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https://elib.bsu.by/handle/123456789/196608| Title: | Вендский и девонский магматизм юга Восточно-Европейского кратона: геодинамические аспекты |
| Authors: | Айзберг, Р. Е. Гарецкий, Р. Г. Старчик, Т. А. |
| Keywords: | ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геология |
| Issue Date: | 2000 |
| Publisher: | Минск : Універсітэцкае |
| Citation: | Вестник Белорусского государственного университета. Сер. 2, Химия. Биология. География. – 2000. - № 1. – С. 65-71. |
| Abstract: | The Vendian and Devonian magmatic complexes of the region are associated with continental riftinq zones The Pripyat-Donets volcanogenic belt of Devonian age had been developed from the junction of the three-radia rift system as a ray gradually disappearing from east to west. The Volyn volcanites were accumulated along a presumably active ray subparaliel to the spreading axis in the Teisseyre-Tornquist zone. This is responsible for petrochemical differences between the studied ton-nations |
| URI: | http://elib.bsu.by/handle/123456789/196608 |
| ISSN: | 0372-5340 |
| Licence: | info:eu-repo/semantics/openAccess |
| Appears in Collections: | 2000, №1 (февраль) |
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