Return to search

Source mechanisms of the 2004 Baladeh (Iran) earthquake sequence from Iranian broadband and short-period data and seismotectonic implications

The northward movement and collision of the Arabian plate with Eurasia generates compressive stresses and resulting shortening in Iran. Within the Alborz Mountains, North Iran, a complex and not well understood system of strike-slip and thrust faults accomodates a fundamental part of the NNE-SSW oriented shortening.
On 28th of May 2004 the Mw 6.3 Baladeh earthquake hit the north-central Alborz Mountains. It is one of the rare and large events in this region in modern time and thus a seldom chance to study earthquake mechanisms and the local ongoing deformation processes. It also demonstrated the high vulnerability of this densily populated region.

Identiferoai:union.ndltd.org:Potsdam/oai:kobv.de-opus-ubp:5398
Date January 2011
CreatorsDonner, Stefanie, Rößler, Dirk, Krüger, Frank, Ghods, Abdolreza, Strecker, Manfred
ContributorsTechnical University Denmark, Inst. for Advanced Studies in Basic Sciences
PublisherUniversität Potsdam, Mathematisch-Naturwissenschaftliche Fakultät. Institut für Erd- und Umweltwissenschaften
Source SetsPotsdam University
LanguageEnglish
Detected LanguageEnglish
TypeMisc
Formatapplication/pdf
Rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/de/

Page generated in 0.0018 seconds