End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia

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dc.contributor.author Xiao W.J.
dc.contributor.author Windley B.F.
dc.contributor.author Huang B.C.
dc.contributor.author Han C.M.
dc.contributor.author Yuan C.
dc.contributor.author Chen H.L.
dc.contributor.author Sun M.
dc.contributor.author Sun S.
dc.contributor.author Li J.L.
dc.date.accessioned 2022-11-06T04:10:46Z
dc.date.available 2022-11-06T04:10:46Z
dc.date.issued 2009
dc.identifier.citation International Journal of Earth Sciences, 2009, v.98, p.1189-1217 ru_RU
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/39541
dc.description.abstract The Altaids is one of the largest accretionary orogenic collages in the world with the highest rate of Phanerozoic continental growth and significantmetallogenic importance. It is widely accepted that subduction-related orogenesis of the Altaids started in the late Precambrian and gradually migrated southward (present coordinates). How- ever, it is uncertain when and how the building of the Altaids was finally completed. Based on structural geology, geochemical, geochronological, and paleomagnetic data, this paper presents late Paleozoic to earlyMesozoic accretionary tectonics of two key areas, North Xinjiang in the west and Inner Mongolia in the east, together with neighboring Mongolia. The late Paleozoic tectonics of North Xinjiang and adjacent areas were characterized by continuous southward accretion along the wide southern active margin of Siberia and its final amalgamationwith the passivemargin of Tarim, which may have lasted to the end-Permian to early/ mid-Triassic. ru_RU
dc.language.iso en ru_RU
dc.subject End-Permian to mid-Triassic termination ru_RU
dc.subject Accretionary process ru_RU
dc.subject Southern Altaids ru_RU
dc.subject Geodynamic evolution ru_RU
dc.subject Continental growth ru_RU
dc.subject Metallogeny ru_RU
dc.subject Central Asia ru_RU
dc.title End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia ru_RU
dc.type Article ru_RU
dc.identifier.doi 10.1007/s00531-008-0407-z
dc.subject.age Mesozoic::Triassic
dc.subject.age Paleozoic::Permian
dc.subject.age Палеозой::Пермская ru
dc.subject.age Мезозой::Триасовая ru


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