2004, 23, 5, 655-671 | |
dc.identifier.issn | 1367-9120 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38800 | |
dc.description.abstract | The present kinematic and dynamic analysis of large-scale strike-slip faults, which enabled the formation of a collage of Altai terranes as a result of two collisional events. The Late Devonian–Early Carboniferous collision of the Gondwana-derived Altai-Mongolian terrane and the Siberian continent resulted in the formation of the Charysh–Terekta system of dextral strike-slip faults and later the Kurai and Kuznetsk–Teletsk–Bashkauss sinistral strike-slip faults. The Late Carboniferous–Permian collision of the Siberian and Kazakhstan continents resulted in the formation of the Chara, Irtysh and North-East sinistral strike-slip zones. The age of deformation of both collisional events becomes younger toward the inner areas of the Siberian continent. In the same direction the amount of displacement of strike-slip faulting decreases from several thousand to several hundred kilometers. The width of the Late Paleozoic zone of deformation reaches 1500 km. These events deformed the accretion-collision continental margins and their primary paleogeographic pattern. | |
dc.subject | Strike-slip fault | |
dc.subject | Collision | |
dc.subject | Altai-Mongolian terrane | |
dc.subject | Kazakhstan continent | |
dc.subject | Siberian continen | |
dc.subject | Paleozoic | |
dc.title | LATE PALEOZOIC FAULTS OF THE ALTAI REGION, CENTRAL ASIA: TECTONIC PATTERN AND MODEL OF FORMATION | |
dc.type | Статья | |
dc.subject.age | Paleozoic | |
dc.subject.age | Палеозой | ru |
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