NDLI: Seismotectonic content by the source parameters of the 10 June 2012 Ölüdeniz-Fethiye (Dodecanese Islands) Mw 6.1 earthquake and aftershocks (southwestern Turkey)

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Seismotectonic content by the source parameters of the 10 June 2012 Ölüdeniz-Fethiye (Dodecanese Islands) Mw 6.1 earthquake and aftershocks (southwestern Turkey)

Content Provider	Springer Nature Link
Author	Serkan Irmak, T. Kalafat, Doğan Karakaş, Ahmet Doğan, Bülent
Copyright Year	2015
Abstract	A detailed source and rupture process analyzes of the 10 June 2012 Ölüdeniz-Fethiye (Dodecanese Islands; Mw 6.1) earthquake has been carried out using inversion of both complex body waves and strong ground motion records. The rupture starting from the hypocenter propagated gradually to the southwest. The main rupture is modeled by a main asperity located 2–3 km beneath the hypocenter and two small asperities. The size of the effective source area is about 24 × 12 km, the rupture duration was approximately 12 s and the total seismic moment was estimated to be 1.955 × 10$^{18 }$Nm. Continuation of compression from the Hellenic Arc to the southeast part of Fethiye Gulf in the north developed many active faults with complex geometries in the region. According to the stress field obtained from the focal mechanism solutions of the 10 June 2012 Fethiye (Dodecanese Islands; Mw 6.1) earthquake and M ≥ 3.5 earthquakes which occurred in Fethiye Gulf, the region between Fethiye Gulf and Rhodes Basin was deformed by the NW–SE oriented extension. (T-σ3) principal stress axis is dominant in the region. Additionally, NNW–SSE compression (P-σ1) in further southwest of Fethiye Gulf contributed to forming normal and strike-slip faults. Continuation of the NE–SW trending thrust faults located from the west limb of the Hellenic Arc to the southeast of Fethiye Gulf caused deformation in the region due to the seismotectonic model of the region. Both, normal faulting related to the “pure extension” occurred after the compression, and strike-slip faulting associated with the “transtension”, have been expressed by the spatial positions of the principal stress axes in the study area.
Starting Page	15
Ending Page	41
Page Count	27
File Format	PDF
ISSN	22135812
Journal	Acta Geodaetica et Geophysica Hungarica
Volume Number	51
Issue Number	1
e-ISSN	22135820
Language	English
Publisher	Springer Netherlands
Publisher Date	2015-03-05
Publisher Institution	Quarterly of the Hungarian Academy of Sciences
Publisher Place	Dordrecht
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Extension Stress field Fethiye (Dodecanese Islands; Mw 6.1) earthquake Geophysics/Geodesy Focal mechanism Transtension Seismotectonic model
Content Type	Text
Resource Type	Article
Subject	Building and Construction Geology Geophysics

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