2018
DOI: 10.4028/www.scientific.net/jera.35.77
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Analytical Research of the Stress-Deformed State in the Rock Massif around Faulting

Abstract: In this paper, the geological faults in the zone of stable geodynamic and tectonic activity are studied. The purpose of the analytical research is to establish regularities of rock pressure in the hanging and foot walls of the geological fault and its influence on the state-deformed state of the rock massif. Comprehensive methodology that included analytical calculation will be implemented in the work. Taking into account the complexity of determining the stress-deformed state of the rocks, evaluation method o… Show more

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Cited by 71 publications
(59 citation statements)
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“…the room) and, on the opposite, harder ores tend to accumulate stress due to smaller deformations. However, stability of less hard ore crowns decreases due to reduction of their ultimate strength [12][13][14].…”
Section: Methodsmentioning
confidence: 99%
“…the room) and, on the opposite, harder ores tend to accumulate stress due to smaller deformations. However, stability of less hard ore crowns decreases due to reduction of their ultimate strength [12][13][14].…”
Section: Methodsmentioning
confidence: 99%
“…The technique of determining the line of the least resistance and distances between borehole ends should be applied when determining parameters of blasting and drilling operations [25,36,37,40].…”
Section: Resultsmentioning
confidence: 99%
“…from 56% to 62%) [19][20][21]. This updating trend is based on force impacts on the substance during disintegration in the activator but it does not consider processes connected with underground mining of the useful mineral [22][23][24][25]. Constantly improved software of the automated complexes indicates iron content in real time and is able to split ore mass flows by quality.…”
Section: Introductionmentioning
confidence: 99%
“…where q n -quantity of an explosive at undermining of a massif with n the bared surfaces, kg/t; q -quantity of an explosive at undermining of a massif with one bared surface, kg/t; n -quantity of the bared surfaces, pieces. If the bared surface faces broken-down rocks in this case fading of amplitude of waves of stresses there will be something smaller, than in a case with the bared surface of considerable width [3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%