THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS

The article presents results of field studies and interpretation of tectonophysical data from profiles in the valleys of Bystritsa Nadvornyanskaya, Prut, Pistynka (the right-side tributary of the Prut river), Belyi and Chernyi Cheremosh, and Seret rivers. The stress fields reconstructed from differe...

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Main Authors: I. M. Bubniak, Yu. M. Vikhot, M. V. Nakapelyukh
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Series:Геодинамика и тектонофизика
Subjects:
Online Access:https://www.gt-crust.ru/jour/article/view/65
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author I. M. Bubniak
Yu. M. Vikhot
M. V. Nakapelyukh
author_facet I. M. Bubniak
Yu. M. Vikhot
M. V. Nakapelyukh
author_sort I. M. Bubniak
collection DOAJ
description The article presents results of field studies and interpretation of tectonophysical data from profiles in the valleys of Bystritsa Nadvornyanskaya, Prut, Pistynka (the right-side tributary of the Prut river), Belyi and Chernyi Cheremosh, and Seret rivers. The stress fields reconstructed from different groups of joints and slickensides in flysch and molasse sediments of the Skyba and Boryslav-Pokuttya nappes are analyzed.A combination of the structural-paragenesis and kinematic analysis methods provided for determination of deformation modes, their sequences, and  average azimuth values of orientations of the principal axes of regional paleostress fields (σ1, σ2, σ3) which were manifested through the Alpine stage of the Ukrainian Carpathians development.The paleostress fields were reconstructed for the south-eastern part of the Skyba nappe of the Ukrainian Carpathians and the Boryslav-Pokuttya nappe of the Carpathian foretrough. The article describes similarities and differences in the stress-and-strain states, specific features of the paleostress fields, and the ratio of joints in different groups (oblique and perpendicular to the rock layers) and slickensides in the area under study.
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series Геодинамика и тектонофизика
spelling doaj-art-5cd2083268dc48dbb71038ad9dd620c52025-08-20T03:59:45ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2015-09-014331332610.5800/GT-2013-4-3-010365THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANSI. M. Bubniak0Yu. M. Vikhot1M. V. Nakapelyukh2Ivan Franko National University of Lviv, Department of Geology, Lviv, UkraineIvan Franko National University of Lviv, Department of Geology, Lviv, UkraineS.I. Subbotin Institute of Geophysics, NAS of Ukraine, Kyiv, UkraineThe article presents results of field studies and interpretation of tectonophysical data from profiles in the valleys of Bystritsa Nadvornyanskaya, Prut, Pistynka (the right-side tributary of the Prut river), Belyi and Chernyi Cheremosh, and Seret rivers. The stress fields reconstructed from different groups of joints and slickensides in flysch and molasse sediments of the Skyba and Boryslav-Pokuttya nappes are analyzed.A combination of the structural-paragenesis and kinematic analysis methods provided for determination of deformation modes, their sequences, and  average azimuth values of orientations of the principal axes of regional paleostress fields (σ1, σ2, σ3) which were manifested through the Alpine stage of the Ukrainian Carpathians development.The paleostress fields were reconstructed for the south-eastern part of the Skyba nappe of the Ukrainian Carpathians and the Boryslav-Pokuttya nappe of the Carpathian foretrough. The article describes similarities and differences in the stress-and-strain states, specific features of the paleostress fields, and the ratio of joints in different groups (oblique and perpendicular to the rock layers) and slickensides in the area under study.https://www.gt-crust.ru/jour/article/view/65ukrainian carpathiansskyba nappeboryslav-pokuttya nappeevolution of palaeostress fieldsdeformation modejointslickenside
spellingShingle I. M. Bubniak
Yu. M. Vikhot
M. V. Nakapelyukh
THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
Геодинамика и тектонофизика
ukrainian carpathians
skyba nappe
boryslav-pokuttya nappe
evolution of palaeostress fields
deformation mode
joint
slickenside
title THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
title_full THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
title_fullStr THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
title_full_unstemmed THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
title_short THE STRESS-AND-STRAIN STATE OF THE SOUTH-EASTERN PART OF THE SKYBA AND BORYSLAV-POKUTTYA NAPPES OF THE UKRAINIAN CARPATHIANS
title_sort stress and strain state of the south eastern part of the skyba and boryslav pokuttya nappes of the ukrainian carpathians
topic ukrainian carpathians
skyba nappe
boryslav-pokuttya nappe
evolution of palaeostress fields
deformation mode
joint
slickenside
url https://www.gt-crust.ru/jour/article/view/65
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