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Abstract

Summary

Structural-morphometric works were carried out within the Middle Dnipro Region using remote sensing methods and geographic information systems. A wide complex of structural-morphometric analyses was applied and geological interpretation was carried out to determine the presence and nature of the identified morphometric indicators and how the latter are related to terrace levels, as well as the direction and intensity of recent and modern tectonic movements, deep erosion, denudation and accumulation of the studied region. The neotectonic conditions of development and formation of the Right Bank were reconstructed, taking into account the advantage of some factors over others at each stage. Peculiarities of the development of terrace levels in the Neogene and Quaternary times have been established. Attention was paid to development of dangerous processes caused by many factors of development of the region. The obtained data may serve as a basis to analyze the impact of tectonic movements on the intensification of dangerous geological processes within the Middle Dnipro Region and to forecast their development in the future.

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/content/papers/10.3997/2214-4609.20215K2071
2021-11-17
2024-04-27
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References

  1. Development of draft Regulations on the landslide regime and the Concept of stabilization of landslide processes on the territory of Kyiv
    Development of draft Regulations on the landslide regime and the Concept of stabilization of landslide processes on the territory of Kyiv. (2013). Information report on NDR № 04/2013100. National Academy of Sciences of Ukraine DU «Institute of Environmental Geochemistry of the National Academy of Sciences of Ukraine». https://drive.google.com/file/d/1NVjnekvlaNoE_kxNf_qeQRfOxhuO-Dm_/view
    [Google Scholar]
  2. Ivanik, O., Shevchuk, V., Kravchenko, D., Yanchenko, V., Shpyrko, S., Gadiatska, K.
    (2019). Geological and Geomorphological Factors of Natural Hazards in Ukrainian Carpathians. Journal of Ecological Engineering, 20(4), 177–186. doi:10.12911/22998993/102964.
    https://doi.org/10.12911/22998993/102964 [Google Scholar]
  3. Ivanik, O., TustanovskaL.
    , (2011). Application of classical methods of structural-morphometric analysis for reconstruction of modern GIS-based tectogenesis. Journal of Geologe, 53, 4–7.
    [Google Scholar]
  4. Ivanik, O.M., Shevchuk, V.V., Tustanovska, L.V., Hadiatska, K.P., Volkova, S.G.
    (2020). Estimation of neotectogenesis factors of the Middle Dnieper region by structural-morphometric nethod. Geoinformatics2020, 11–14May 2020, Kiev.
    [Google Scholar]
  5. Menshov, O., Kuderavets, R., & Chobotok, I.
    (2018). Magnetic and mineralogy analysis of soils of hydrocarbon prospective areas in Ukraine. In 24th European Meeting of Environmental and Engineering Geophysics, 1, 1–5. European Association of Geoscientists & Engineers.
    [Google Scholar]
  6. Menshov, O., Spassov, S., Camps, P., Vyzhva, S., Pereira, P., Pastushenko, T., & Demidov, V.
    (2020). Soil and dust magnetism in semi-urban area Truskavets, Ukraine. Environmental Earth Sciences, 79(8), 1–10.
    [Google Scholar]
  7. Philosophov, V.P.
    (1975). Fundamentals of the morphometric method for the search for tectonic structures. Saratov, 231.
    [Google Scholar]
  8. Report on engineering-geological and geophysical study
    Report on engineering-geological and geophysical study. (2007). Ministry of Environmental Protection of Ukraine, State Geological Survey, Northern State Regional Geological Enterprise “Northern Geology”, Center for Hydrogeological and Geological-Ecological Research, Center for Geophysical Research, 138. https://drive.google.com/file/d/1ArhRjam21JvtHt5439DgIobyc8AH8AQO/view
    [Google Scholar]
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