STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION

<span lang="EN-US">The tectonites confined to fault zones with abnormally high, up to 12 kbar, pressures, which appear to be the products of stress-metamorphism of relatively late stage of deformation-metamorphic evolution, are identified in the regionally metamorphosed Precambrian r...

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Main Authors: Алексей Львович Кулаковский, Юрий Алексеевич Морозов, Анна Игоревна Смульская, Alexey Kulakovsky, Yury Morozov, Anna Smul'skaya
Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2015-06-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
Online Access:http://journals.krc.karelia.ru/index.php/precambrian/article/view/159
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author Алексей Львович Кулаковский
Юрий Алексеевич Морозов
Анна Игоревна Смульская
Alexey Kulakovsky
Yury Morozov
Anna Smul'skaya
author_facet Алексей Львович Кулаковский
Юрий Алексеевич Морозов
Анна Игоревна Смульская
Alexey Kulakovsky
Yury Morozov
Anna Smul'skaya
author_sort Алексей Львович Кулаковский
collection DOAJ
description <span lang="EN-US">The tectonites confined to fault zones with abnormally high, up to 12 kbar, pressures, which appear to be the products of stress-metamorphism of relatively late stage of deformation-metamorphic evolution, are identified in the regionally metamorphosed Precambrian rocks of the Ladoga region. Most of these stress-metamorphites are localized in the Meyeri tectonic zone, separating the Svecofennian and Karelian geoblocks. The features of structure and composition of the two groups of stress-metamorphites belonging to the different stages of the deformation-metamorphic phase are described. Some parameters and trends in stress-metamorphism of each stage are defined.</span>
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spelling doaj.art-ed830d8d30b14435b0ad6ff6739b03c82022-12-22T02:39:48ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042015-06-0107193510.17076/geo15979STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGIONАлексей Львович КулаковскийЮрий Алексеевич МорозовАнна Игоревна СмульскаяAlexey KulakovskyYury MorozovAnna Smul'skaya<span lang="EN-US">The tectonites confined to fault zones with abnormally high, up to 12 kbar, pressures, which appear to be the products of stress-metamorphism of relatively late stage of deformation-metamorphic evolution, are identified in the regionally metamorphosed Precambrian rocks of the Ladoga region. Most of these stress-metamorphites are localized in the Meyeri tectonic zone, separating the Svecofennian and Karelian geoblocks. The features of structure and composition of the two groups of stress-metamorphites belonging to the different stages of the deformation-metamorphic phase are described. Some parameters and trends in stress-metamorphism of each stage are defined.</span>http://journals.krc.karelia.ru/index.php/precambrian/article/view/159стрессметаморфизмприладожье
spellingShingle Алексей Львович Кулаковский
Юрий Алексеевич Морозов
Анна Игоревна Смульская
Alexey Kulakovsky
Yury Morozov
Anna Smul'skaya
STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
Transactions of the Karelian Research Centre of the Russian Academy of Sciences
стресс
метаморфизм
приладожье
title STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
title_full STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
title_fullStr STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
title_full_unstemmed STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
title_short STRESS-METAMORPHISM AND STRESS-METAMORPHITES IN PRECAMBRIAN OF THE LADOGA REGION
title_sort stress metamorphism and stress metamorphites in precambrian of the ladoga region
topic стресс
метаморфизм
приладожье
url http://journals.krc.karelia.ru/index.php/precambrian/article/view/159
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