Özet:

Chameli is one of the active tectonic areas located in the middle part of the Burdur-Fethiye Fay area. In the years 2007-2008 there was an increase in micro-agriculture activity. The largest of these earthquakes was the 29th October 2007 (ML=5.1) Chameli earthquake. TÜBİTAK Land and Maritime Sciences Institute and the General Directorate of Disaster Affairs of the Earthquake Research Department (AFAD) jointly conducted the 'Emergency Observation Research' project, which was established in the district of Chameli with 10 earthquakes and more than 700 earthquakes after the Chameli earthquake were recorded. The University of Boğaziçi Kandilli Rasathanesi has collected 1206 earthquake data from the catalogue prepared by the National Earthquake Monitoring Center of the Earthquake Research Institute (BDTIM) in the Chameli Region in 2007-2008. The data from both BDTIM and TÜBİTAK have been examined. The earthquakes were properly repositioned and a profound change of the seismogenic generation for the work area was detected. The geometry of the benefit of the Chameli earthquake and the distribution of the focus depth are revealed. It is used by the Earthquake Couple Difference Method (HypoDD). With the application of the HypoDD method, the boundary of the seismogenous skin is clearly seen with the improvement of the depths of the earthquake focus from the vertical cuts, where the dispersed earthquake positions are shrinked to smaller sets for both data groups. The increase in shocks of the Chameli earthquake is between 5 and 15 km. This also applies to the subtle fragile part of the skin. On the surface, the earthquakes were found to form linearity in the direction of KB-GD and KD-GB.

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