Assessment of the deformation field of the Tashkent region based on GNSS data analysis

This paper presents the results of determining the present-day vertical movements of the Earth's crust in the Tashkent region based on data from GNSS stations measured over two observation cycles in the eastern part of Uzbekistan. The thickness of the Earth's crust was calculated using the Airy isostatic equilibrium model, and the obtained results were analyzed. The deformation state of the Earth's crust was also quantitatively assessed, and the results obtained were compared with the seismicity of the region.

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