Özet:

On 08.08.2019, a earthquake of MW:6.0 (AFAD) magnitude occurred in the Bozkurt district connected to the Denizli province. The outer center of the earthquake that occurred at a depth of 8 km is located on the KD-GB-long Acıgöl Grabeni, about 50 km long. When the main shock of the earthquake and the distribution of increasing shocks, the depth and focus mechanism solutions and the seismological data and the active tectonic structure of the area and the living foil characteristics are evaluated together, the benefit that leads to the earthquake is observed as the DKD-BGB extended and northwest-wrapped foil, which limits the south-eastern edge of the grape. In this study, two-dimensional demand analysis was carried out with measurements in the past years (pre- earthquake) in the GNSS network of 21 points consisting of continuous and campaign-type points located in the region and with the help of the speed range obtained. The highest voltage is at the nearest point to the earthquake center base and the earthquake solutions are in harmony with the earthquake. Using measurements in the past years (pre- earthquake) and measurements in the year 2019 (post earthquake), co-sismic deformations (surface changes) have been determined. The deformations occurring in the post- earthquake area are varied between -7.3 and 7.5 mm for the northern components, while for the east components are varied between -4.6 and 11.6 mm.

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