Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data
Journal: SHILAP Revista de lepidopterología
Year: 2012

Within the limits of western Crimean Mountains 2016 tectonic slickenside with kinematic indicators and 600 ruptures without visible signs of displacement have been studied. Stress fields were determined using structural-paragenetic and kinematic analyses. These fields were subdivided into three types: strike-slip, normal, and reverse that constitute 51, 30 и 19 % of the total fault planes. The principal axes trends for each field type were compared with the strike of the Main Ridge. Contemporary