Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield)
New geological and petrological data are presented for the Precambrian eclogites of Gridino area, Belomorian Province. The detailed optical and microprobe studies of eclogites in the Samylino locality allow distinguishing the essential features of eclogitic metamorphism in this area. The early stage...
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ftdoajarticles:oai:doaj.org/article:25adba46b29b4aefa180746ef402954b 2023-05-15T16:12:58+02:00 Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) Олег Александрович Максимов Oleg Maksimov 2019-03-01T00:00:00Z https://doi.org/10.17076/geo958 https://doaj.org/article/25adba46b29b4aefa180746ef402954b EN RU eng rus Karelian Research Centre of the Russian Academy of Sciences http://journals.krc.karelia.ru/index.php/precambrian/article/view/958 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/geo958 https://doaj.org/article/25adba46b29b4aefa180746ef402954b Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 2 (2019) эклогит метаморфизм докембрий беломорская провинция феносканднавский щит Science Q article 2019 ftdoajarticles https://doi.org/10.17076/geo958 2022-12-31T11:41:47Z New geological and petrological data are presented for the Precambrian eclogites of Gridino area, Belomorian Province. The detailed optical and microprobe studies of eclogites in the Samylino locality allow distinguishing the essential features of eclogitic metamorphism in this area. The early stage of high-pressure metamorphism in this tholeiitic series mafic rocks is recognized by the presence of diopside-plagioclase symplectitic inclusions (symplectites I) in the central parts of large omphacite (jadeite 30–35 %) crystals and in the cores of zoned garnet grains. The eclogitic metamorphism is distinguished by omphacite in the matrix and its inclusions in the garnet (pyrope 27–30 %, almandin 48–52 %, grossular 19–23 %) inner zones. The high-pressure amphibolite facies overprinting is represented by garnet rims (pyrope 22–24 %, almandin 52–56 %, grossular 22 %) and diopside-plagioklase (± hornblende) symplectites II. These data suggest a two-stage character of eclogitic metamorphism in Gridino area. Article in Journal/Newspaper Fennoscandian Directory of Open Access Journals: DOAJ Articles Gridino ENVELOPE(34.675,34.675,65.923,65.923) Proceedings of the Karelian Research Centre of the Russian Academy of Sciences 2 88 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English Russian |
topic |
эклогит метаморфизм докембрий беломорская провинция феносканднавский щит Science Q |
spellingShingle |
эклогит метаморфизм докембрий беломорская провинция феносканднавский щит Science Q Олег Александрович Максимов Oleg Maksimov Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
topic_facet |
эклогит метаморфизм докембрий беломорская провинция феносканднавский щит Science Q |
description |
New geological and petrological data are presented for the Precambrian eclogites of Gridino area, Belomorian Province. The detailed optical and microprobe studies of eclogites in the Samylino locality allow distinguishing the essential features of eclogitic metamorphism in this area. The early stage of high-pressure metamorphism in this tholeiitic series mafic rocks is recognized by the presence of diopside-plagioclase symplectitic inclusions (symplectites I) in the central parts of large omphacite (jadeite 30–35 %) crystals and in the cores of zoned garnet grains. The eclogitic metamorphism is distinguished by omphacite in the matrix and its inclusions in the garnet (pyrope 27–30 %, almandin 48–52 %, grossular 19–23 %) inner zones. The high-pressure amphibolite facies overprinting is represented by garnet rims (pyrope 22–24 %, almandin 52–56 %, grossular 22 %) and diopside-plagioklase (± hornblende) symplectites II. These data suggest a two-stage character of eclogitic metamorphism in Gridino area. |
format |
Article in Journal/Newspaper |
author |
Олег Александрович Максимов Oleg Maksimov |
author_facet |
Олег Александрович Максимов Oleg Maksimov |
author_sort |
Олег Александрович Максимов |
title |
Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
title_short |
Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
title_full |
Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
title_fullStr |
Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
title_full_unstemmed |
Geology and petrology of eclogites in the Samylino area (Belomorian Province of the Fennoscandian Shield) |
title_sort |
geology and petrology of eclogites in the samylino area (belomorian province of the fennoscandian shield) |
publisher |
Karelian Research Centre of the Russian Academy of Sciences |
publishDate |
2019 |
url |
https://doi.org/10.17076/geo958 https://doaj.org/article/25adba46b29b4aefa180746ef402954b |
long_lat |
ENVELOPE(34.675,34.675,65.923,65.923) |
geographic |
Gridino |
geographic_facet |
Gridino |
genre |
Fennoscandian |
genre_facet |
Fennoscandian |
op_source |
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 2 (2019) |
op_relation |
http://journals.krc.karelia.ru/index.php/precambrian/article/view/958 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/geo958 https://doaj.org/article/25adba46b29b4aefa180746ef402954b |
op_doi |
https://doi.org/10.17076/geo958 |
container_title |
Proceedings of the Karelian Research Centre of the Russian Academy of Sciences |
container_issue |
2 |
container_start_page |
88 |
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1765998575319252992 |