Relation of Alpine magmatism with structural and fault tectonics of the Carpathians
The Alpine activity cycle of tectonic development of the Carpathians and adjacent TransCarpathian, Pannonian, Transilvanian depressions, Dinarides (Pancardi) was accompanied by active magmatism. Its three main stages have been established: Mesozoic (Т 3-КД, Miocene, and Pliocene-Pleistocene. Thrusti...
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| Дата: | 2011 |
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| Формат: | Стаття |
| Мова: | rus |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2011
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116937 |
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journalsuranua-geofizicheskiy-article-1169372020-10-07T11:01:56Z Relation of Alpine magmatism with structural and fault tectonics of the Carpathians Lyashkevich, Z. M. The Alpine activity cycle of tectonic development of the Carpathians and adjacent TransCarpathian, Pannonian, Transilvanian depressions, Dinarides (Pancardi) was accompanied by active magmatism. Its three main stages have been established: Mesozoic (Т 3-КД, Miocene, and Pliocene-Pleistocene. Thrusting process of the Low Cretaceous - Oligocene produced a folded structure of the Carpathians with numerous allochtonous bodies of Mesozoic magmatic rocks (ophiolite association). The collision stage of the region development, which came in Neogene, is related to intense volcanism of antidrome order indicating the destruction of the continental crust. Coincidence of strikes of principal fractures and the areas of volcanites development is a characteristic feature. Finally, the third phase of alkali-basaltoid volcanites of Pancardi has manifested itself in connection with intra-plate rupturing tectonics of the continents. Volcanites are of the mantle - plume genesis. Subbotin Institute of Geophysics of the NAS of Ukraine 2011-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116937 10.24028/gzh.0203-3100.v33i3.2011.116937 Geofizicheskiy Zhurnal; Vol. 33 No. 3 (2011); 144-150 Геофизический журнал; Том 33 № 3 (2011); 144-150 Геофізичний журнал; Том 33 № 3 (2011); 144-150 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116937/110996 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| format |
Article |
| author |
Lyashkevich, Z. M. |
| spellingShingle |
Lyashkevich, Z. M. Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| author_facet |
Lyashkevich, Z. M. |
| author_sort |
Lyashkevich, Z. M. |
| title |
Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| title_short |
Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| title_full |
Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| title_fullStr |
Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| title_full_unstemmed |
Relation of Alpine magmatism with structural and fault tectonics of the Carpathians |
| title_sort |
relation of alpine magmatism with structural and fault tectonics of the carpathians |
| description |
The Alpine activity cycle of tectonic development of the Carpathians and adjacent TransCarpathian, Pannonian, Transilvanian depressions, Dinarides (Pancardi) was accompanied by active magmatism. Its three main stages have been established: Mesozoic (Т 3-КД, Miocene, and Pliocene-Pleistocene. Thrusting process of the Low Cretaceous - Oligocene produced a folded structure of the Carpathians with numerous allochtonous bodies of Mesozoic magmatic rocks (ophiolite association). The collision stage of the region development, which came in Neogene, is related to intense volcanism of antidrome order indicating the destruction of the continental crust. Coincidence of strikes of principal fractures and the areas of volcanites development is a characteristic feature. Finally, the third phase of alkali-basaltoid volcanites of Pancardi has manifested itself in connection with intra-plate rupturing tectonics of the continents. Volcanites are of the mantle - plume genesis. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2011 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/116937 |
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2024-04-21T19:41:35Z |
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