New Data on the Basement of Franz Josef Land, Arctic Region

We have studied pebbles of igneous rocks from the Lower Jurassic sedimentary succession of Hall Island, Franz Josef Land. Pebbles are represented by felsic intrusive and extrusive rocks, often cataclased and greisenized. The U–Pb age of crystallization for zircons of the studied samples yielded the...

Full description

Bibliographic Details
Main Author: Ершова, Виктория Бэртовна
Format: Article in Journal/Newspaper
Language:English
Published: Pleiades Publishing, Ltd 2017
Subjects:
Online Access:http://hdl.handle.net/11701/19289
id ftstpetersburgun:oai:dspace.spbu.ru:11701/19289
record_format openpolar
spelling ftstpetersburgun:oai:dspace.spbu.ru:11701/19289 2023-05-15T14:59:39+02:00 New Data on the Basement of Franz Josef Land, Arctic Region Ершова, Виктория Бэртовна 2017 http://hdl.handle.net/11701/19289 en eng Pleiades Publishing, Ltd http://hdl.handle.net/11701/19289 Article 2017 ftstpetersburgun 2020-09-14T23:50:15Z We have studied pebbles of igneous rocks from the Lower Jurassic sedimentary succession of Hall Island, Franz Josef Land. Pebbles are represented by felsic intrusive and extrusive rocks, often cataclased and greisenized. The U–Pb age of crystallization for zircons of the studied samples yielded the Latest Devonian– Early Carboniferous and Early–Middle Permian ages. In addition, the studied zircons demonstrate a broad scatter of ages, from Middle Paleozoic to Mesozoic, suggesting repeated thermal reworking and metamorphism of granites. It is shown that coeval Late Paleozoic magmatism indicates the similarity of the geological evolution of the northern Barents Sea and the Severnaya Zemlya archipelago. Article in Journal/Newspaper Arctic Barents Sea Franz Josef Land Severnaya Zemlya Saint Petersburg State University: Research Repository (DSpace SPbU) Arctic Barents Sea Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) Hall Island ENVELOPE(-38.133,-38.133,-54.000,-54.000)
institution Open Polar
collection Saint Petersburg State University: Research Repository (DSpace SPbU)
op_collection_id ftstpetersburgun
language English
description We have studied pebbles of igneous rocks from the Lower Jurassic sedimentary succession of Hall Island, Franz Josef Land. Pebbles are represented by felsic intrusive and extrusive rocks, often cataclased and greisenized. The U–Pb age of crystallization for zircons of the studied samples yielded the Latest Devonian– Early Carboniferous and Early–Middle Permian ages. In addition, the studied zircons demonstrate a broad scatter of ages, from Middle Paleozoic to Mesozoic, suggesting repeated thermal reworking and metamorphism of granites. It is shown that coeval Late Paleozoic magmatism indicates the similarity of the geological evolution of the northern Barents Sea and the Severnaya Zemlya archipelago.
format Article in Journal/Newspaper
author Ершова, Виктория Бэртовна
spellingShingle Ершова, Виктория Бэртовна
New Data on the Basement of Franz Josef Land, Arctic Region
author_facet Ершова, Виктория Бэртовна
author_sort Ершова, Виктория Бэртовна
title New Data on the Basement of Franz Josef Land, Arctic Region
title_short New Data on the Basement of Franz Josef Land, Arctic Region
title_full New Data on the Basement of Franz Josef Land, Arctic Region
title_fullStr New Data on the Basement of Franz Josef Land, Arctic Region
title_full_unstemmed New Data on the Basement of Franz Josef Land, Arctic Region
title_sort new data on the basement of franz josef land, arctic region
publisher Pleiades Publishing, Ltd
publishDate 2017
url http://hdl.handle.net/11701/19289
long_lat ENVELOPE(55.000,55.000,81.000,81.000)
ENVELOPE(98.000,98.000,79.500,79.500)
ENVELOPE(-38.133,-38.133,-54.000,-54.000)
geographic Arctic
Barents Sea
Franz Josef Land
Severnaya Zemlya
Hall Island
geographic_facet Arctic
Barents Sea
Franz Josef Land
Severnaya Zemlya
Hall Island
genre Arctic
Barents Sea
Franz Josef Land
Severnaya Zemlya
genre_facet Arctic
Barents Sea
Franz Josef Land
Severnaya Zemlya
op_relation http://hdl.handle.net/11701/19289
_version_ 1766331759446720512