HAZARD SEISMIC STUDIES FOR THE ROMANIAN CAPITAL - APPLING THE SHAKE MAP METHOD

dc.contributor.author	Balan S.F.
dc.contributor.author	Cioflan C.O.
dc.contributor.author	Apostol B.F.
dc.date.accessioned	2024-09-22T02:54:24Z
dc.date.available	2024-09-22T02:54:24Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=14395854
dc.identifier.citation	Acta Geodaetica et Geophysica Hungarica, 2006, 41, 3-4, 341-347
dc.identifier.issn	1217-8977
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/45380
dc.description.abstract	The shake map methodology for seismic hazard studies has been applied to a sector of Bucharest, the capital of Romania. Geological and geotechnical profiles are known for this region. We have chosen as seismic input the event of 30 August 1986, MW = 7.1. We discuss the propagation of a synthetic signal with known source characteristics, from source to bedrock and back to surface. It is possible to produce surface synthetic signals in the studied area, having very similar characteristics (accelerations) to the observed ones. © 2006 Akadémiai Kiadó, Budapest.
dc.subject	ACCELERATION
dc.subject	BEDROCK
dc.subject	SEISMIC HAZARD
dc.subject	SHAKE MAP
dc.title	HAZARD SEISMIC STUDIES FOR THE ROMANIAN CAPITAL - APPLING THE SHAKE MAP METHOD
dc.type	Статья
dc.identifier.doi	10.1556/AGeod.41.2006.3-4.6

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