1887

Abstract

Summary

The model has been developed in which by the resistivity of lithologic-and-stratigraphic units determined before and after coal seam winning the undermining impact area was recognized. This area breaks down into two flexure zones respectively, without and with discontinuity of rocks. The model is described as physico-geological basis for the use of EM sounding to predict hazardous mining-and-geological events that result from coal winning and to evaluate rock mass as methane reservoir produced after coal seam was taken away.

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/content/papers/10.3997/2214-4609.201701835
2017-05-15
2024-03-28
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References

  1. ГречухинВ. В.
    [1990]. Петрофизика угленосных формаций. Москва, Недра, 472.
    [Google Scholar]
  2. ИвановЛ. А.
    [2015]. Расчленение угленосного карбона Донбасса на пачки по принципу однозначности петрофизических зависимостей для геофизической оценки качества коллекторов метана. Тектоніка і стратиграфія, 42, 101–105.
    [Google Scholar]
  3. ИофисМ. А., ШмелевА. И.
    [1985]. Инженерная геомеханика при подземных разработках. Москва, Недра, 248.
    [Google Scholar]
  4. Итенберг, С. С.
    [1987]. Интерпретация результатов геофизических исследований скважин. Москва, Недра, 375 с.
    [Google Scholar]
  5. Руководство интерпретатора
    Руководство интерпретатора [2004]. Станция электроразведочная “Импульс-Д”. ИКГП 416461.002Д2. Новосибирск, ООО “Сибгеотех”, 36.
    [Google Scholar]
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