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...
Published in: | International Geology Review |
---|---|
Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2017
|
Subjects: | |
Online Access: | https://doi.org/10.1080/00206814.2017.1289341 https://openrepository.ru/article?id=284281 |
id |
ftneicon:oai:rour.neicon.ru:rour/284281 |
---|---|
record_format |
openpolar |
spelling |
ftneicon:oai:rour.neicon.ru:rour/284281 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 https://openrepository.ru/article?id=284281 eng eng vtls:000629898 doi:10.1080/00206814.2017.1289341 https://openrepository.ru/article?id=284281 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 ftneicon https://doi.org/10.1080/00206814.2017.1289341 2020-07-21T12:29:29Z 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 NORA (National aggregator of open repositories of Russian universities) Valhalla ENVELOPE(161.933,161.933,-77.583,-77.583) International Geology Review 59 13 1632 1656 |
institution |
Open Polar |
collection |
NORA (National aggregator of open repositories of Russian universities) |
op_collection_id |
ftneicon |
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, Nadezhda |
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 https://openrepository.ru/article?id=284281 |
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_relation |
vtls:000629898 doi:10.1080/00206814.2017.1289341 https://openrepository.ru/article?id=284281 |
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 |
_version_ |
1766214962598903808 |