Dynamics of engineering and geological conditions of mineral deposits (from exploration to exploitation)
Автор: Abaturova I.V., Storozhenko L.A., Nugmanova E.D., Kozlov V.S.
Журнал: Вестник Пермского университета. Геология @geology-vestnik-psu
Рубрика: Инженерная геология, мерзлотоведение и грунтоведение
Статья в выпуске: 3 т.20, 2021 года.
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The development of mineral deposits has strong transformative effect on the geological environment. At the same time, all the components of geotechnical conditions (relief, structure of rock massifs, hydrogeological and geocryological conditions etc.), formed over a long geological time, are actively changing. Geological processes are activated and new mining-geological processes are formed. New strata are formed on the Earth's surface along with the technogenic formations and technogenic deposits. Today, the scale of technogenesis in mining is comparable to the results of geological activities that have been going on for many millions of years. The reaction of the geological environment is immediate and is expressed in the development of large-scale engineering and geological processes, which often do not allow the further development of mineral resources and threaten the human life. Therefore, even at the early stages of prospecting and/or exploration, it is necessary to understand the dynamics of changes in surrounding medium in order to develop methods for proper managing of the ore extraction. By the example of a number of objects, all the stages of study of engineering-geological conditions are considered, the dynamics of their change, which led to the formation of engineering-geological processes affecting the further development of mineral resource, is estimated.
Mineral deposits, geological environment, geotechnical processes, engineering-geological conditions, engineering-geological model, dynamics of engineering-geological processes, stability of quarry walls, physical and mechanical properties, fracturing
Короткий адрес: https://sciup.org/147246213
IDR: 147246213 | DOI: 10.17072/psu.geol.20.3.222
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