THE CENTRAL KURIL "GAP": STRUCTURE AND SEISMIC POTENTIAL

Laverov N.P.; Lappo S.S.; Lobkovsky L.I.; Baranov B.V.; Kulinich R.G.; Karp B.Ya.

dc.contributor.author	Laverov N.P.
dc.contributor.author	Lappo S.S.
dc.contributor.author	Lobkovsky L.I.
dc.contributor.author	Baranov B.V.
dc.contributor.author	Kulinich R.G.
dc.contributor.author	Karp B.Ya.
dc.date.accessioned	2024-11-09T08:38:10Z
dc.date.available	2024-11-09T08:38:10Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526133
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 787-790
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46408
dc.description.abstract	The method of revealing probable areas of future strong earthquakes (“seismic gaps”) was first proposed with the Kuril–Kamchatka island arc (KKA). The method is based on the following principle: sources of the strongest (M ≥ 7.7) earthquakes have a significant tendency not to overlap each other. Based on this principle, potential areas of future earthquakes (seismic gaps) were established with a probability of 0.8–0.9. They were located in the south-western, northeastern, and central parts of the arc.
dc.subject	Kuril–Kamchatka island arc
dc.title	THE CENTRAL KURIL "GAP": STRUCTURE AND SEISMIC POTENTIAL
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050254