Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Svir-Oyat paleoseismic event took place in the time interval between 4,5 and 2,0 kyr BP, more likely close to the maximum stage of Late Holocene Ladoga Lake transgression. Seismic structures connected with the earthquake are registered in the 35-km area as I≥8 and in the 50-km area as I≥6 (MSK-64, so magnitude of the event might be more than 6. The seismic event is more likely to be connected with displacement along the side of Pasha-Ladoga paleo-rift (Precambrian) triggered by growing of water mass in Ladoga Lake during the transgression.
Переведенное название | Late Holocene paleoseismic event at southeastern coast of Ladoga Lake. II. Parameters |
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Язык оригинала | русский |
Страницы (с-по) | 18-28 |
Число страниц | 11 |
Журнал | ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ |
Том | 2010 |
Номер выпуска | 3 |
Состояние | Опубликовано - 22 дек 2010 |
ID: 5256806