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Any geodynamic stress in the earth’s crust leads to a change in the relief. Beams and ravines develop along weak fractured zones, faults are traced as changes in the direction of rivers, beams, ravines, and lake contours. The fourth chapter is devoted to the study of these manifestations. It analyzes the manifestation of the tectonic structure using geophysical methods (gravity exploration, seismic exploration, magnetic exploration, drilling) and salt bodies in the morphostructures of the relief when deciphering materials from remote sensing of the Earth.

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Morphostructural Analysis and Results of Structural Interpretation of Remote Sensing Data and Topographic Materials

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  • 发表日期：

    2026年

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  • Ihor Bagriy,
  • Iaroslav Kryl,
  • Oleksandr Riepkin,
  • Oleksandr Popov

摘要

Any geodynamic stress in the earth’s crust leads to a change in the relief. Beams and ravines develop along weak fractured zones, faults are traced as changes in the direction of rivers, beams, ravines, and lake contours. The fourth chapter is devoted to the study of these manifestations. It analyzes the manifestation of the tectonic structure using geophysical methods (gravity exploration, seismic exploration, magnetic exploration, drilling) and salt bodies in the morphostructures of the relief when deciphering materials from remote sensing of the Earth.