Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The interrelation of vulcanites with bedding granitoids in the north-east bank of the Lekhtin structure (Northern Karelia) are described. The conducted investigation shows that in the base of the Okhtinsk strata cut the ultrabasic komatiite-series metamorpihzed vulcanites are bedding. For the first time at the Baltic craton the direct interrelations of lopian volcanic-origin-sedimentary complex of greenstone belts with the basement gneiss-granitoids are established, which are expressed by the weathering profile with the age 2.8 mlrd. years.
Язык оригинала | английский |
---|---|
Страницы (с-по) | 83-87 |
Число страниц | 5 |
Журнал | Doklady Akademii Nauk |
Том | 400 |
Номер выпуска | 1 |
Состояние | Опубликовано - 21 сен 2005 |
ID: 41539338