The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia
U–Pb detrital zircon results from New Siberian Islands sandstones illuminate the long-lived controversy regarding the continuation of the Uralian orogen into the Arctic region. A dominant age peak of c . 285 Ma from Permian sandstone requires proximal derivation from Taimyr’s Carboniferous–Permian g...
Main Authors: | , , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
2016
|
Subjects: | |
Online Access: | https://doi.org/10.6084/m9.figshare.3453830.v1 https://figshare.com/articles/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830 |
id |
ftgeosoclonfig:oai:figshare.com:article/3453830 |
---|---|
record_format |
openpolar |
spelling |
ftgeosoclonfig:oai:figshare.com:article/3453830 2023-05-15T14:45:30+02:00 The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia Victoria L. Pease Alexander B. Kuzmichev Maria K. Danukalova 2016-06-21T11:42:35Z https://doi.org/10.6084/m9.figshare.3453830.v1 https://figshare.com/articles/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830 unknown doi:10.6084/m9.figshare.3453830.v1 https://figshare.com/articles/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830 CC BY 4.0 CC-BY Geology Taimyr continuation Permian sandstone data record Islands sandstones New Permian time 285 Ma provenance age peak Uralian foreland basin Devonian sandstone Uralian orogen Baltica affinities Uralian source Arctic region Dataset 2016 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.3453830.v1 2020-02-21T07:23:58Z U–Pb detrital zircon results from New Siberian Islands sandstones illuminate the long-lived controversy regarding the continuation of the Uralian orogen into the Arctic region. A dominant age peak of c . 285 Ma from Permian sandstone requires proximal derivation from Taimyr’s Carboniferous–Permian granites, thought to reflect syn- to post-tectonic Uralian magmatism. The provenance of Devonian sandstone has Baltica affinities. The data record a dramatic change in provenance between Devonian and Permian time, from Baltica to a mixed Baltica + Uralian source. Our results confirm that the Uralian foreland basin extended from Taimyr to the New Siberian Islands. Dataset Arctic New Siberian Islands Taimyr Geological Society of London: Figshare Arctic New Siberian Islands ENVELOPE(142.000,142.000,75.000,75.000) |
institution |
Open Polar |
collection |
Geological Society of London: Figshare |
op_collection_id |
ftgeosoclonfig |
language |
unknown |
topic |
Geology Taimyr continuation Permian sandstone data record Islands sandstones New Permian time 285 Ma provenance age peak Uralian foreland basin Devonian sandstone Uralian orogen Baltica affinities Uralian source Arctic region |
spellingShingle |
Geology Taimyr continuation Permian sandstone data record Islands sandstones New Permian time 285 Ma provenance age peak Uralian foreland basin Devonian sandstone Uralian orogen Baltica affinities Uralian source Arctic region Victoria L. Pease Alexander B. Kuzmichev Maria K. Danukalova The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
topic_facet |
Geology Taimyr continuation Permian sandstone data record Islands sandstones New Permian time 285 Ma provenance age peak Uralian foreland basin Devonian sandstone Uralian orogen Baltica affinities Uralian source Arctic region |
description |
U–Pb detrital zircon results from New Siberian Islands sandstones illuminate the long-lived controversy regarding the continuation of the Uralian orogen into the Arctic region. A dominant age peak of c . 285 Ma from Permian sandstone requires proximal derivation from Taimyr’s Carboniferous–Permian granites, thought to reflect syn- to post-tectonic Uralian magmatism. The provenance of Devonian sandstone has Baltica affinities. The data record a dramatic change in provenance between Devonian and Permian time, from Baltica to a mixed Baltica + Uralian source. Our results confirm that the Uralian foreland basin extended from Taimyr to the New Siberian Islands. |
format |
Dataset |
author |
Victoria L. Pease Alexander B. Kuzmichev Maria K. Danukalova |
author_facet |
Victoria L. Pease Alexander B. Kuzmichev Maria K. Danukalova |
author_sort |
Victoria L. Pease |
title |
The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
title_short |
The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
title_full |
The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
title_fullStr |
The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
title_full_unstemmed |
The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia |
title_sort |
new siberian islands and evidence for the continuation of the uralides, arctic russia |
publishDate |
2016 |
url |
https://doi.org/10.6084/m9.figshare.3453830.v1 https://figshare.com/articles/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830 |
long_lat |
ENVELOPE(142.000,142.000,75.000,75.000) |
geographic |
Arctic New Siberian Islands |
geographic_facet |
Arctic New Siberian Islands |
genre |
Arctic New Siberian Islands Taimyr |
genre_facet |
Arctic New Siberian Islands Taimyr |
op_relation |
doi:10.6084/m9.figshare.3453830.v1 https://figshare.com/articles/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.3453830.v1 |
_version_ |
1766316894571200512 |