2017
DOI: 10.1002/9781119227519.ch13
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Geophysical Method of Defining Residual and Active Rock Stresses

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“…The paper [12] indicates that for undisturbed rock without fractures, the failure zone is smaller than in the mass with bedding layers. Stratified structure reduces rock strength due to planes of weakening [13], [14]. The authors of the paper [15], based on experimental data, constructed regression relationships to assess the influence of bedding angle and lateral pressure on strength and deformation.…”
Section: Introductionmentioning
confidence: 99%
“…The paper [12] indicates that for undisturbed rock without fractures, the failure zone is smaller than in the mass with bedding layers. Stratified structure reduces rock strength due to planes of weakening [13], [14]. The authors of the paper [15], based on experimental data, constructed regression relationships to assess the influence of bedding angle and lateral pressure on strength and deformation.…”
Section: Introductionmentioning
confidence: 99%