The Taimyr Peninsula of Arctic Siberia has tradi-
Late Precambrian and Palaeozoic platform sediments from the Central–South Taimyr Peninsula (Arctic Siberia) are all remagnetised. The remagnetisation is prefold and is related to thermal remagnetisation caused by Taimyr Trap magmatism. The remagnetisation age is estimated to 220–230 Ma and, hence, i...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.9223 2023-05-15T14:52:17+02:00 The Taimyr Peninsula of Arctic Siberia has tradi- Trond H. Torsvik A Torgeir B. Andersen D South Taimyr North Taimyr The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.9223 http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.9223 http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf text 2001 ftciteseerx 2016-04-24T00:01:09Z Late Precambrian and Palaeozoic platform sediments from the Central–South Taimyr Peninsula (Arctic Siberia) are all remagnetised. The remagnetisation is prefold and is related to thermal remagnetisation caused by Taimyr Trap magmatism. The remagnetisation age is estimated to 220–230 Ma and, hence, is considerably younger than the ca. 251 Ma age for the main body of Siberian Trap flood basalts. The folding that affected the Taimyr region platform sediments also included the Taimyr ‘‘Traps,’ ’ hence, relegating Taimyr deformation to post-Mid Triassic time, and most probably, to a Late Triassic age. This shows that whilst thrusting terminated in the Urals during the Permian, crustal shortening continued in Taimyr, Novaya–Zemlya and the South Barents Sea, well into the Mesozoic. Text Arctic Barents Sea Novaya Zemlya Taimyr Siberia Unknown Arctic Barents Sea |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Late Precambrian and Palaeozoic platform sediments from the Central–South Taimyr Peninsula (Arctic Siberia) are all remagnetised. The remagnetisation is prefold and is related to thermal remagnetisation caused by Taimyr Trap magmatism. The remagnetisation age is estimated to 220–230 Ma and, hence, is considerably younger than the ca. 251 Ma age for the main body of Siberian Trap flood basalts. The folding that affected the Taimyr region platform sediments also included the Taimyr ‘‘Traps,’ ’ hence, relegating Taimyr deformation to post-Mid Triassic time, and most probably, to a Late Triassic age. This shows that whilst thrusting terminated in the Urals during the Permian, crustal shortening continued in Taimyr, Novaya–Zemlya and the South Barents Sea, well into the Mesozoic. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Trond H. Torsvik A Torgeir B. Andersen D South Taimyr North Taimyr |
spellingShingle |
Trond H. Torsvik A Torgeir B. Andersen D South Taimyr North Taimyr The Taimyr Peninsula of Arctic Siberia has tradi- |
author_facet |
Trond H. Torsvik A Torgeir B. Andersen D South Taimyr North Taimyr |
author_sort |
Trond H. Torsvik A |
title |
The Taimyr Peninsula of Arctic Siberia has tradi- |
title_short |
The Taimyr Peninsula of Arctic Siberia has tradi- |
title_full |
The Taimyr Peninsula of Arctic Siberia has tradi- |
title_fullStr |
The Taimyr Peninsula of Arctic Siberia has tradi- |
title_full_unstemmed |
The Taimyr Peninsula of Arctic Siberia has tradi- |
title_sort |
taimyr peninsula of arctic siberia has tradi- |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.9223 http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf |
geographic |
Arctic Barents Sea |
geographic_facet |
Arctic Barents Sea |
genre |
Arctic Barents Sea Novaya Zemlya Taimyr Siberia |
genre_facet |
Arctic Barents Sea Novaya Zemlya Taimyr Siberia |
op_source |
http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.9223 http://folk.uio.no/torgeir/pdfpapers/Taimyr2002.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766323495474561024 |