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Abstract

Summary

The geological mapping, structural, lithological, petrographic, and petrophysical investigations carried out in the «Pivdennyi» and «Pivnichnyi» iron ore quarries of the Saksahansky district of the Kryvyi Rih iron ore basin allowed us to characterize a “new” morphological and genetic type of anthropogenic formations/deposits in Kryvyi Rih basin (Kryvbas) – shear zones due to underground mining, as well as to raise the question of the relevance of including it in modern classifications of anthropogenic deposits in Kryvyi Rih basin as a separate type. The main structural, morphological and material element of the above-mentioned zones is the so-called collapse technobreccias (breccias due to the collapse of overlying rock masses into the mined underground space), which make up huge volumes within the quarries, actually forming new large-scale anthropogenic geological bodies with their own morphology, material composition and physical properties that differ from the original parent rocks. It has been shown that collapse technobreccias are widespread within the «Pivdennyi» and «Pivnichnyi» quarries, occupying almost 100% of their axial areas, as well as significant volumes of the western sides of the quarries. They, along with the remains of ferruginous quartzite and the remnants of rich ore left over from underground mining, are the subject of modern industrial mining. Technobreccias are new technogenic rocks. Genetically and morphologically, they fully correspond to the essence of technogenic formations and it is quite legitimate to apply the conceptual and legal framework of technogenic deposits to them in case of their economically feasible extraction, just as it is generally recognized for bulk dumps and sludge pits.

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/content/papers/10.3997/2214-4609.2023520052
2023-11-07
2025-04-20
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References

  1. Evtekhov, V.D. (2003). Technogenic deposits: from the use of existing ones to the creation of more advanced ones.Geological and Mineralogical Bulletin, 1, 19–26. [in Russian].
    [Google Scholar]
  2. Kazakov, V.L. (1999). Geomorphology of the Kryvbas collapse zones. Environmental protection: ecological, educational, medical aspects.Mater. IV All-Ukrainian Conference, Kryvyi Rih, part III, 29–31. [in Ukrainian].
    [Google Scholar]
  3. Complex development of ore deposits. (2005). Edited by A.D.Chernykh. Kyiv: Technika. [in Russian].
    [Google Scholar]
  4. Malakhov, G.M. (1990). Management of mountain pressure in the development of ore deposits of the Kryvyi Rih basin. Kyiv: Naukova dumka. [in Russian].
    [Google Scholar]
  5. Malakhov, I.M. (2003). Technogenesis in the geological environment. Kryvyi Rih. [in Ukrainian].
    [Google Scholar]
  6. Oliynyk, T.A., Kushniruk, N.V., Saitgareev, L.N., Nagnibida, I.O. (2012). Technogenic deposits and their classification.Minerals Enrichment, 50(91). [in Ukrainian].
    [Google Scholar]
  7. Rivkin, I.D. (1959). Features of the collapse of rocks of the hanging side of ore deposits of the Kryvyi Rih basin.Mining journal, 4, 10–15. [in Russian].
    [Google Scholar]
  8. Chernenko, V.A. (1998). Forecasting the development of anthropogenic deposits in Kryvbas.Bulletin of the Academy of Mining Sciences of Ukraine, 1, 26–29. [in Russian].
    [Google Scholar]
  9. Chernyi, G.I. (1959). Displacement of rocks of the lying side in the Kryvyi Rih basin. Kyiv: URSR Academy of Sciences, Institute of Mining. [in Ukrainian].
    [Google Scholar]
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