The determination of relations between statistical seismicity data and geodetic strain analysis, in sultandaği fault

Aksehir-Simav Fault System (ASFS) was first named by Koçyigit (1984) and a 500 km long zone extending between the south of Konya and Balıkesir in the east. This fault system is located within the fault system of Western Anatolia. There are a number of horst and graben types of structures extending parallel to each other in this system. In thisstudy, a GNSS network consisting of 27 points was established in 2012 in order to determine the crustal movements in the part between Afyon and Sultandağı located in ASFS. 5-campaign of GNSS measurements were performed from 2012 to 2018 and the velocity vectors of the region were obtained. These GNSS measurements were evaluated using GAMIT / GLOBK software. In addition, the b parameters of the region were calculated using the earthquake data in the region and compared with the geodetic strains. As a result, it is observed that the geodetic strains have increased towards the west of the region after the 2002 Eber earthquakes.