WHERE AND HOW DID THE RUPTURES OF DECEMBER 26, 2004 AND MARCH 28, 2005 EARTHQUAKES NEAR SUMATRA ORIGINATE?

Mukhamediev Sh.A.; Galybin A.N.

dc.contributor.author	Mukhamediev Sh.A.
dc.contributor.author	Galybin A.N.
dc.date.accessioned	2024-11-09T08:38:17Z
dc.date.available	2024-11-09T08:38:17Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13527416
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 52-55
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46432
dc.description.abstract	The earthquakes of December 26, 2004, (magnitude Mw = 9.3; epicenter coordinates 3.3° N, 96.0° E; depth h ≈ 30 km [1, 2]; approximately 300 000 victims due to the tsunami on the Indian Ocean coast) and March 28, 2005, (Mw = 8.6; 2.1° N, 97.0° E; h ≈ 30 km; more than 1000 victims), which occurred in the Sunda Trench west of Sumatra Island, confirm the common opinion that the search for factors controlling the origin of great earthquakes in island arcs is a problem of vital importance in seismology.
dc.title	WHERE AND HOW DID THE RUPTURES OF DECEMBER 26, 2004 AND MARCH 28, 2005 EARTHQUAKES NEAR SUMATRA ORIGINATE?
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010132