The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform
Identifying the cratonic affinity of Neoproterozoic crust that surrounds the northern margin of the Siberian Craton (SC) is critical for determining its tectonic evolution and placing the Craton in Neoproterozoic supercontinental reconstructions. Integration of new U–Pb–Hf detrital zircon data with...
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fttomskstateuniv:vtls:000629898 2023-05-15T18:31:14+02:00 The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform Priyatkina Nadezhda Khudoley Andrei Zastrozhnov Dmitry Ershova Victoria Chamberlain Kevin R. Shatsillo Andrey Proskurnin Vasily Collins William J. 2017 https://doi.org/10.1080/00206814.2017.1289341 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000629898 eng eng International geology review. 2017. Vol. 59 № 13. P. 1632-1656 детритовый циркон Сибирь протерозой орогенные пояса сибирский кратон Таймырский ороген осадочные породы статьи в журналах info:eu-repo/semantics/article 2017 fttomskstateuniv https://doi.org/10.1080/00206814.2017.1289341 2019-05-17T20:02:06Z Identifying the cratonic affinity of Neoproterozoic crust that surrounds the northern margin of the Siberian Craton (SC) is critical for determining its tectonic evolution and placing the Craton in Neoproterozoic supercontinental reconstructions. Integration of new U–Pb–Hf detrital zircon data with regional geological constraints indicates that distinct Neoproterozoic arc-related magmatic belts can be identified within the Taimyr orogen. Sedimentary rocks derived from 970 to 800 Ma arc-related suites reveal abundant Archean and Paleoproterozoic detritus characteristic of the SC. The 720–600 Ma arc-related zircon population from the younger Cambrian sedimentary rocks is also complemented by an exotic juvenile Mesoproterozoic zircon population and erosional products of older arc-related suites. Nonetheless numerous evidences imply that both arcs broadly reworked Siberian basement components. We suggest that the early Neoproterozoic (ca. 970–800 Ma) arc system of the Taimyr orogen evolved on the active margin of the SC and probably extended along the periphery of Rodinia into Valhalla orogen of NE Laurentia. We also suggest the late Neoproterozoic (750–550 Ma) arc system could have been part of the Timanian orogen which linked Siberia and Baltica at the Precambrian/Phanerozoic transition. Article in Journal/Newspaper Taimyr Siberia Tomsk State University Research Library Valhalla ENVELOPE(161.933,161.933,-77.583,-77.583) International Geology Review 59 13 1632 1656 |
institution |
Open Polar |
collection |
Tomsk State University Research Library |
op_collection_id |
fttomskstateuniv |
language |
English |
topic |
детритовый циркон Сибирь протерозой орогенные пояса сибирский кратон Таймырский ороген осадочные породы |
spellingShingle |
детритовый циркон Сибирь протерозой орогенные пояса сибирский кратон Таймырский ороген осадочные породы Priyatkina Nadezhda Khudoley Andrei Zastrozhnov Dmitry Ershova Victoria Chamberlain Kevin R. Shatsillo Andrey Proskurnin Vasily Collins William J. The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
topic_facet |
детритовый циркон Сибирь протерозой орогенные пояса сибирский кратон Таймырский ороген осадочные породы |
description |
Identifying the cratonic affinity of Neoproterozoic crust that surrounds the northern margin of the Siberian Craton (SC) is critical for determining its tectonic evolution and placing the Craton in Neoproterozoic supercontinental reconstructions. Integration of new U–Pb–Hf detrital zircon data with regional geological constraints indicates that distinct Neoproterozoic arc-related magmatic belts can be identified within the Taimyr orogen. Sedimentary rocks derived from 970 to 800 Ma arc-related suites reveal abundant Archean and Paleoproterozoic detritus characteristic of the SC. The 720–600 Ma arc-related zircon population from the younger Cambrian sedimentary rocks is also complemented by an exotic juvenile Mesoproterozoic zircon population and erosional products of older arc-related suites. Nonetheless numerous evidences imply that both arcs broadly reworked Siberian basement components. We suggest that the early Neoproterozoic (ca. 970–800 Ma) arc system of the Taimyr orogen evolved on the active margin of the SC and probably extended along the periphery of Rodinia into Valhalla orogen of NE Laurentia. We also suggest the late Neoproterozoic (750–550 Ma) arc system could have been part of the Timanian orogen which linked Siberia and Baltica at the Precambrian/Phanerozoic transition. |
format |
Article in Journal/Newspaper |
author |
Priyatkina Nadezhda Khudoley Andrei Zastrozhnov Dmitry Ershova Victoria Chamberlain Kevin R. Shatsillo Andrey Proskurnin Vasily Collins William J. |
author_facet |
Priyatkina Nadezhda Khudoley Andrei Zastrozhnov Dmitry Ershova Victoria Chamberlain Kevin R. Shatsillo Andrey Proskurnin Vasily Collins William J. |
author_sort |
Priyatkina |
title |
The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
title_short |
The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
title_full |
The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
title_fullStr |
The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
title_full_unstemmed |
The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform |
title_sort |
proterozoic evolution of northern siberian craton margin: a comparison of u–pb–hf signatures from sedimentary units of the taimyr orogenic belt and the siberian platform |
publishDate |
2017 |
url |
https://doi.org/10.1080/00206814.2017.1289341 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000629898 |
long_lat |
ENVELOPE(161.933,161.933,-77.583,-77.583) |
geographic |
Valhalla |
geographic_facet |
Valhalla |
genre |
Taimyr Siberia |
genre_facet |
Taimyr Siberia |
op_source |
International geology review. 2017. Vol. 59 № 13. P. 1632-1656 |
op_doi |
https://doi.org/10.1080/00206814.2017.1289341 |
container_title |
International Geology Review |
container_volume |
59 |
container_issue |
13 |
container_start_page |
1632 |
op_container_end_page |
1656 |
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1766214962263359488 |