The high pressure created by the stretching or compression of the rocks on the earth causes the earth's crust to break and faults occur. These faults are found in many parts of the world and are actively seen in Türkiye. In this study, space and satellite techniques and geodetic results of the Sofalaca-Şehitkamil Gaziantep earthquake that occurred on the Eastern Anatolian Fault Zone on 06.02.2023 in Türkiye were evaluated. Stations recording GNSS observations at 1Hz sampling interval of the network of Continuously Operating Reference Stations, Türkiye (CORS-TR) were used, homogeneously distributed in and around the epicenter where the earthquake occurred. In order to examine the characteristics of the surface movements occurring at the time of the earthquake, the Kinematic-PPP technique and the 1 second RINEX data in the RTKLIB software were evaluated with both real-time and post-process solution approaches. With both solution approaches, displacement amounts and velocities, of the surface waveforms occurring at the time of the earthquake were calculated at all stations. In addition, the co-seismic displacements of the selected 23 stations after the earthquake were calculated and the changes on the surface of the earthquake were interpreted. At GNSS Stations, the maximum velocities during the earthquake were calculated in the range of 1.6-23.3cm/s for the north component, 0.5-13.5cm/s for the east component, and 1.9-24.6cm/s for the up component. The post-earthquake co-seismic displacements at stations were determined as 0.1-37.1 cm for the north component, 0.1-22.7cm for the east component and 0.1-20.0cm for the up component.