Evaluation of the possibility of manifestation of deformations from the position of disturbance of the massif (using the Kamagan field as an example)
Introduction. The main task in the development of mineral deposits by open and underground methods is to ensure the safety of mining operations. As a result of long-time standing of the pit walls in the near edge zone massif, changes in natural stresses can occur, which lead to deformations. Prediction and prevention of deformation processes of the near-rock massif largely depend on reliable information about its structural features, including the structure of the massif and the degree of its disturbance. Purpose of research is to assess the possibility of manifestation of deformations from the position of disturbance of the massif. Methods of research. When assessing the possibility of deformation manifestation, a set of methods was used, including: full-scale measurements of fracturing; methods of mathematical statistics using the Stereonet program for processing measurement results; analysis of the spatial position of cracks relative to the direction of strike of the slopes and sides of the open pit with the identification of the most dangerous ones; kinematic analysis, allowing to determine potential types of loss of stability from the position of disturbance of the massif. Result of research. In the southeastern, northern and western sides of the Kamagan open pit, 41 fracture systems have been identified; the prevailing systems are northwestern dip systems at angles of 50 ° –85 °; south-east - at an angle of 50 ° and south-west - at an angle of 50 °. For example, for the northern side (Ap = 90 °; n = 60 °), it was found that potential types of destabilization are: wedge formed by systems of cracks with spatial characteristics Ap = 65 °; n = 45 ° and Apr = 150 °; n = 90 °, and planar sliding formed by systems of cracks with the parameters Ap = 90 °; n = 55 ° and Apr = 100 °; n = 42 °. Conclusions. Studies have proven the need to study and identify weakening surfaces in the process of mining and determine the parameters of their occurrence in order to assess the possibility of deformations and further assess the stability of slopes.