Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent

The paper presents the calculation of modern tectonic flow fields in the Yenisei Ridge located on the stable Siberian Craton. At the first stage, we solve the problem of calculating the average field of tectonic flows due to collisional processes at the southern and northeastern margins of the Euras...

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Main Authors: Ayan Zh. Akhmetov, Igor Yu. Smolin, Aleksey Yu. Peryshkin
Format: Article
Language:English
Published: Gruppo Italiano Frattura 2019-07-01
Series:Frattura ed Integrità Strutturale
Subjects:
Online Access:https://www.fracturae.com/index.php/fis/article/view/2475/2533
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spelling doaj-31c398141bdc4af496d86fe7049bd0692020-11-25T00:50:11ZengGruppo Italiano FratturaFrattura ed Integrità Strutturale1971-89932019-07-01134919020010.3221/IGF-ESIS.49.2010.3221/IGF-ESIS.49.20Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continentAyan Zh. AkhmetovIgor Yu. SmolinAleksey Yu. PeryshkinThe paper presents the calculation of modern tectonic flow fields in the Yenisei Ridge located on the stable Siberian Craton. At the first stage, we solve the problem of calculating the average field of tectonic flows due to collisional processes at the southern and northeastern margins of the Eurasian Plate with Indian and Arabian and with North American plates, respectively. These calculations clarify the state of stress and the structure of tectonic flows on the territory of the Siberian Craton. The subtraction of the average displacements of the Siberian Craton as a whole in the northeast direction reveals the detailed structure of tectonic flows. Structural models are built along the Batolit-1982 and Shpat geological profiles crossing the Yenisei Ridge. At the second stage, we numerically study the state of stress and strain along these profiles determined by the global tectonics of Central and Southeast Asia, as well as their structural organization and interaction with the neighboring crustal elements.https://www.fracturae.com/index.php/fis/article/view/2475/2533Tectonic flowCollisionGeological cross-sectionState of stress and strainNumerical modelling
collection DOAJ
language English
format Article
sources DOAJ
author Ayan Zh. Akhmetov
Igor Yu. Smolin
Aleksey Yu. Peryshkin
spellingShingle Ayan Zh. Akhmetov
Igor Yu. Smolin
Aleksey Yu. Peryshkin
Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
Frattura ed Integrità Strutturale
Tectonic flow
Collision
Geological cross-section
State of stress and strain
Numerical modelling

author_facet Ayan Zh. Akhmetov
Igor Yu. Smolin
Aleksey Yu. Peryshkin
author_sort Ayan Zh. Akhmetov
title Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
title_short Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
title_full Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
title_fullStr Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
title_full_unstemmed Numerical analysis of the state of stress and strain in the Yenisei Ridge based on the regional tectonic state in the Asian continent
title_sort numerical analysis of the state of stress and strain in the yenisei ridge based on the regional tectonic state in the asian continent
publisher Gruppo Italiano Frattura
series Frattura ed Integrità Strutturale
issn 1971-8993
publishDate 2019-07-01
description The paper presents the calculation of modern tectonic flow fields in the Yenisei Ridge located on the stable Siberian Craton. At the first stage, we solve the problem of calculating the average field of tectonic flows due to collisional processes at the southern and northeastern margins of the Eurasian Plate with Indian and Arabian and with North American plates, respectively. These calculations clarify the state of stress and the structure of tectonic flows on the territory of the Siberian Craton. The subtraction of the average displacements of the Siberian Craton as a whole in the northeast direction reveals the detailed structure of tectonic flows. Structural models are built along the Batolit-1982 and Shpat geological profiles crossing the Yenisei Ridge. At the second stage, we numerically study the state of stress and strain along these profiles determined by the global tectonics of Central and Southeast Asia, as well as their structural organization and interaction with the neighboring crustal elements.
topic Tectonic flow
Collision
Geological cross-section
State of stress and strain
Numerical modelling

url https://www.fracturae.com/index.php/fis/article/view/2475/2533
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