Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians)
The data on surface, subsurface and deep structure of the Pieniny Klippen Belt (PKB) have been summarized and new results of its geological-structural and fault kinematic studies within the Ukrainian part of the Eastern Carpathians have been presented. In its contemporary appearance as a narrow stro...
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| Дата: | 2016 |
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| Автори: | , , , , , |
| Формат: | Стаття |
| Мова: | Російська |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/107826 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543130244874240 |
|---|---|
| author | Murovskaya, A. V. Nakapelyukh, M. V. Vikhot, Yu. M. Shlapinskiy, V. E. Bubnyak, I. N. Mychak, S. V. |
| author_facet | Murovskaya, A. V. Nakapelyukh, M. V. Vikhot, Yu. M. Shlapinskiy, V. E. Bubnyak, I. N. Mychak, S. V. |
| author_sort | Murovskaya, A. V. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:19:44Z |
| description | The data on surface, subsurface and deep structure of the Pieniny Klippen Belt (PKB) have been summarized and new results of its geological-structural and fault kinematic studies within the Ukrainian part of the Eastern Carpathians have been presented. In its contemporary appearance as a narrow strongly tectonized zone between the Outer Carpathians and Trans-Carpathian trough PKB was formed in Oligocene—Miocene in the place of ancient ocean. On the surface it is situated within the rootless Pieniny nappe and in the deep it is a steeply dipping deformation zone which developed under compression, simple dextral strike-slip, transtension and transpression. Mesostructures of horizontal shortening and vertical elongation, thrusts and thrust-related folds as well as structures of lateral extrusion — dextral strike-slip along sub-meridional slicken-sides correspond to SW—NE 220° trending compression and correlate with the stage of Alcapa microplate progression in NE direction in Oligocene—Early Miocene. In Early Miocene as a result of counter-clockwork rotation of Alcapa dextral strike-slip deformation is concentrated in boundary zone between Alcapa and accretionary prism of Ukrainian Flysch Carpathians. The stress fields of strike-slip type with orientation of compression axis SE 165—SW 215° and its “rotation” in a zone of simple shear correspond to this stage. Present deformation regime is characterized as transpressure with SW—NE orientation of compression axis. |
| first_indexed | 2025-07-17T11:05:01Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-107826 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:01Z |
| publishDate | 2016 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1078262020-10-07T11:19:44Z Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) Murovskaya, A. V. Nakapelyukh, M. V. Vikhot, Yu. M. Shlapinskiy, V. E. Bubnyak, I. N. Mychak, S. V. Ukrainian Carpathians Pieniny nappe Pennine Klippen Belt kinematic analysis stress fields deformational regime The data on surface, subsurface and deep structure of the Pieniny Klippen Belt (PKB) have been summarized and new results of its geological-structural and fault kinematic studies within the Ukrainian part of the Eastern Carpathians have been presented. In its contemporary appearance as a narrow strongly tectonized zone between the Outer Carpathians and Trans-Carpathian trough PKB was formed in Oligocene—Miocene in the place of ancient ocean. On the surface it is situated within the rootless Pieniny nappe and in the deep it is a steeply dipping deformation zone which developed under compression, simple dextral strike-slip, transtension and transpression. Mesostructures of horizontal shortening and vertical elongation, thrusts and thrust-related folds as well as structures of lateral extrusion — dextral strike-slip along sub-meridional slicken-sides correspond to SW—NE 220° trending compression and correlate with the stage of Alcapa microplate progression in NE direction in Oligocene—Early Miocene. In Early Miocene as a result of counter-clockwork rotation of Alcapa dextral strike-slip deformation is concentrated in boundary zone between Alcapa and accretionary prism of Ukrainian Flysch Carpathians. The stress fields of strike-slip type with orientation of compression axis SE 165—SW 215° and its “rotation” in a zone of simple shear correspond to this stage. Present deformation regime is characterized as transpressure with SW—NE orientation of compression axis. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/107826 10.24028/gzh.0203-3100.v38i5.2016.107826 Geofizicheskiy Zhurnal; Vol. 38 No. 5 (2016); 119-136 Геофизический журнал; Том 38 № 5 (2016); 119-136 Геофізичний журнал; Том 38 № 5 (2016); 119-136 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/107826/102775 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Ukrainian Carpathians Pieniny nappe Pennine Klippen Belt kinematic analysis stress fields deformational regime Murovskaya, A. V. Nakapelyukh, M. V. Vikhot, Yu. M. Shlapinskiy, V. E. Bubnyak, I. N. Mychak, S. V. Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title | Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title_full | Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title_fullStr | Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title_full_unstemmed | Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title_short | Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians) |
| title_sort | kinematic evolution of the pieniny klippen belt in cenozoic (ukrainian carpathians) |
| topic | Ukrainian Carpathians Pieniny nappe Pennine Klippen Belt kinematic analysis stress fields deformational regime |
| topic_facet | Ukrainian Carpathians Pieniny nappe Pennine Klippen Belt kinematic analysis stress fields deformational regime |
| url | https://journals.uran.ua/geofizicheskiy/article/view/107826 |
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