The impact of structural-tectonic and lithogenous peculiarities of the rock mass on the formation and development of geo-deformation processes

摘要

The paper introduces the results of long-term observations of the displacement of outlines of underground drainage galleries No. 2 and 3 located at the area of the first stage of landslide protection structures of Odessa shore and of rock deformation in depth of adits (the measuring depth of projection meter u0001M-100 is 42-43 m) drilled in right bank slope basis on the territory of portYuzhny. It reveals structural-tectonic peculiarities of the rock mass and shows that spatial arrangement of tectonically weak zones determines the direction of shear deformation and of the drift of slope and structure bases.