Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA
The Nyasyukka dike complex forms a NW-trending dike swarm in the Archean bedrock of the Murmansk Province adjacent to the Pechenga Complex. The dikes are mostly composed of two rock types, kaersutite-bearing peridotites and olivine gabbros. Also a rounded pyroxenite stock has been found in the area....
Published in: | Proceedings of the Karelian Research Centre of the Russian Academy of Sciences |
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Karelian Research Centre of the Russian Academy of Sciences
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Online Access: | https://doi.org/10.17076/geo164 https://doaj.org/article/7cb9b66c33cd48d484984666342c45be |
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ftdoajarticles:oai:doaj.org/article:7cb9b66c33cd48d484984666342c45be 2023-05-15T17:04:59+02:00 Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA Валерий Федорович Смолькин Ееро Хански Ханну Хухма Жорж Александрович Федотов Valery Smolkin Eero Hanski Hannu Huhma Zhorzh Fedotov 2015-06-01T00:00:00Z https://doi.org/10.17076/geo164 https://doaj.org/article/7cb9b66c33cd48d484984666342c45be EN RU eng rus Karelian Research Centre of the Russian Academy of Sciences http://journals.krc.karelia.ru/index.php/precambrian/article/view/164 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/geo164 https://doaj.org/article/7cb9b66c33cd48d484984666342c45be Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 7, Pp 74-84 (2015) палеопротерозойская печенгская структура дайковый комплекс перидотитов-оливиновых габбро sm-nd и u-pb изотопные данные бадделеит циркон Science Q article 2015 ftdoajarticles https://doi.org/10.17076/geo164 2022-12-31T05:50:09Z The Nyasyukka dike complex forms a NW-trending dike swarm in the Archean bedrock of the Murmansk Province adjacent to the Pechenga Complex. The dikes are mostly composed of two rock types, kaersutite-bearing peridotites and olivine gabbros. Also a rounded pyroxenite stock has been found in the area. The dikes were generated from ferropicritic parental magma which was similar to Pechenga ferropicrites though having a somewhat higher silica activity. A peridotite sample yielded an internal Sm-Nd isochron with an age of 1956 ± 19 Ma (MSWD = 0.7) and an initial 6 Nd value of +1.4 ± 0.4. This is consistent with the baddeleyite age of 1941 ± 3 Ma, showing that the Nyasyukka dikes are ca. 40 Ma younger than the Pechenga ferropicrites. The pyroxenite stock shows geochemical and Nd isotopic evidence for significant crustal contamination. We also present isotopic and geochemical data for olivine gabbro-norite from the Tuloma River area, supporting the earlier view that there exist dikes of the Nyasyukka type in this area. Article in Journal/Newspaper kola peninsula Directory of Open Access Journals: DOAJ Articles Kola Peninsula Murmansk Pechenga ENVELOPE(30.989,30.989,69.401,69.401) Tuloma ENVELOPE(32.687,32.687,68.816,68.816) Proceedings of the Karelian Research Centre of the Russian Academy of Sciences 7 74 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
палеопротерозойская печенгская структура дайковый комплекс перидотитов-оливиновых габбро sm-nd и u-pb изотопные данные бадделеит циркон Science Q |
spellingShingle |
палеопротерозойская печенгская структура дайковый комплекс перидотитов-оливиновых габбро sm-nd и u-pb изотопные данные бадделеит циркон Science Q Валерий Федорович Смолькин Ееро Хански Ханну Хухма Жорж Александрович Федотов Valery Smolkin Eero Hanski Hannu Huhma Zhorzh Fedotov Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
topic_facet |
палеопротерозойская печенгская структура дайковый комплекс перидотитов-оливиновых габбро sm-nd и u-pb изотопные данные бадделеит циркон Science Q |
description |
The Nyasyukka dike complex forms a NW-trending dike swarm in the Archean bedrock of the Murmansk Province adjacent to the Pechenga Complex. The dikes are mostly composed of two rock types, kaersutite-bearing peridotites and olivine gabbros. Also a rounded pyroxenite stock has been found in the area. The dikes were generated from ferropicritic parental magma which was similar to Pechenga ferropicrites though having a somewhat higher silica activity. A peridotite sample yielded an internal Sm-Nd isochron with an age of 1956 ± 19 Ma (MSWD = 0.7) and an initial 6 Nd value of +1.4 ± 0.4. This is consistent with the baddeleyite age of 1941 ± 3 Ma, showing that the Nyasyukka dikes are ca. 40 Ma younger than the Pechenga ferropicrites. The pyroxenite stock shows geochemical and Nd isotopic evidence for significant crustal contamination. We also present isotopic and geochemical data for olivine gabbro-norite from the Tuloma River area, supporting the earlier view that there exist dikes of the Nyasyukka type in this area. |
format |
Article in Journal/Newspaper |
author |
Валерий Федорович Смолькин Ееро Хански Ханну Хухма Жорж Александрович Федотов Valery Smolkin Eero Hanski Hannu Huhma Zhorzh Fedotov |
author_facet |
Валерий Федорович Смолькин Ееро Хански Ханну Хухма Жорж Александрович Федотов Valery Smolkin Eero Hanski Hannu Huhma Zhorzh Fedotov |
author_sort |
Валерий Федорович Смолькин |
title |
Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
title_short |
Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
title_full |
Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
title_fullStr |
Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
title_full_unstemmed |
Sm-Nd AND U-Pb ISOTOPIC STUDY OF THE NYASYUKKA DIKE COMPLEX, KOLA PENINSULA, RUSSIA |
title_sort |
sm-nd and u-pb isotopic study of the nyasyukka dike complex, kola peninsula, russia |
publisher |
Karelian Research Centre of the Russian Academy of Sciences |
publishDate |
2015 |
url |
https://doi.org/10.17076/geo164 https://doaj.org/article/7cb9b66c33cd48d484984666342c45be |
long_lat |
ENVELOPE(30.989,30.989,69.401,69.401) ENVELOPE(32.687,32.687,68.816,68.816) |
geographic |
Kola Peninsula Murmansk Pechenga Tuloma |
geographic_facet |
Kola Peninsula Murmansk Pechenga Tuloma |
genre |
kola peninsula |
genre_facet |
kola peninsula |
op_source |
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 7, Pp 74-84 (2015) |
op_relation |
http://journals.krc.karelia.ru/index.php/precambrian/article/view/164 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/geo164 https://doaj.org/article/7cb9b66c33cd48d484984666342c45be |
op_doi |
https://doi.org/10.17076/geo164 |
container_title |
Proceedings of the Karelian Research Centre of the Russian Academy of Sciences |
container_issue |
7 |
container_start_page |
74 |
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1766059359168626688 |