SOURCE MECHANISM OF THE KALININGRAD EARTHQUAKE ON SEPTEMBER 21, 2004

Nikonov A.A.

dc.contributor.author	Nikonov A.A.
dc.date.accessioned	2024-11-02T11:07:59Z
dc.date.available	2024-11-02T11:07:59Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524334
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 317-320
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46388
dc.description.abstract	The Kaliningrad earthquake on September 21, 2004 was a rare but very significant example of the potential of moderate earthquakes in the East European Platform. The following three shocks were instrumentally recorded with sequential magnitudes mb: 4.1, 4.9, and 3.0 (Geophysical Service of Russia); 4.4 and 5.0 (EMSC); and 4.8 and 4.9 (NEIC).
dc.title	SOURCE MECHANISM OF THE KALININGRAD EARTHQUAKE ON SEPTEMBER 21, 2004
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020371