Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic
Small depressions across the north-eastern part of October Revolution Island (Severnaya Zemlya archipelago, Kara terrane) are filled with continental terrigenous rocks, dated as Upper Carboniferous–Lower Permian in age based on palynological data. These rocks overlie Ordovician volcaniclastic rocks...
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ftmdpi:oai:mdpi.com:/2075-163X/12/10/1325/ 2023-08-20T04:04:08+02:00 Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic Victoria Ershova Andrei Prokopiev Daniel Stockli Daria Zbukova Anton Shmanyak agris 2022-10-20 application/pdf https://doi.org/10.3390/min12101325 EN eng Multidisciplinary Digital Publishing Institute Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min12101325 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 12; Issue 10; Pages: 1325 geochronology U-Pb dating Late Paleozoic Arctic Kara Sea Text 2022 ftmdpi https://doi.org/10.3390/min12101325 2023-08-01T06:57:56Z Small depressions across the north-eastern part of October Revolution Island (Severnaya Zemlya archipelago, Kara terrane) are filled with continental terrigenous rocks, dated as Upper Carboniferous–Lower Permian in age based on palynological data. These rocks overlie Ordovician volcaniclastic rocks above a prominent angular unconformity. U-Pb dating of detrital zircons from the Late Carboniferous–Lower Permian rocks reveals that most grains are Ordovician in age, ranging between 475–455 Ma. A subordinate population of Silurian detrital zircons is also present, contributing up to 15% of the dated population, while Precambrian grains mainly yield Neo-Mesoproterozoic ages and do not form prominent peaks. The combined U-Pb and (U-Th)/He ages indicate that most zircon (U-Th)/He ages were reset and average at ca. 317 Ma, suggesting ~6–7 km of Late Carboniferous uplift within the provenance area. This provenance area, mainly comprising Ordovician magmatic and volcanic rocks, was located close to the study area based on the coarse-grained nature of Late Carboniferous–Lower Permian rocks of north-eastern October Revolution Island. Therefore, we propose that Late Paleozoic tectonism significantly affected both the southern margin of the Kara terrane, as previously supposed, and also its north-eastern part. We propose that the Late Paleozoic Uralian suture zone continued to the north-eastern October Revolution Island and was responsible for the significant tectonic uplift of the studied region. This suture zone is now hidden beneath the younger Arctic basins. Text Arctic Kara Sea October Revolution Island Severnaya Zemlya MDPI Open Access Publishing Arctic Kara Sea Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) Minerals 12 10 1325 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
geochronology U-Pb dating Late Paleozoic Arctic Kara Sea |
spellingShingle |
geochronology U-Pb dating Late Paleozoic Arctic Kara Sea Victoria Ershova Andrei Prokopiev Daniel Stockli Daria Zbukova Anton Shmanyak Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
topic_facet |
geochronology U-Pb dating Late Paleozoic Arctic Kara Sea |
description |
Small depressions across the north-eastern part of October Revolution Island (Severnaya Zemlya archipelago, Kara terrane) are filled with continental terrigenous rocks, dated as Upper Carboniferous–Lower Permian in age based on palynological data. These rocks overlie Ordovician volcaniclastic rocks above a prominent angular unconformity. U-Pb dating of detrital zircons from the Late Carboniferous–Lower Permian rocks reveals that most grains are Ordovician in age, ranging between 475–455 Ma. A subordinate population of Silurian detrital zircons is also present, contributing up to 15% of the dated population, while Precambrian grains mainly yield Neo-Mesoproterozoic ages and do not form prominent peaks. The combined U-Pb and (U-Th)/He ages indicate that most zircon (U-Th)/He ages were reset and average at ca. 317 Ma, suggesting ~6–7 km of Late Carboniferous uplift within the provenance area. This provenance area, mainly comprising Ordovician magmatic and volcanic rocks, was located close to the study area based on the coarse-grained nature of Late Carboniferous–Lower Permian rocks of north-eastern October Revolution Island. Therefore, we propose that Late Paleozoic tectonism significantly affected both the southern margin of the Kara terrane, as previously supposed, and also its north-eastern part. We propose that the Late Paleozoic Uralian suture zone continued to the north-eastern October Revolution Island and was responsible for the significant tectonic uplift of the studied region. This suture zone is now hidden beneath the younger Arctic basins. |
format |
Text |
author |
Victoria Ershova Andrei Prokopiev Daniel Stockli Daria Zbukova Anton Shmanyak |
author_facet |
Victoria Ershova Andrei Prokopiev Daniel Stockli Daria Zbukova Anton Shmanyak |
author_sort |
Victoria Ershova |
title |
Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
title_short |
Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
title_full |
Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
title_fullStr |
Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
title_full_unstemmed |
Provenance and Stratigraphy of the Upper Carboniferous—Lower Permian Strata of October Revolution Island (Severnaya Zemlya Archipelago): Implications for Geological History of the Russian High Arctic |
title_sort |
provenance and stratigraphy of the upper carboniferous—lower permian strata of october revolution island (severnaya zemlya archipelago): implications for geological history of the russian high arctic |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2022 |
url |
https://doi.org/10.3390/min12101325 |
op_coverage |
agris |
long_lat |
ENVELOPE(98.000,98.000,79.500,79.500) |
geographic |
Arctic Kara Sea Severnaya Zemlya |
geographic_facet |
Arctic Kara Sea Severnaya Zemlya |
genre |
Arctic Kara Sea October Revolution Island Severnaya Zemlya |
genre_facet |
Arctic Kara Sea October Revolution Island Severnaya Zemlya |
op_source |
Minerals; Volume 12; Issue 10; Pages: 1325 |
op_relation |
Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min12101325 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/min12101325 |
container_title |
Minerals |
container_volume |
12 |
container_issue |
10 |
container_start_page |
1325 |
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1774714551116234752 |