2020
DOI: 10.3390/en13081897
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Occurrence of Linear Discontinuous Deformations in Upper Silesia (Poland) in Conditions of Intensive Mining Extraction—Case Study

Abstract: Currently, linear discontinuous deformations in mining areas are an important issue, both due to the frequency of their occurrence and the threat they pose to general safety. This paper presents a case study of an occurrence of such a deformation. The analyses of the geological and mining conditions, as well as the conducted calculations presented herein, indicate that the cause of the deformation was the occurrence of high-value horizontal tensile strains. It was triggered by mining exploitation carried out w… Show more

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Cited by 15 publications
(9 citation statements)
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“…The category of the "mining area", depending on the interpretation of the horizontal strain (including the relaxation (or not) of the horizontal strain), ranged from III (with relaxation) to V (without relaxation). Such high values of the terrain category and the occurrence of tectonic faults in Carboniferous beds were found to be the main causes of linear discontinuous deformations, which is confirmed by studies conducted in this field to date [6,7,9,10].…”
Section: Discussionsupporting
confidence: 59%
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“…The category of the "mining area", depending on the interpretation of the horizontal strain (including the relaxation (or not) of the horizontal strain), ranged from III (with relaxation) to V (without relaxation). Such high values of the terrain category and the occurrence of tectonic faults in Carboniferous beds were found to be the main causes of linear discontinuous deformations, which is confirmed by studies conducted in this field to date [6,7,9,10].…”
Section: Discussionsupporting
confidence: 59%
“…Linear discontinuous deformations of the surface type result from the formation of fractures and slippage of the near-surface soil layer, which is most frequently subjected to continuous deformations due to underground mining excavations [6,7,10,[50][51][52]. Kwiatek (2003) [50], analyzing the impact of horizontal loosening of near-surface layers of soil, stated that the cause of the formation of discontinuities is from bringing the near-surface layer of the rock mass made of soil to the state of limit equilibrium, as a result of which, slippage surfaces may appear, or, in the cases of horizontal loosening of the layer with cohesion c ≠ 0, vertical fractures separating soil masses that continue to move as non-deformable masses.…”
Section: Methodsmentioning
confidence: 99%
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