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Earthquake Focal Mechanisms Along the Central Segment of the North Anatolian Fault
Date
2010-05-02
Author
Karasözen, Ezgi
Özacar, Atilla Arda
Biryol, C. Berk
Beck, Susan L.
Zandt, George
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The North Anatolian Fault (NAF) is one of the world’s largest active continental strike-slip faults, and forms the northern margin of the Anatolian plate. Although its geologic and geomorphologic features are well defined, crustal deformation and associated seismicity around central segment of the NAF is relatively less-known. In this study, we analyzed locations and focal mechanisms of over hundred events with magnitude ≥ 3, which are recorded by 39 broadband seismic stations deployed by the North Anatolian Passive Seismic Experiment (2005-2008). The distribution of the events shows that the local seismicity in the area is widely distributed, suggesting a widespread continental deformation in the southern block. For the entire data set, P- and S- arrival times are picked and events are relocated using the HYPOCENTER program. Then, relocated events which have a good azimuthal coverage with a maximum gap of 120 and at least 13 P- wave readings are selected and 1-D inversion algorithm, VELEST, is used to derive the 1-D seismic velocity model of the region. The final model, with updated locations is later put together to the FOCMEC program, to obtain focal mechanisms solutions. In this step, an iterative scheme is applied, by increasing the number of data errors. To obtain more unique solutions, first motions are used along with SH/P wave amplitude ratios. Preliminary results indicate a dominant strike-slip mechanism in the southern block that correlates with the splays of NAF. Overall stress field is highly variable across the region, which will be mapped out by stress inversion of resultant focal mechanism solutions and available geological data.
URI
http://meetingorganizer.copernicus.org/EGU2010/EGU2010-6712-6.pdf
https://hdl.handle.net/11511/94691
Conference Name
European Geosciences Union General Assembly 2010
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Department of Geological Engineering, Conference / Seminar
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The North Anatolian Fault (NAF) is one of the world’s largest active continental strikeslip faults, and forms the northern margin of the Anatolian plate. Although its geologic and geomorphologic features are well defined, crustal deformation and associated seismicity around central segment of the NAF is relatively less-known. In this study, we analyzed locations and focal mechanisms of 172 events with magnitude ≥ 3, which are recorded by 39 broadband seismic stations deployed by the North Anatolian Passive ...
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Anatolian interior is characterized by large lateral and vertical displacements and a complex tectonic history. Especially, Central Anatolia is located between escape tectonics in the east and extensional deformation in the west. The nature of this transition is still under much debate and requires detailed analysis of active tectonic stresses within the region. In this study, regional moment tensor inversion is performed for 29 earthquakes with M>3.5 recorded between 2013-2015 by a temporary broadband seis...
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The North Anatolian Fault (NAF) is one of the world's largest continental strike-slip faults. Despite much geological work at the surface, the deep structure of the NAF is relatively unknown. The North Anatolian Fault Passive Seismic Experiment is mainly focused on the lithospheric structure of this newly coalescing continental transform plate boundary. In the summer of 2005, we deployed 5 broadband seismic stations near the fault to gain more insight on the background seismicity, and in June 2006 we deploy...
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E. Karasözen, A. A. Özacar, C. B. Biryol, S. L. Beck, and G. Zandt, “Earthquake Focal Mechanisms Along the Central Segment of the North Anatolian Fault,” VİYANA, Avusturya, 2010, vol. 12, Accessed: 00, 2021. [Online]. Available: http://meetingorganizer.copernicus.org/EGU2010/EGU2010-6712-6.pdf.