THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION
Many mobile belts contain narrow (a few kilometres wide) and elongated (several hundreds and thousands kilometres long) zones characterized by complicated tectonic interiors and intensive rock metamorphism. Such zones are important components of the crustal structure; they determine the internal div...
| Published in: | Геодинамика и тектонофизика |
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| Main Author: | |
| Format: | Article |
| Language: | English |
| Published: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2015-09-01
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| Subjects: | |
| Online Access: | https://www.gt-crust.ru/jour/article/view/9 |
| _version_ | 1849502408845033472 |
|---|---|
| author | M. G. Leonov |
| author_facet | M. G. Leonov |
| author_sort | M. G. Leonov |
| collection | DOAJ |
| container_title | Геодинамика и тектонофизика |
| description | Many mobile belts contain narrow (a few kilometres wide) and elongated (several hundreds and thousands kilometres long) zones characterized by complicated tectonic interiors and intensive rock metamorphism. Such zones are important components of the crustal structure; they determine the internal divisibility of the crust and act as accommodation areas or buffers between fragments of the crust which differ in origin and have specific evolution features. The article describes the paleo-evolution and characteristics of the Pieniny klippen belt, a major tectonic structure of the Carpathians and one of the largest linear tectonic zones in the Alpine-Himalayan folded belt. |
| format | Article |
| id | doaj-art-ee395b3788674c8a9ef0fb9dc1cd79f6 |
| institution | Directory of Open Access Journals |
| issn | 2078-502X |
| language | English |
| publishDate | 2015-09-01 |
| publisher | Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
| record_format | Article |
| spelling | doaj-art-ee395b3788674c8a9ef0fb9dc1cd79f62025-08-20T03:02:21ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2015-09-015370371510.5800/GT-2014-5-3-01509THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTIONM. G. Leonov0Geological Institute of RAS, Moscow, RussiaMany mobile belts contain narrow (a few kilometres wide) and elongated (several hundreds and thousands kilometres long) zones characterized by complicated tectonic interiors and intensive rock metamorphism. Such zones are important components of the crustal structure; they determine the internal divisibility of the crust and act as accommodation areas or buffers between fragments of the crust which differ in origin and have specific evolution features. The article describes the paleo-evolution and characteristics of the Pieniny klippen belt, a major tectonic structure of the Carpathians and one of the largest linear tectonic zones in the Alpine-Himalayan folded belt.https://www.gt-crust.ru/jour/article/view/9tectonicsdeformationtectonic flowfolded beltflower-type structurepieniny klippen belt |
| spellingShingle | M. G. Leonov THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION tectonics deformation tectonic flow folded belt flower-type structure pieniny klippen belt |
| title | THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION |
| title_full | THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION |
| title_fullStr | THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION |
| title_full_unstemmed | THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION |
| title_short | THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION |
| title_sort | pieniny klippen belt its tectonic structure and evolution |
| topic | tectonics deformation tectonic flow folded belt flower-type structure pieniny klippen belt |
| url | https://www.gt-crust.ru/jour/article/view/9 |
| work_keys_str_mv | AT mgleonov thepieninyklippenbeltitstectonicstructureandevolution AT mgleonov pieninyklippenbeltitstectonicstructureandevolution |