ОБОСНОВАНИЕ ПРИРОДЫ ОБРАЗОВАНИЯ МЕЛКОАМПЛИТУДНЫХ ТЕКТОНИЧЕСКИХ НАРУШЕНИЙ В ЗАПАДНОМ ДОНБАССЕ

Features of tectonic structures distribution in soft rocks confirm the presence of horizontal tectonic forces in the formation of faults and are based on the manifestation of their morphological features. Linear dependences of the amplitude on the length of a tectonic dislocation in the wedging area were obtained as a result of mathematical processing of experimental data. Actual position of crossing lines of fault plane and the seam were considered while studying the distribution of co-fault fracturing. Data analysis confirms that distribution of faulting has undulating character. Analysis of observations showed that deviation of the crossing line of fault plane with the seam from the middle line is subject to the normal law of random variable distribution. Thus, the studies and the obtained results allow planning mining operations and assessing their utility while developing fault areas.