Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians

Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians

New results of interpretation of tectonophysical investigations of the flysh deposits in the Skyba nappe of the Ukrainian Carpathians carried out in four areas in its northwestern and central parts are presented. Complex application of structural - paragenetic and kinematic analyses helped to synchr...

Повний опис

Збережено в:
Бібліографічні деталі
Дата:2011
Автори: Gintov, O.B., Bubnyak, I. N., Vikhot', Yu. M., Murovskaya, A. V., Nakapeluch, M. V.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2011
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116847
Теги: Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
Назва журналу:Geofizicheskiy Zhurnal

Репозитарії

Geofizicheskiy Zhurnal
id journalsuranua-geofizicheskiy-article-116847
record_format ojs
spelling journalsuranua-geofizicheskiy-article-1168472020-10-07T11:02:34Z Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians Gintov, O.B. Bubnyak, I. N. Vikhot', Yu. M. Murovskaya, A. V. Nakapeluch, M. V. New results of interpretation of tectonophysical investigations of the flysh deposits in the Skyba nappe of the Ukrainian Carpathians carried out in four areas in its northwestern and central parts are presented. Complex application of structural - paragenetic and kinematic analyses helped to synchronize three parameters - time of deformation, azimuths of the main axes of stresses orientation and deformation modes for prefolding, folding and postfolding stages of development of the outer part of the Ukrainian Carpathians. It has been proved that thrust shear strain was coeval with strike-slip that provided the rapid advancement of the thrust front. The role of normal faulting with о 3 axis stretching of northeastern and northwestern orientations has been shown. It is assumed that the mentioned deformations had relatively young age. Formation of the Skyba nappe structure is related to the development of the Western and Southern Carpathians. In the global scale the activity of the tangential forces of northwestern and sub-longitudinal directions is explained by the convergence of the Adriatic and European microplates and also the African-Arabian and Eurasian mega-plates. Subbotin Institute of Geophysics of the NAS of Ukraine 2011-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116847 10.24028/gzh.0203-3100.v33i5.2011.116847 Geofizicheskiy Zhurnal; Vol. 33 No. 5 (2011); 17-34 Геофизический журнал; Том 33 № 5 (2011); 17-34 Геофізичний журнал; Том 33 № 5 (2011); 17-34 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116847/110918 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapeluch, M. V.
spellingShingle Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapeluch, M. V.
Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
author_facet Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapeluch, M. V.
author_sort Gintov, O.B.
title Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
title_short Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
title_full Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
title_fullStr Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
title_full_unstemmed Evolution of the stress-strain state and the dynamics of the Skip cover of the Ukrainian Carpathians
title_sort evolution of the stress-strain state and the dynamics of the skip cover of the ukrainian carpathians
description New results of interpretation of tectonophysical investigations of the flysh deposits in the Skyba nappe of the Ukrainian Carpathians carried out in four areas in its northwestern and central parts are presented. Complex application of structural - paragenetic and kinematic analyses helped to synchronize three parameters - time of deformation, azimuths of the main axes of stresses orientation and deformation modes for prefolding, folding and postfolding stages of development of the outer part of the Ukrainian Carpathians. It has been proved that thrust shear strain was coeval with strike-slip that provided the rapid advancement of the thrust front. The role of normal faulting with о 3 axis stretching of northeastern and northwestern orientations has been shown. It is assumed that the mentioned deformations had relatively young age. Formation of the Skyba nappe structure is related to the development of the Western and Southern Carpathians. In the global scale the activity of the tangential forces of northwestern and sub-longitudinal directions is explained by the convergence of the Adriatic and European microplates and also the African-Arabian and Eurasian mega-plates.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2011
url https://journals.uran.ua/geofizicheskiy/article/view/116847
work_keys_str_mv AT gintovob evolutionofthestressstrainstateandthedynamicsoftheskipcoveroftheukrainiancarpathians
AT bubnyakin evolutionofthestressstrainstateandthedynamicsoftheskipcoveroftheukrainiancarpathians
AT vikhotyum evolutionofthestressstrainstateandthedynamicsoftheskipcoveroftheukrainiancarpathians
AT murovskayaav evolutionofthestressstrainstateandthedynamicsoftheskipcoveroftheukrainiancarpathians
AT nakapeluchmv evolutionofthestressstrainstateandthedynamicsoftheskipcoveroftheukrainiancarpathians
first_indexed 2024-04-21T19:41:26Z
last_indexed 2024-04-21T19:41:26Z
_version_ 1796974561911111680

Схожі ресурси